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    <title>Recent lbnl_ees_ce items</title>
    <link>https://escholarship.org/uc/lbnl_ees_ce/rss</link>
    <description>Recent eScholarship items from Climate &amp; Ecosystems</description>
    <pubDate>Fri, 15 May 2026 07:01:19 +0000</pubDate>
    <item>
      <title>Participatory modeling in the AI era</title>
      <link>https://escholarship.org/uc/item/2f18q3mv</link>
      <description>PM is a now established approach to improve the utility and actionability of modeling for decision making and management. With the advent of the AI era, there are multiple avenues for its use in the context of PM. We reviewed a number of recent papers that describe how various AI tools have been used to assist the PM process, both in improving the quality of modeling and the participation efficiency. We have identified AI applications that can help stakeholders in the process of knowledge acquisition and decision making during the steps of the PM process. We also looked at how AI has been put to several innovative uses in PM related areas, such as collective intelligence, deliberative democracy and participatory governance, and how these can be adopted and used in the PM process. These enhancements escalate in degree of AI intervention and autonomy. They start with augmenting approaches such as informing, modeling and data processing, and can lead to deeper AI engagement such...</description>
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      <pubDate>Tue, 5 May 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Kolagani, Nagesh</name>
      </author>
      <author>
        <name>Glynn, Pierre D</name>
      </author>
      <author>
        <name>Voinov, Alexey</name>
      </author>
      <author>
        <name>Quinn, Nigel WT</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
      <author>
        <name>Helgeson, Jennifer</name>
      </author>
      <author>
        <name>Dyckman, Caitlin S</name>
      </author>
    </item>
    <item>
      <title>Best practices in software development for robust and reproducible geoscientific models based on insights from the Global Carbon Budget's dynamic vegetation models</title>
      <link>https://escholarship.org/uc/item/9nx801c6</link>
      <description>Abstract. Computational models play an increasingly vital role in scientific research by enabling the numerical simulation of complex processes. Such models are also fundamental in geosciences. For instance, they offer critical insights into the impacts of global change on the Earth system today and in the future. Beyond their value as research tools, models are also software products and should therefore adhere to certain established software engineering standards. However, scientists are rarely trained as software developers, which can lead to potential deficiencies in software quality like unreadable, inefficient, or erroneous code. The complexity of models, coupled with their integration into broader workflows, also often makes it challenging to reproduce results, evaluate processes, and build upon them. In this paper, we review the state and current practices of the development processes of the state-of-the-art land surface models used by the Global Carbon Budget. We combine...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9nx801c6</guid>
      <pubDate>Fri, 24 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Gregor, Konstantin</name>
      </author>
      <author>
        <name>Meyer, Benjamin F</name>
      </author>
      <author>
        <name>Gaida, Tillmann</name>
      </author>
      <author>
        <name>Vasquez, Victor Justo</name>
      </author>
      <author>
        <name>Bett-Williams, Karina</name>
      </author>
      <author>
        <name>Forrest, Matthew</name>
      </author>
      <author>
        <name>Darela-Filho, João P</name>
      </author>
      <author>
        <name>Rabin, Sam</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Melton, Joe R</name>
      </author>
      <author>
        <name>Nord, Johan</name>
      </author>
      <author>
        <name>Anthoni, Peter</name>
      </author>
      <author>
        <name>Bastrikov, Vladislav</name>
      </author>
      <author>
        <name>Colligan, Thomas</name>
      </author>
      <author>
        <name>Delire, Christine</name>
      </author>
      <author>
        <name>Dietze, Michael C</name>
      </author>
      <author>
        <name>Hurtt, George</name>
      </author>
      <author>
        <name>Ito, Akihiko</name>
      </author>
      <author>
        <name>Keetz, Lasse T</name>
      </author>
      <author>
        <name>Knauer, Jürgen</name>
      </author>
      <author>
        <name>Köster, Johannes</name>
      </author>
      <author>
        <name>Lin, Tzu-Shun</name>
      </author>
      <author>
        <name>Ma, Lei</name>
      </author>
      <author>
        <name>Minvielle, Marie</name>
      </author>
      <author>
        <name>Olin, Stefan</name>
      </author>
      <author>
        <name>Ostberg, Sebastian</name>
      </author>
      <author>
        <name>Shi, Hao</name>
      </author>
      <author>
        <name>Schnur, Reiner</name>
      </author>
      <author>
        <name>Sun, Qing</name>
      </author>
      <author>
        <name>Thornton, Peter E</name>
      </author>
      <author>
        <name>Rammig, Anja</name>
      </author>
    </item>
    <item>
      <title>Soil Moisture Buffers the Impact of Precipitation Variability on Ecosystem Productivity</title>
      <link>https://escholarship.org/uc/item/3x389929</link>
      <description>Abstract Water availability governs ecosystem productivity, yet estimates of vegetation sensitivity to water can differ greatly depending on whether the sensitivity is examined spatially or temporally. In particular, the spatial sensitivity is often reported to be much stronger than temporal sensitivities, leading to highly uncertain projections of ecosystem responses to future climate change when using space‐for‐time substitution. The large difference between spatial and temporal sensitivities remains unexplained. Prior research, however, primarily relied on precipitation as the water availability proxy, whereas vegetation responds to soil moisture. Here, we combined satellite estimates of vegetation productivity with soil moisture data across water‐limited ecosystems of the continental United States (CONUS) to identify a convergent sensitivity of productivity to water availability. Using precipitation, we show that temporal sensitivity is 66% lower than spatial sensitivity overall....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3x389929</guid>
      <pubDate>Thu, 23 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Wang, Huiqi</name>
      </author>
      <author>
        <name>Bassiouni, Maoya</name>
        <uri>https://orcid.org/0000-0001-5795-9894</uri>
      </author>
      <author>
        <name>Kang, Yanghui</name>
      </author>
      <author>
        <name>Rifai, Sami W</name>
      </author>
      <author>
        <name>Gherardi, Laureano A</name>
      </author>
      <author>
        <name>Ukkola, Anna</name>
      </author>
      <author>
        <name>Keenan, Trevor F</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
    </item>
    <item>
      <title>Bioenergy Cropping Reduces the Spatiotemporal Scaling of Soil Bacterial Biodiversity</title>
      <link>https://escholarship.org/uc/item/08b4f1cg</link>
      <description>ABSTRACT Widespread bioenergy cropping can transform landscapes, strongly affecting biodiversity. However, the impact of bioenergy cropping on the spatiotemporal scaling of soil biodiversity remains virtually unknown, despite its profound implications for the functioning of the ecological community. Here, we investigated how bioenergy cropping influenced the spatiotemporal scaling of soil bacterial biodiversity in marginal soils (sandy loam and clay loam soils) in Oklahoma, USA. We detected strong, significant species‐time‐area relationships (STARs) and phylogenetic‐time‐area relationships (PTARs) in bacterial communities and their lineages, suggesting that STARs and PTARs exist in microbial ecology within the studied system. Also, spatiotemporal scaling rates (the slopes of STAR and PTAR models) varied substantially among bacterial lineages and were positively correlated with their 16S rRNA gene copy numbers, a genomic trait indicative of microbial growth potentials. Strikingly,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/08b4f1cg</guid>
      <pubDate>Thu, 23 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Ye, Zhencheng</name>
      </author>
      <author>
        <name>Kuang, Jialiang</name>
      </author>
      <author>
        <name>Bates, Colin T</name>
      </author>
      <author>
        <name>Escalas, Arthur</name>
      </author>
      <author>
        <name>Ning, Daliang</name>
      </author>
      <author>
        <name>Wu, Liyou</name>
      </author>
      <author>
        <name>Liu, Suo</name>
      </author>
      <author>
        <name>Deng, Sihang</name>
      </author>
      <author>
        <name>Lei, Jiesi</name>
      </author>
      <author>
        <name>Chen, Xiangwen</name>
      </author>
      <author>
        <name>Pett‐Ridge, Jennifer</name>
      </author>
      <author>
        <name>Saha, Malay</name>
      </author>
      <author>
        <name>Hale, Lauren</name>
      </author>
      <author>
        <name>Wang, Gangsheng</name>
      </author>
      <author>
        <name>Tian, Renmao</name>
      </author>
      <author>
        <name>Fu, Ying</name>
      </author>
      <author>
        <name>Tang, Yu</name>
      </author>
      <author>
        <name>Firestone, Mary</name>
      </author>
      <author>
        <name>Zhou, Jizhong</name>
        <uri>https://orcid.org/0000-0003-2014-0564</uri>
      </author>
      <author>
        <name>Yang, Yunfeng</name>
      </author>
    </item>
    <item>
      <title>A global methane observation system to track climate feedbacks for verifiable climate impact</title>
      <link>https://escholarship.org/uc/item/34j1f61w</link>
      <description>Methane measurements, particularly of natural sources, need to be expanded considerably.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/34j1f61w</guid>
      <pubDate>Wed, 22 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Watts, Jennifer D</name>
      </author>
      <author>
        <name>Ordway, Elsa</name>
        <uri>https://orcid.org/0000-0002-7720-1754</uri>
      </author>
      <author>
        <name>Malone, Sparkle L</name>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Palmer, Paul I</name>
      </author>
      <author>
        <name>Patel-Tupper, Dhruv</name>
      </author>
      <author>
        <name>Ciais, Philippe</name>
      </author>
      <author>
        <name>Li, Fa</name>
      </author>
      <author>
        <name>Monteverde, Danielle R</name>
      </author>
      <author>
        <name>Arndt, Kyle A</name>
      </author>
      <author>
        <name>Bruhwiler, Lori</name>
      </author>
      <author>
        <name>Buma, Brian</name>
      </author>
      <author>
        <name>Cadillo-Quiroz, Hinsby</name>
      </author>
      <author>
        <name>Euskirchen, Eugenie</name>
      </author>
      <author>
        <name>Hoyt, Alison M</name>
      </author>
      <author>
        <name>Holgerson, Meredith</name>
      </author>
      <author>
        <name>Hugelius, Gustaf</name>
      </author>
      <author>
        <name>Jackson, Robert B</name>
      </author>
      <author>
        <name>Jacob, Daniel</name>
      </author>
      <author>
        <name>Kuhn, McKenzie</name>
      </author>
      <author>
        <name>Natali, Susan M</name>
      </author>
      <author>
        <name>Peng, Shushi</name>
      </author>
      <author>
        <name>Perryman, Clarice R</name>
      </author>
      <author>
        <name>Poulter, Benjamin</name>
      </author>
      <author>
        <name>Rey-Sánchez, Camilo</name>
      </author>
      <author>
        <name>Sagang, Le Bienfaiteur</name>
      </author>
      <author>
        <name>Schuur, Edward AG</name>
      </author>
      <author>
        <name>Varner, Ruth K</name>
      </author>
      <author>
        <name>Vargas, Rodrigo</name>
      </author>
    </item>
    <item>
      <title>Contrasting Parametric Sensitivities in Two Global Vegetation Models Using Parameter Perturbation Ensembles</title>
      <link>https://escholarship.org/uc/item/7rc4t27b</link>
      <description>Uncertainty in land model projections remains high and the roles of parametric and structural uncertainty are difficult to disentangle. To compare parametric sensitivity across model structures we present two parameter perturbation ensembles using the Community Land Model (CLM) operating in satellite phenology mode. The ensembles contrast two vegetation modules: (a) the default CLM vegetation module and (b) the Functionally Assembled Terrestrial Ecosystem Simulator (CLM‐FATES). We perturbed over 300 parameters and quantified their effects on biophysical fluxes globally and across biomes. Most parameters have minimal impact on biophysical fluxes, with only a few substantially influencing results. While both models exhibit similar parameter sensitivity for some fluxes, CLM‐FATES shows larger spread in gross primary productivity (GPP), driven by strong sensitivity to carboxylation rate. CLM‐FATES also shows a weaker GPP response to soil hydrology parameters and exhibits higher water...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7rc4t27b</guid>
      <pubDate>Wed, 15 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Foster, AC</name>
      </author>
      <author>
        <name>Hawkins, LR</name>
      </author>
      <author>
        <name>Kennedy, D</name>
      </author>
      <author>
        <name>Bonan, GB</name>
      </author>
      <author>
        <name>Fisher, RA</name>
      </author>
      <author>
        <name>Needham, JF</name>
        <uri>https://orcid.org/0000-0003-3653-3848</uri>
      </author>
      <author>
        <name>Knox, RG</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Koven, CD</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Wieder, WR</name>
      </author>
      <author>
        <name>Dagon, K</name>
      </author>
      <author>
        <name>Lawrence, DM</name>
      </author>
    </item>
    <item>
      <title>Recent Increasing Trend in October–November Caribbean Tropical Cyclone Activity</title>
      <link>https://escholarship.org/uc/item/46z7r317</link>
      <description>October–November Caribbean tropical cyclone (TC) activity has significant impacts for both the Caribbean islands and Central America (e.g., Hurricanes Eta and Iota in 2020). October–November Caribbean TCs can also track northward and make continental United States landfall, resulting in substantial damage and fatalities (e.g., Hurricane Michael in 2018 and Delta and Zeta in 2020). We find significant increasing trends in October–November Caribbean hurricanes, rapidly intensifying hurricanes (winds increasing by ≥15 m s−1 within 24 hr), and landfalling hurricanes during the global satellite era (1979–present). Since 1979, we also observe significant warming trends in the western Atlantic Warm Pool and anomalous relative cooling in the eastern Pacific during October–November. These trends yield a more conducive dynamic and thermodynamic environment for Caribbean TCs, including reductions in Caribbean vertical wind shear, increases in Caribbean potential intensity, and a more TC‐conducive...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/46z7r317</guid>
      <pubDate>Tue, 14 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Klotzbach, PJ</name>
      </author>
      <author>
        <name>Silvers, LG</name>
      </author>
      <author>
        <name>Bercos‐Hickey, E</name>
      </author>
      <author>
        <name>Allen, CJT</name>
      </author>
      <author>
        <name>Bell, MM</name>
      </author>
      <author>
        <name>Blake, ES</name>
      </author>
      <author>
        <name>Bloemendaal, N</name>
      </author>
      <author>
        <name>Bowen, SG</name>
      </author>
      <author>
        <name>Chand, SS</name>
      </author>
      <author>
        <name>Chavas, DR</name>
      </author>
      <author>
        <name>Ekström, M</name>
      </author>
      <author>
        <name>Hemmati, M</name>
      </author>
      <author>
        <name>Jones, JJ</name>
      </author>
      <author>
        <name>Lowry, MR</name>
      </author>
      <author>
        <name>Patricola‐DiRosario, CM</name>
      </author>
      <author>
        <name>Schreck, CJ</name>
      </author>
      <author>
        <name>Truchelut, RE</name>
      </author>
      <author>
        <name>Wood, KM</name>
      </author>
    </item>
    <item>
      <title>Storylines for the 1997 New Year’s Flood: The role of watershed antecedent conditions and future warming in shaping discharge in the Truckee River watershed</title>
      <link>https://escholarship.org/uc/item/3bm339zm</link>
      <description>The 1997 New Year’s flood was among the most devastating floods in the Truckee River watershed located in western Nevada. This event resulted from complex interactions of flood drivers, such as extreme precipitation, wet antecedent watershed conditions, warm temperatures and rapid snowmelt. We leveraged simulated forcings from the regionally refined mesh capabilities of the Energy Exascale Earth System Model (RRM-E3SM) and a process-based hydrological model to recreate the 1997 New Year’s flood for the Truckee River watershed across four climate warming levels ranging from the current temperatures to + 4° C. For each scenario, we conducted ensemble simulations with the same forcing but with 100 different seasonal watershed antecedent conditions, which were randomly sampled from long-term hydrological simulations. The results show that the 1997 New Year’s flood can be reproduced or exceeded consistently only when the antecedent watershed conditions are wet, specifically when streamflows...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3bm339zm</guid>
      <pubDate>Thu, 2 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Yu, Guo</name>
      </author>
      <author>
        <name>Rhoades, Alan M</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Albano, Christine M</name>
      </author>
      <author>
        <name>Miller, Julianne J</name>
      </author>
      <author>
        <name>Webb, Mariana J</name>
      </author>
      <author>
        <name>Dahl, Travis</name>
      </author>
      <author>
        <name>Floyd, Ian</name>
      </author>
    </item>
    <item>
      <title>Depth of nutrient uptake by deep-rooted plants is regulated by water availability</title>
      <link>https://escholarship.org/uc/item/14w4h314</link>
      <description>The capacity of some plants to access water and nutrients at depths greater than one meter is a critical functional trait that confers resistance to drought and impacts both belowground and shallow soil processes. Here, we report water and strontium isotopic data from an alpine meadow transect showing the correlation between water and nutrient acquisition depths. The isotopic compositions of Sr (&lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr ratio) and water in rock and soil, and in plant leaf tissues, reveal that deeper-rooted plants acquire a higher proportion of water, Sr, and cation nutrients that are derived from the saprolite, a zone of silicate weathering, than shallow-rooted grass. A three-decade dendrochemical record reveals that reductions of wet precipitation drive deep-rooted plants to acquire cation nutrients from deeper saprolite or bedrock regions. Thus, the depth of cation nutrient acquisition by deep-rooted plant species at this site is tightly coupled with, and likely determined...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/14w4h314</guid>
      <pubDate>Mon, 30 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Li, Langlang</name>
      </author>
      <author>
        <name>Christensen, John N</name>
      </author>
      <author>
        <name>Bill, Markus</name>
        <uri>https://orcid.org/0000-0001-7002-2174</uri>
      </author>
      <author>
        <name>Dong, Wenming</name>
        <uri>https://orcid.org/0000-0003-2074-8887</uri>
      </author>
      <author>
        <name>Wu, Yuxin</name>
        <uri>https://orcid.org/0000-0002-6953-0179</uri>
      </author>
      <author>
        <name>Beutler, Curtis</name>
      </author>
      <author>
        <name>Sprenger, Matthias</name>
        <uri>https://orcid.org/0000-0003-1221-2767</uri>
      </author>
      <author>
        <name>Gulick, Brian W</name>
      </author>
      <author>
        <name>Bone, Sharon E</name>
      </author>
      <author>
        <name>Faybishenko, Boris</name>
        <uri>https://orcid.org/0000-0003-0085-8499</uri>
      </author>
      <author>
        <name>Sanders, John</name>
      </author>
      <author>
        <name>Chou, Chunwei</name>
      </author>
      <author>
        <name>Henderson, Amanda</name>
      </author>
      <author>
        <name>Bouskill, Nicholas J</name>
      </author>
      <author>
        <name>Williams, Kenneth H</name>
        <uri>https://orcid.org/0000-0002-3568-1155</uri>
      </author>
      <author>
        <name>Gilbert, Benjamin</name>
      </author>
    </item>
    <item>
      <title>Dataset about Warming Effects on Carbon Cycling and Greenhouse Gas Fluxes in Permafrost Ecosystems</title>
      <link>https://escholarship.org/uc/item/965986wq</link>
      <description>Field observations provide direct evidence of how does carbon cycling in permafrost ecosystems respond to climate change. This study provides a comprehensive dataset on the impact of warming on carbon cycling and greenhouse gas (GHG) fluxes in permafrost ecosystems. The dataset is extracted and integrated from 132 peer-reviewed studies with 1430 paired observations across eight major permafrost ecosystems, including Arctic and subarctic tundra and wetland, and alpine meadow, steppe, tundra and wetland. This dataset includes 17 variables from experiments conducted during the growing season, covering the plant and soil carbon pools, soil nitrogen pool, and GHG (i.e., CO2, CH4, and N2O) fluxes, among others. Background information on site climate conditions, vegetation and soil characteristics, and details of the warming experiments, including timing, methods, and warming magnitude, are also contained in the dataset. This dataset facilitates a comprehensive understanding of the impact...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/965986wq</guid>
      <pubDate>Fri, 27 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Bao, Tao</name>
      </author>
      <author>
        <name>Xu, Xiyan</name>
      </author>
      <author>
        <name>Jia, Gensuo</name>
      </author>
      <author>
        <name>Zhu, Xingru</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Yang, Yuanhe</name>
      </author>
    </item>
    <item>
      <title>A tale of two towers: comparing NEON and AmeriFlux data streams at Bartlett Experimental Forest</title>
      <link>https://escholarship.org/uc/item/5xb120jf</link>
      <description>Long-term ecological data are essential for detecting impacts of climate change and other global change factors, and for making informed predictions about future change. However, long-term measurements are rarely replicated at the site level, which raises questions about their representativeness. We used a multiscale approach to evaluate the agreement of parallel observations from AmeriFlux and NEON (National Ecological Observatory Network) towers at Bartlett Experimental Forest, New Hampshire, USA. The two towers are separated by a horizontal distance of 93 m. We focused our analysis on standard meteorological variables; fluxes of CO2, sensible heat, and latent heat measured by eddy covariance; and phenology derived from PhenoCam imagery. Results suggest excellent agreement between AmeriFlux and NEON in meteorology and phenology, and good agreement in fluxes at the half-hourly scale. However, large disagreements in CO2 and latent heat fluxes occurred at the annual scale, with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5xb120jf</guid>
      <pubDate>Thu, 19 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Liu, Yujie</name>
      </author>
      <author>
        <name>Stoy, Paul</name>
      </author>
      <author>
        <name>Chu, Housen</name>
        <uri>https://orcid.org/0000-0002-8131-4938</uri>
      </author>
      <author>
        <name>Hollinger, Dave Y</name>
      </author>
      <author>
        <name>Ollinger, Scott V</name>
      </author>
      <author>
        <name>Ouimette, Andrew P</name>
      </author>
      <author>
        <name>Durden, David J</name>
      </author>
      <author>
        <name>Sturtevant, Cove</name>
      </author>
      <author>
        <name>Lucas, Ben</name>
      </author>
      <author>
        <name>Richardson, Andrew D</name>
      </author>
    </item>
    <item>
      <title>Thermal stress in degraded forests in the Brazilian Amazon Arc of Deforestation</title>
      <link>https://escholarship.org/uc/item/3nb5z8gs</link>
      <description>Understanding thermal stress in tropical forests has taken on new urgency in light of accelerating climate change and expansion of deforestation and forest degradation. Degraded tropical forests in particular may be approaching critical temperature thresholds even more rapidly than intact forests, with implications for tree survival and ecosystem recovery. We investigate thermal stress in degraded tropical forests within the Brazilian Amazon Arc of Deforestation. Using land surface temperature data from the ECOsystem Spaceborne Thermal Radiometer Experiment on the international Space Station (ECOSTRESS), we compared canopy temperatures of intact, selectively logged, and burned forests in Feliz Natal, Mato Grosso, Brazil. Upper canopy temperatures in previously burned forests were 4.1% higher (mean = 36.5 °C) and 50.9% more variable compared to intact and logged forests, which showed remarkably similar temperature distributions (means of 34.9 °C and 35.1 °C, respectively). Modeled...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3nb5z8gs</guid>
      <pubDate>Fri, 13 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Cooley, Savannah S</name>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Csillik, Ovidiu</name>
      </author>
      <author>
        <name>Dias, André P</name>
      </author>
      <author>
        <name>Silgueiro, Vinicius</name>
      </author>
      <author>
        <name>Carvalho, Raquel</name>
      </author>
      <author>
        <name>Anderson, Doug</name>
      </author>
      <author>
        <name>Gilbreath, Micah</name>
      </author>
      <author>
        <name>Duffy, Paul</name>
      </author>
      <author>
        <name>Adami, Marcos</name>
      </author>
      <author>
        <name>Cawse-Nicholson, Kerry</name>
      </author>
      <author>
        <name>Menge, Duncan NL</name>
      </author>
    </item>
    <item>
      <title>Topography and functional traits shape the distribution of key shrub plant functional types in low-Arctic tundra</title>
      <link>https://escholarship.org/uc/item/660517p5</link>
      <description>The expansion of shrubs in the Arctic tundra fundamentally modifies land-atmosphere interactions. However, it remains unclear how shrub distribution and expansion differ across key species due to challenges with discriminating tundra plant species at regional scales. Here, we combined multi-scale, multi-platform remote sensing and &lt;i&gt;in situ&lt;/i&gt; trait measurements to elucidate the distribution patterns and primary controls of two representative deciduous-tall-shrub (DTS) genera, &lt;i&gt;Alnus&lt;/i&gt; and &lt;i&gt;Salix&lt;/i&gt;, in low-Arctic tundra. We show that topographic features were a key control on DTSs, creating heterogeneous, but predictable distributions of &lt;i&gt;Alnus&lt;/i&gt; and &lt;i&gt;Salix&lt;/i&gt; fractional cover (fCover). &lt;i&gt;Alnus&lt;/i&gt; was more tolerant of elevation and slope and was found on hilly uplands (slope &amp;gt;10°) within a specific elevational band (200-400 m above sea level [MSL]). In contrast, &lt;i&gt;Salix&lt;/i&gt; occurred at lower elevations (50-300 m MSL) on gentler slopes (3-10°) and required...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/660517p5</guid>
      <pubDate>Wed, 11 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Yang, Daryl</name>
      </author>
      <author>
        <name>Hantson, Wouter</name>
      </author>
      <author>
        <name>Davidson, Kenneth J</name>
      </author>
      <author>
        <name>Lamour, Julien</name>
      </author>
      <author>
        <name>Morrison, Bailey D</name>
      </author>
      <author>
        <name>Salmon, Verity G</name>
      </author>
      <author>
        <name>Zhang, Tianqi</name>
      </author>
      <author>
        <name>Ely, Kim S</name>
      </author>
      <author>
        <name>Miller, Charles E</name>
      </author>
      <author>
        <name>Hayes, Daniel J</name>
      </author>
      <author>
        <name>Baines, Stephen</name>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>Serbin, Shawn P</name>
      </author>
    </item>
    <item>
      <title>Tradeoffs between uniform land protection and biodiversity-specific land protection with &amp;lt;2 °C global warming</title>
      <link>https://escholarship.org/uc/item/6vn032vr</link>
      <description>Nearly 200 countries have pledged to conserve 30% of terrestrial ecosystems to stop the global biodiversity crisis. However, biodiversity is not uniformly distributed across countries. Adequately addressing this crisis requires a scientific basis for selecting protected land that considers both ecological benefits and impacts to humans. We use the global change analysis model to evaluate land use tradeoffs of four land protection cases under two climate cases. We find that biodiversity-specific land protection up to 39% globally can reduce land use constraints and food prices compared to protecting 30% of land uniformly in each country (’30 × 30’ initiative). Valuing terrestrial carbon for climate change mitigation reduces land conversion pressure and can complement protection strategies. Global impacts to agriculture of additional land protection are small, but regional impacts vary and may be considerable. Overall, biodiversity-specific land protection has greater potential...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6vn032vr</guid>
      <pubDate>Tue, 10 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>DiVittorio, Alan V</name>
      </author>
      <author>
        <name>Narayan, Kanishka B</name>
      </author>
      <author>
        <name>Westphal, Michael I</name>
      </author>
    </item>
    <item>
      <title>Radiative, Hydrologic, and Circulation Responses to Warming in Cess‐Potter Simulations Using the Global 3.25‐km SCREAM</title>
      <link>https://escholarship.org/uc/item/5t65r0x2</link>
      <description>Abstract Using the global 3.25‐km Simple Cloud Resolving E3SM Atmosphere Model (SCREAM 3&amp;nbsp;km), a pair of 13‐month Cess‐Potter simulations are performed to quantify the radiative feedbacks and the hydrologic and circulation responses to warming. Large‐scale aspects of SCREAM 3&amp;nbsp;km's top‐of‐atmosphere radiative fluxes, precipitation rates, and circulations are in good agreement with observations and reanalysis, with notable differences, including a drier lower free‐troposphere in the Tropics, reduced precipitation and humidity over the Tropical West Pacific, and poleward shifted Southern Hemisphere midlatitude jet. In response to warming, SCREAM 3&amp;nbsp;km predicts a total radiative feedback within the top 15% of the CMIP5 and CMIP6 models, which puts it substantially higher than the feedback reported by other kilometer‐scale models. SCREAM 3&amp;nbsp;km's high radiative feedback stems from a strongly positive shortwave cloud feedback, most prominent over the mid‐ and high‐latitudes....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5t65r0x2</guid>
      <pubDate>Tue, 10 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Terai, CR</name>
      </author>
      <author>
        <name>Keen, ND</name>
        <uri>https://orcid.org/0000-0003-3607-3554</uri>
      </author>
      <author>
        <name>Caldwell, PM</name>
      </author>
      <author>
        <name>Beydoun, H</name>
      </author>
      <author>
        <name>Bogenschutz, PA</name>
      </author>
      <author>
        <name>Chao, L‐W</name>
      </author>
      <author>
        <name>Hillman, BR</name>
      </author>
      <author>
        <name>Ma, H‐Y</name>
      </author>
      <author>
        <name>Zelinka, MD</name>
      </author>
      <author>
        <name>Bertagna, L</name>
      </author>
      <author>
        <name>Bradley, AM</name>
      </author>
      <author>
        <name>Clevenger, TC</name>
      </author>
      <author>
        <name>Donahue, AS</name>
      </author>
      <author>
        <name>Foucar, J</name>
      </author>
      <author>
        <name>Golaz, J‐C</name>
      </author>
      <author>
        <name>Guba, O</name>
      </author>
      <author>
        <name>Hannah, W</name>
      </author>
      <author>
        <name>Lee, J</name>
      </author>
      <author>
        <name>Lin, W</name>
      </author>
      <author>
        <name>Mahfouz, N</name>
      </author>
      <author>
        <name>Mülmenstädt, J</name>
      </author>
      <author>
        <name>Salinger, AG</name>
      </author>
      <author>
        <name>Singh, B</name>
      </author>
      <author>
        <name>Sreepathi, S</name>
      </author>
      <author>
        <name>Qin, Y</name>
      </author>
      <author>
        <name>Taylor, MA</name>
      </author>
      <author>
        <name>Ullrich, PA</name>
        <uri>https://orcid.org/0000-0003-4118-4590</uri>
      </author>
      <author>
        <name>Wu, W‐Y</name>
      </author>
      <author>
        <name>Yuan, X</name>
      </author>
      <author>
        <name>Zender, CS</name>
        <uri>https://orcid.org/0000-0003-0129-8024</uri>
      </author>
      <author>
        <name>Zhang, Y</name>
      </author>
    </item>
    <item>
      <title>Simulating Hurricane Katrina in the Simple Cloud‐Resolving E3SM Atmosphere Model v1</title>
      <link>https://escholarship.org/uc/item/1fq1f49x</link>
      <description>Abstract Climate models are important tools for advancing understanding and prediction of tropical cyclones (TCs). Traditional global climate models, however, do not have the ability to properly simulate TC intensity due to their coarse horizontal resolution. Regional models can be run at convection‐permitting resolutions, but these models are often strongly influenced by the data used in the lateral boundary forcing, and domain choice can have a large impact on the simulation. Cloud‐resolving global climate models have demonstrated great potential for realism in TC simulations, and in this study we focus specifically on the Simple Cloud‐Resolving Energy Exascale Earth System Model (E3SM) Atmosphere Model (SCREAM) v1 configuration. We evaluate SCREAMv1 against the observational record and the Weather Research and Forecasting (WRF) model run at a convection‐permitting resolution with Hurricane Katrina as our case study. We found that both models produced realistic simulations of...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1fq1f49x</guid>
      <pubDate>Fri, 6 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Bercos‐Hickey, Emily</name>
      </author>
      <author>
        <name>Mahfouz, Naser</name>
      </author>
      <author>
        <name>Keen, Noel D</name>
        <uri>https://orcid.org/0000-0003-3607-3554</uri>
      </author>
      <author>
        <name>Patricola‐DiRosario, Christina M</name>
      </author>
      <author>
        <name>Hannah, Walter M</name>
      </author>
      <author>
        <name>Beydoun, Hassan</name>
      </author>
      <author>
        <name>Wehner, Michael F</name>
        <uri>https://orcid.org/0000-0001-8423-7870</uri>
      </author>
      <author>
        <name>Lin, Wuyin</name>
      </author>
      <author>
        <name>Terai, Christopher R</name>
      </author>
      <author>
        <name>Hillman, Benjamin</name>
      </author>
    </item>
    <item>
      <title>Duration of super-emitting oil and gas methane sources</title>
      <link>https://escholarship.org/uc/item/93r2d7qw</link>
      <description>The duration of super-emitting events (&amp;gt;100 kg h-1) in oil and gas basins remains insufficiently understood but is key for reporting programs and mitigation strategies. Carbon Mapper conducted aerial surveys from April 30 to May 17, 2024, over the New Mexico Permian Basin, covering 276,000 wells, 1100 compressor stations, 175 gas processing plants, and 27,000 km of pipeline. We find over 500 super-emitting sources with 300 of these sources observed repeatedly across multiple days. We quantify total super emissions by integrating individual events with observationally constrained event durations (5.98 −14.7 Gg CH4) and compare to total emissions derived from basin average snapshots (12.7 ± 0.92 Gg CH4). This gap between emission estimates is reconciled through assumptions on missed detections, characteristic event duration, detection frequency, and diurnal variability. Emission events generally lasted for at least 2 hours, and a small subset of sources (18 total), persistently...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/93r2d7qw</guid>
      <pubDate>Thu, 26 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Cusworth, Daniel H</name>
      </author>
      <author>
        <name>Bon, Daniel M</name>
      </author>
      <author>
        <name>Varon, Daniel J</name>
      </author>
      <author>
        <name>Ayasse, Alana K</name>
      </author>
      <author>
        <name>Asner, Gregory P</name>
      </author>
      <author>
        <name>Heckler, Joseph</name>
      </author>
      <author>
        <name>Sherwin, Evan D</name>
        <uri>https://orcid.org/0000-0003-2180-4297</uri>
      </author>
      <author>
        <name>Biraud, Sebastien C</name>
      </author>
      <author>
        <name>Duren, Riley M</name>
      </author>
    </item>
    <item>
      <title>A Statistician’s Overview of Physics-Informed Neural Networks for Spatio-Temporal Data</title>
      <link>https://escholarship.org/uc/item/7590w4xd</link>
      <description>A Statistician’s Overview of Physics-Informed Neural Networks for Spatio-Temporal Data</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7590w4xd</guid>
      <pubDate>Tue, 24 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Wikle, Christopher K</name>
      </author>
      <author>
        <name>North, Joshua</name>
        <uri>https://orcid.org/0000-0001-7631-8021</uri>
      </author>
      <author>
        <name>Gopalan, Giri</name>
      </author>
      <author>
        <name>Yoo, Myungsoo</name>
      </author>
    </item>
    <item>
      <title>Long-term soil warming decreases fungal biomass and alters fungal but not bacterial communities in a temperate forest</title>
      <link>https://escholarship.org/uc/item/0nr491wg</link>
      <description>Long-term soil warming may alter microbial community structure and functioning in forest soils, thereby affecting carbon and nutrient cycling processes. We examined the effects of &amp;gt;14 years of soil warming (+4°C during snow-free seasons) on the fungal biomass marker ergosterol, and on fungal and bacterial communities in a spruce dominated mountain forest in the Austrian Alps. Soil warming decreased ergosterol, and the ergosterol-to-microbial biomass carbon (MBC) ratio at 0-10 and 10-20 cm soil depth, with a stronger decline in ergosterol, indicating a higher sensitivity of fungi than bacteria to long-term warming. Warming also shifted the fungal community at both soil depths, favoring Boletus luridus, an ectomycorrhizal (ECM) fungus, which emerged as the dominant OTU in warmed plots. The dominance of ECM over saprotrophic fungi (SAP) under warming at topsoil likely resulted from increased fine root production and enhanced competition for substrates and nutrients. Bacterial...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0nr491wg</guid>
      <pubDate>Tue, 24 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Ullah, Mohammad Rahmat</name>
      </author>
      <author>
        <name>Kengdo, Steve Kwatcho</name>
      </author>
      <author>
        <name>Peršoh, Derek</name>
      </author>
      <author>
        <name>Tian, Ye</name>
      </author>
      <author>
        <name>Heinzle, Jakob</name>
      </author>
      <author>
        <name>Malo, Carolina Urbina</name>
      </author>
      <author>
        <name>Shi, Chupei</name>
      </author>
      <author>
        <name>Lueders, Tillmann</name>
      </author>
      <author>
        <name>Poll, Christian</name>
      </author>
      <author>
        <name>Wanek, Wolfgang</name>
      </author>
      <author>
        <name>Schindlbacher, Andreas</name>
      </author>
      <author>
        <name>Borken, Werner</name>
      </author>
    </item>
    <item>
      <title>Water availability modulates maximum canopy heights of low-elevation Amazonian second-growth forests</title>
      <link>https://escholarship.org/uc/item/7xj0c3rz</link>
      <description>Tropical second-growth forests of the Amazon sequester large amounts of carbon and are important carbon sinks, contributing substantially to climate change mitigation, biodiversity conservation, and providing crucial ecosystem services. Deforestation due to selective logging and shifting cultivation is expanding second-growth forest areas in tropical forest regions, which if well managed, regenerate rapidly over time. Maximum forest canopy height is an important metric of biomass and carbon accumulation in second-growth forests and is strongly influenced by water availability. The water limitation hypothesis explains the positive influence of water availability on maximum tree heights and has been examined and demonstrated at a small-scale using field data, and at a global scale, with limited accuracy, using remote sensing data in tropical ecosystems. However, this hypothesis concerning maximum canopy height has not been much studied at regional and national scales for tropical...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7xj0c3rz</guid>
      <pubDate>Tue, 17 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Mohan, Midhun</name>
      </author>
      <author>
        <name>Pastorello, Gilberto Z</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Adrah, Esmaeel</name>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Ewane, Ewane Basil</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Csillik, Ovidiu</name>
      </author>
      <author>
        <name>Ferraz, Antonio</name>
      </author>
      <author>
        <name>Dutta Roy, Abhilash</name>
      </author>
      <author>
        <name>Meng, Lin</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>The Influence of African Easterly Waves on Atlantic Tropical Cyclone Tracks and Landfall in Large Ensembles</title>
      <link>https://escholarship.org/uc/item/9ck1c2bq</link>
      <description>Abstract African easterly waves (AEWs) are an important precursor or “seed” for Atlantic tropical cyclones (TCs), with 60%–80% of major hurricanes observed to originate from AEWs. However, climate model simulations indicate that AEWs are not necessary to maintain annual Atlantic TC frequency. Furthermore, small ensembles suggest that AEWs may impact the spatial distribution and landfall of Atlantic TCs. Here, we investigated the influence of AEWs on the spatial distribution of Atlantic TC tracks and landfall using 50‐member ensembles of TC‐permitting regional model simulations for five hurricane seasons characterized by different levels of TC activity. The control simulations are seasonal hindcasts in which AEWs were prescribed through the eastern lateral boundary condition using reanalysis. In the experiments, we suppressed AEWs by applying a 2–10&amp;nbsp;day filter to the eastern lateral boundary condition. In response to AEW suppression, we discovered statistically significant...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9ck1c2bq</guid>
      <pubDate>Wed, 11 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Kouski, Ronald H</name>
      </author>
      <author>
        <name>Patricola‐DiRosario, Christina M</name>
      </author>
      <author>
        <name>Bercos‐Hickey, Emily</name>
      </author>
      <author>
        <name>Risser, Mark D</name>
        <uri>https://orcid.org/0000-0003-1956-1783</uri>
      </author>
    </item>
    <item>
      <title>Characterizing the vertical structure of forests in the Brazilian Amazon</title>
      <link>https://escholarship.org/uc/item/76q799kj</link>
      <description>Little is known about the structure of tropical forests despite its critical role in the provisioning of ecosystem services. Here we assess the vertical structure of forests in the Brazilian Amazon with a large-scale airborne LiDAR dataset. We show that fire has greater impact in the lowest forest strata, differently from selective logging and windthrow. We also find that secondary forests quickly recover or even exceed reference areas at the 1-10 m height stratum but that full recovery for the 20-30 m height stratum has not been achieved even after 35 years. Our modeling results suggest that proximity to roads, elevation, precipitation, soil pH, and proportion of sand in the soil are the most important predictors of forest structure. Finally, we identify 5 forest structural types (FSTs) and use them to visualize the spatial distribution of forest structure. This study provides important information for forest monitoring, management, and conservation.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/76q799kj</guid>
      <pubDate>Tue, 10 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Valle, Denis</name>
      </author>
      <author>
        <name>Haneda, Leo</name>
      </author>
      <author>
        <name>Brack, Ismael Verrastro</name>
      </author>
      <author>
        <name>Ometto, Jean</name>
      </author>
      <author>
        <name>Csillik, Ovidiu</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Almeida, Danilo</name>
      </author>
    </item>
    <item>
      <title>Microbial inoculants and invasions: a call to action</title>
      <link>https://escholarship.org/uc/item/9vm3k68s</link>
      <description>Microbial inoculants are increasingly used for beneficial purposes in agriculture, bioremediation, and medicine, but they can carry risks of generating invasive microbes. Here, we present a roadmap for guarding against these invasions, proposing developing (i) coherent mechanistic understandings of how microbial inoculants can effect invasions, (ii) predictive models forecasting microbial invasion risks, and (iii) effective management strategies. To guide mechanistic understandings, we distill 17 guiding hypotheses. For predictive modeling, we highlight data collection needs and qualitative approaches. For management strategies, we stress the importance of accurately weighing the risks against benefits. The unified approach presented here provides a route toward an effective research and management infrastructure for microbial inoculants in order to avoid potentially catastrophic microbial invasions.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9vm3k68s</guid>
      <pubDate>Wed, 28 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Ladau, Joshua</name>
      </author>
      <author>
        <name>Fahimipour, Ashkaan K</name>
      </author>
      <author>
        <name>Newcomer, Michelle E</name>
        <uri>https://orcid.org/0000-0001-5138-9026</uri>
      </author>
      <author>
        <name>Brown, James B</name>
      </author>
      <author>
        <name>Vora, Gary J</name>
      </author>
      <author>
        <name>Melby, Melissa K</name>
      </author>
      <author>
        <name>Maresca, Julia A</name>
      </author>
    </item>
    <item>
      <title>The Global Spectra-Trait Initiative: A database of paired leaf spectroscopy and functional traits associated with leaf photosynthetic capacity</title>
      <link>https://escholarship.org/uc/item/9kn473ng</link>
      <description>Abstract. Accurate assessment of leaf functional traits is crucial for a diverse range of applications from crop phenotyping to parameterizing global climate models. Leaf reflectance spectroscopy offers a promising avenue to advance ecological and agricultural research by complementing traditional, time-consuming gas exchange measurements. However, the development of robust hyperspectral models for predicting leaf photosynthetic capacity and associated traits from reflectance data has been hindered by limited data availability across species and environments. Here we introduce the Global Spectra-Trait Initiative (GSTI), a collaborative repository of paired leaf hyperspectral and gas exchange measurements from diverse ecosystems. The GSTI repository currently encompasses over 7500 observations from 397 species and 41 sites gathered from 36 published and unpublished studies, thereby offering a key resource for developing and validating hyperspectral models of leaf photosynthetic...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9kn473ng</guid>
      <pubDate>Tue, 27 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Lamour, Julien</name>
      </author>
      <author>
        <name>Serbin, Shawn P</name>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>Acebron, Kelvin T</name>
      </author>
      <author>
        <name>Ainsworth, Elizabeth</name>
      </author>
      <author>
        <name>Albert, Loren P</name>
      </author>
      <author>
        <name>Alonzo, Michael</name>
      </author>
      <author>
        <name>Anderson, Jeremiah</name>
      </author>
      <author>
        <name>Atkin, Owen K</name>
      </author>
      <author>
        <name>Barbier, Nicolas</name>
      </author>
      <author>
        <name>Barnes, Mallory L</name>
      </author>
      <author>
        <name>Bernacchi, Carl J</name>
      </author>
      <author>
        <name>Besson, Ninon</name>
      </author>
      <author>
        <name>Burnett, Angela C</name>
      </author>
      <author>
        <name>Caplan, Joshua S</name>
      </author>
      <author>
        <name>Chave, Jérôme</name>
      </author>
      <author>
        <name>Cheesman, Alexander W</name>
      </author>
      <author>
        <name>Clocher, Ilona</name>
      </author>
      <author>
        <name>Coast, Onoriode</name>
      </author>
      <author>
        <name>Coste, Sabrina</name>
      </author>
      <author>
        <name>Croft, Holly</name>
      </author>
      <author>
        <name>Cui, Boya</name>
      </author>
      <author>
        <name>Dauvissat, Clément</name>
      </author>
      <author>
        <name>Davidson, Kenneth J</name>
      </author>
      <author>
        <name>Doughty, Christopher</name>
      </author>
      <author>
        <name>Ely, Kim S</name>
      </author>
      <author>
        <name>Evans, John R</name>
      </author>
      <author>
        <name>Féret, Jean-Baptiste</name>
      </author>
      <author>
        <name>Filella, Iolanda</name>
      </author>
      <author>
        <name>Fortunel, Claire</name>
      </author>
      <author>
        <name>Fu, Peng</name>
      </author>
      <author>
        <name>Furbank, Robert T</name>
      </author>
      <author>
        <name>Garcia, Maquelle</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Guan, Kaiyu</name>
      </author>
      <author>
        <name>Guo, Zhengfei</name>
      </author>
      <author>
        <name>Heckmann, David</name>
      </author>
      <author>
        <name>Heuret, Patrick</name>
      </author>
      <author>
        <name>Isaac, Marney</name>
      </author>
      <author>
        <name>Kothari, Shan</name>
      </author>
      <author>
        <name>Kumagai, Etsushi</name>
      </author>
      <author>
        <name>Kyaw, Thu Ya</name>
      </author>
      <author>
        <name>Liu, Liangyun</name>
      </author>
      <author>
        <name>Liu, Lingli</name>
      </author>
      <author>
        <name>Liu, Shuwen</name>
      </author>
      <author>
        <name>Llusià, Joan</name>
      </author>
      <author>
        <name>Magney, Troy</name>
      </author>
      <author>
        <name>Maréchaux, Isabelle</name>
      </author>
      <author>
        <name>Martin, Adam R</name>
      </author>
      <author>
        <name>Meacham-Hensold, Katherine</name>
      </author>
      <author>
        <name>Montes, Christopher M</name>
      </author>
      <author>
        <name>Ogaya, Romà</name>
      </author>
      <author>
        <name>Ojo, Joy</name>
      </author>
      <author>
        <name>Oliveira, Regison</name>
      </author>
      <author>
        <name>Paquette, Alain</name>
      </author>
      <author>
        <name>Peñuelas, Josep</name>
      </author>
      <author>
        <name>Placido, Antonia Debora</name>
      </author>
      <author>
        <name>Posada, Juan M</name>
      </author>
      <author>
        <name>Qian, Xiaojin</name>
      </author>
      <author>
        <name>Renninger, Heidi J</name>
      </author>
      <author>
        <name>Rodriguez-Caton, Milagros</name>
      </author>
      <author>
        <name>Rojas-González, Andrés</name>
      </author>
      <author>
        <name>Schlüter, Urte</name>
      </author>
      <author>
        <name>Sellan, Giacomo</name>
      </author>
      <author>
        <name>Siegert, Courtney M</name>
      </author>
      <author>
        <name>Silva-Perez, Viridiana</name>
      </author>
      <author>
        <name>Song, Guangqin</name>
      </author>
      <author>
        <name>Southwick, Charles D</name>
      </author>
      <author>
        <name>Souza, Daisy C</name>
      </author>
      <author>
        <name>Stahl, Clément</name>
      </author>
      <author>
        <name>Su, Yanjun</name>
      </author>
      <author>
        <name>Sujeeun, Leeladarshini</name>
      </author>
      <author>
        <name>Ting, To-Chia</name>
      </author>
      <author>
        <name>Vasquez, Vicente</name>
      </author>
      <author>
        <name>Vijayakumar, Amrutha</name>
      </author>
      <author>
        <name>Vilas-Boas, Marcelo</name>
      </author>
      <author>
        <name>Wang, Diane R</name>
      </author>
      <author>
        <name>Wang, Sheng</name>
      </author>
      <author>
        <name>Wang, Han</name>
      </author>
      <author>
        <name>Wang, Jing</name>
      </author>
      <author>
        <name>Wang, Xin</name>
      </author>
      <author>
        <name>Weber, Andreas PM</name>
      </author>
      <author>
        <name>Wong, Christopher YS</name>
      </author>
      <author>
        <name>Wu, Jin</name>
      </author>
      <author>
        <name>Wu, Fengqi</name>
      </author>
      <author>
        <name>Wu, Shengbiao</name>
      </author>
      <author>
        <name>Yan, Zhengbing</name>
      </author>
      <author>
        <name>Yang, Dedi</name>
      </author>
      <author>
        <name>Zhao, Yingyi</name>
      </author>
    </item>
    <item>
      <title>Future implications of enhanced hydroclimate variability and reduced snowpack on California’s water resources</title>
      <link>https://escholarship.org/uc/item/7gd863wq</link>
      <description>The Sierra Nevada snowpack, which supplies sixty percent of California’s consumptive water use, is under threat due to anthropogenic climate change. While previous studies have examined the impacts of climate change on mountain snowpack in the Sierra Nevada and across the Western US, few have quantified the risks to monthly irrigation water resources posed by shifting hydroclimate patterns and declining snowmelt runoff. Because they use coarse-resolution models, existing global-scale studies lack regional specificity, while existing regional studies rely on statistical or dynamical ‘downscaling’ of coarse-resolution global models. We use a new simulation of the variable resolution Community Earth System Model 2, which provides high spatiotemporal resolution estimates (14 km horizontal grid spacing, daily-to-hourly outputs) of California’s historical and future hydroclimate. We leverage the US Geological Survey’s recent irrigation water use reanalysis to evaluate basin-scale irrigation...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7gd863wq</guid>
      <pubDate>Tue, 27 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Beltran-Peña, Areidy</name>
      </author>
      <author>
        <name>Rhoades, Alan</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Burakowski, Elizabeth</name>
      </author>
      <author>
        <name>Girotto, Manuela</name>
      </author>
      <author>
        <name>Michalak, Anna M</name>
      </author>
      <author>
        <name>Diffenbaugh, Noah S</name>
      </author>
      <author>
        <name>Inda-Diaz, Hector</name>
      </author>
      <author>
        <name>D’Odorico, Paolo</name>
      </author>
    </item>
    <item>
      <title>High-resolution mountain topography can inform global snow vulnerability estimates</title>
      <link>https://escholarship.org/uc/item/73f8271p</link>
      <description>Snow is changing globally. Computationally intensive snow reanalysis products and downscaled climate model projections allow for the estimation of historical and projected changes in snow over ∼4–10 km resolutions, but these resolutions are coarse relative to the scales needed for water supply and flood planning. Fine-scale digital elevation models (DEMs) are widely available but are underutilized to make first-order assessments of snow vulnerability. Here, we leverage DEMs at a 7.5 arc s (∼250 m) resolution, combining these with historical freezing level height estimates from ERA-5 to derive estimates of changes in the snow-receiving area (SRA) and its variability across global mountain ranges. Results show estimated SRA declines in 29% (1.9 million km2) of the global mountain area from 1982–2020; 66% of the mountainous areas had no change over the historical period. At +1.5 °C of warming relative to the pre-industrial control, global mountain SRA would decline by 9.5% (1.0 million...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/73f8271p</guid>
      <pubDate>Tue, 27 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Marshall, Adrienne M</name>
      </author>
      <author>
        <name>Abatzoglou, John T</name>
        <uri>https://orcid.org/0000-0001-7599-9750</uri>
      </author>
      <author>
        <name>Koshkin, Arielle</name>
      </author>
      <author>
        <name>Rhoades, Alan</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
    </item>
    <item>
      <title>Multi-omics reveals nitrogen dynamics associated with soil microbial blooms during snowmelt</title>
      <link>https://escholarship.org/uc/item/36q1s0ff</link>
      <description>Snowmelt triggers a soil microbial bloom and crash that affects nitrogen (N) export in high-elevation watersheds. The mechanisms underlying these microbial dynamics are uncertain, making soil nitrogen processes difficult to predict as snowpack declines globally. Here, integration of genome-resolved metagenomics, metatranscriptomics and metabolomics in a high-elevation watershed revealed ecologically distinct soil microorganisms linked across the snowmelt time-period by their unique nitrogen cycling capacities. The molecular properties and transformations of dissolved organic N suggested that degradation or recycling of microbial biomass provided N for biosynthesis during the microbial bloom. Winter-adapted Bradyrhizobia spp. oxidized amino acids anaerobically and had the highest gene expression for denitrification during the microbial bloom. A pulse of nitrate was driven by spring-adapted Nitrososphaerales after snowmelt, but dissimilatory nitrate reduction to ammonia (DNRA) gene...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/36q1s0ff</guid>
      <pubDate>Tue, 27 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Sorensen, Patrick O</name>
        <uri>https://orcid.org/0000-0002-0558-2789</uri>
      </author>
      <author>
        <name>Karaoz, Ulas</name>
        <uri>https://orcid.org/0000-0002-8238-6757</uri>
      </author>
      <author>
        <name>Beller, Harry R</name>
        <uri>https://orcid.org/0000-0001-9637-3650</uri>
      </author>
      <author>
        <name>Bill, Markus</name>
        <uri>https://orcid.org/0000-0001-7002-2174</uri>
      </author>
      <author>
        <name>Bouskill, Nicholas J</name>
      </author>
      <author>
        <name>Banfied, Jillian F</name>
      </author>
      <author>
        <name>Chu, Rosalie K</name>
      </author>
      <author>
        <name>Hoyt, David W</name>
      </author>
      <author>
        <name>Eder, Elizabeth</name>
      </author>
      <author>
        <name>Eloe-Fadrosh, Emiley</name>
        <uri>https://orcid.org/0000-0002-8162-1276</uri>
      </author>
      <author>
        <name>Sharrar, Allison</name>
      </author>
      <author>
        <name>Tfaily, Malak M</name>
      </author>
      <author>
        <name>Toyoda, Jason</name>
      </author>
      <author>
        <name>Tolic, Nikola</name>
      </author>
      <author>
        <name>Wang, Shi</name>
        <uri>https://orcid.org/0000-0002-2408-2544</uri>
      </author>
      <author>
        <name>Wong, Allison R</name>
      </author>
      <author>
        <name>Williams, Kenneth H</name>
        <uri>https://orcid.org/0000-0002-3568-1155</uri>
      </author>
      <author>
        <name>Zhong, Yangquanwei</name>
      </author>
      <author>
        <name>Brodie, Eoin L</name>
        <uri>https://orcid.org/0000-0002-8453-8435</uri>
      </author>
    </item>
    <item>
      <title>Agile Allocation in the Tundra: A Single Growing Season of Warming Increases Nutrient Availability While Decreasing Fine-Root Length</title>
      <link>https://escholarship.org/uc/item/0w5991r6</link>
      <description>The majority of plant biomass is located belowground in Arctic ecosystems and plant roots are responsible for the uptake of the nutrients that constrain plant growth in these infertile ecosystems. Despite performing a crucial role connecting primary producers to the soil, roots are relatively understudied in the Arctic and their functional response to a rapidly warming and increasingly variable climate is unknown. We assessed whether one growing season with elevated temperatures would have an impact on nutrient uptake and allocation by applying a warming technique that increased daily air temperatures by 3.2&amp;nbsp;°C. Destructive sampling was performed at the peak of the growing season to quantify biomass pools of carbon (C) and nitrogen (N), root traits, and uptake of a 15N tracer (15NH4+) for the dominant plant species, Arctagrostis latifolia. We found that soil nutrient availability increased with short-term warming, but A. latifolia NH4+ uptake remained unchanged. Fine-root...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0w5991r6</guid>
      <pubDate>Tue, 27 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Salmon, Verity G</name>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>Childs, Joanne</name>
      </author>
      <author>
        <name>Ely, Kim S</name>
      </author>
      <author>
        <name>Serbin, Shawn</name>
      </author>
      <author>
        <name>Spencer, Breann</name>
      </author>
      <author>
        <name>Lewin, Keith</name>
      </author>
      <author>
        <name>Norby, Richard J</name>
      </author>
      <author>
        <name>Iversen, Colleen M</name>
      </author>
    </item>
    <item>
      <title>Representing Soil Microbial Dynamics and Organo‐Mineral Interactions in the E3SM Land Model (ELM‐ReSOM)</title>
      <link>https://escholarship.org/uc/item/5p27k0vx</link>
      <description>Abstract  Explicit representation of soil microbial processes and interactions with biotic and abiotic processes in Earth System Models (ESMs) remains limited, despite their importance in biogeochemical cycles. To address this gap, which hinders prediction of global biogeochemial cycling and responses to atmospheric conditions, we integrated a microbe‐ and mineral‐surface‐explicit model, the Reaction‐network‐based model of soil organic matter and Microbes (ReSOM), into the Energy Exascale ESM (E3SM) land model (ELM). Here, we describe ELM‐ReSOM and show a case study at a conifer forest in California. ELM‐ReSOM accurately simulated surface CO 2 fluxes and SOM stocks, demonstrating improved representations of microbial and mineral interactions compared to the default ELM. We examined ELM‐ReSOM sensitivity to microbial traits, enzyme properties, and organo‐mineral interactions. Microbial traits such as the maximum mortality rate, transporter‐density scaling factor, and maximum monomer...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5p27k0vx</guid>
      <pubDate>Thu, 22 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Tao, Jing</name>
        <uri>https://orcid.org/0000-0002-4009-2910</uri>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Tang, Jinyun</name>
        <uri>https://orcid.org/0000-0002-4792-1259</uri>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Pegoraro, Elaine L</name>
      </author>
      <author>
        <name>Castanha, Cristina</name>
        <uri>https://orcid.org/0000-0001-7327-5169</uri>
      </author>
      <author>
        <name>Abramoff, Rose Z</name>
      </author>
      <author>
        <name>Torn, Margaret S</name>
        <uri>https://orcid.org/0000-0002-8174-0099</uri>
      </author>
    </item>
    <item>
      <title>Earlier snowmelt increases the strength of the carbon sink in montane meadows unequally across the growing season</title>
      <link>https://escholarship.org/uc/item/810693t1</link>
      <description>Abstract    Warming temperatures are changing winters, leading to earlier snowmelt. This shift can lead to an earlier and potentially longer growing season, which in turn may affect various plant‐mediated ecosystem functions. Despite its relevance in the carbon cycle, we still know little about how earlier snowmelt impacts the carbon balance in ecosystems over the growing season, for example, does it only shift phenology, or does it affect the overall carbon uptake? Most studies rely on interannual variability in snowmelt timing, making it difficult to isolate snowmelt effects from other confounding variables, for example, temperature and moisture anomalies. To address this uncertainty, we investigated how experimentally advancing snowmelt affects the carbon cycling of montane meadows across the growing season.   We experimentally advanced the snowmelt date in a montane meadow by approximately 12 days and collected data every 2 weeks throughout the growing season, including net...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/810693t1</guid>
      <pubDate>Wed, 21 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Vought, Olivia K</name>
      </author>
      <author>
        <name>Kivlin, Stephanie N</name>
      </author>
      <author>
        <name>Shulman, Hannah B</name>
      </author>
      <author>
        <name>Sorensen, Patrick O</name>
        <uri>https://orcid.org/0000-0002-0558-2789</uri>
      </author>
      <author>
        <name>Inouye, David W</name>
      </author>
      <author>
        <name>Ibáñez, Inés</name>
      </author>
      <author>
        <name>Falb, Peter</name>
      </author>
      <author>
        <name>Rand, Karin</name>
      </author>
      <author>
        <name>Classen, Aimée T</name>
      </author>
    </item>
    <item>
      <title>Hydrology controls thermokarst and alters carbon cycling and methane emissions in peatlands near the southern limit of permafrost</title>
      <link>https://escholarship.org/uc/item/6h00g9gp</link>
      <description>Permafrost peatlands store vast amounts of frozen carbon across northern landscapes. When ground ice melts, surface subsidence produces thermokarst landforms that expand wetlands at the edges of permafrost plateaus. Thermokarst represents an accelerating climate feedback, but uncertainties remain about how ground ice, hydrology, and vegetation interact to shape landscape change and carbon fluxes. We extended the process-based model ecosys to simulate thermokarst dynamics in laterally coupled 2D transects at a well-characterized boreal peatland site in Canada’s Northwest Territories. After benchmarking against site observations, we varied ground ice content and hydrologic boundary conditions across ranges typical near the southern permafrost limit. Simulations revealed distinct degradation regimes governed by the elevation difference between the frost table and the external water table. Rates of lateral retreat, the thaw-driven encroachment of wetlands into adjacent plateaus, ranged...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6h00g9gp</guid>
      <pubDate>Wed, 21 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Shirley, Ian</name>
      </author>
      <author>
        <name>Mekonnen, Zelalem</name>
        <uri>https://orcid.org/0000-0002-2647-0671</uri>
      </author>
      <author>
        <name>Grant, Robert</name>
      </author>
      <author>
        <name>Detto, Matteo</name>
      </author>
      <author>
        <name>Gosselin, Gabriel Hould</name>
      </author>
      <author>
        <name>Talbot, Julie</name>
      </author>
      <author>
        <name>Sonnentag, Oliver</name>
      </author>
      <author>
        <name>Dafflon, Baptiste</name>
        <uri>https://orcid.org/0000-0001-9871-5650</uri>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
    </item>
    <item>
      <title>Crop diversification improves water-use efficiency and regional water sustainability</title>
      <link>https://escholarship.org/uc/item/1fs9d7kw</link>
      <description>As global water scarcity intensifies, identifying agricultural practices that enhance sustainable water management is critical. Temporal crop diversification-rotating multiple species over time-has been proposed to improve soil health and water retention based on field-scale experiments. However, widespread adoption remains limited on farms, in part due to unverified benefits at larger scales. Here, we assess the influence of crop diversification on agricultural water-use efficiency (WUE, ratio of gross primary productivity to evapotranspiration) along a spectrum of monoculture to complex species rotations in California. Leveraging new high-resolution remote sensing datasets, we show that crop diversification is a key driver of agricultural WUE, and increasing the number of species planted in the previous 6 years from two to four increases WUE by ∼20% after accounting for differences between crops. Our results provide spatially explicit, large-scale quantification of crop diversification’s...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1fs9d7kw</guid>
      <pubDate>Wed, 21 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Ruehr, Sophie</name>
      </author>
      <author>
        <name>Bassiouni, Maoya</name>
        <uri>https://orcid.org/0000-0001-5795-9894</uri>
      </author>
      <author>
        <name>Kang, Yanghui</name>
      </author>
      <author>
        <name>Socolar, Yvonne</name>
      </author>
      <author>
        <name>Magney, Troy</name>
        <uri>https://orcid.org/0000-0002-9033-0024</uri>
      </author>
      <author>
        <name>Keenan, Trevor F</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
    </item>
    <item>
      <title>High-resolution national mapping of natural gas composition substantially updates methane leakage impacts</title>
      <link>https://escholarship.org/uc/item/9nz8n48r</link>
      <description>Methane is emitted from oil and gas operations alongside heavier hydrocarbons and non-hydrocarbon gases, shaping emissions management decision-making, including air quality impacts. Yet, most assessments assume fixed gas composition, overlooking significant spatial and temporal variations. Here, we generate a high-resolution, data-driven map of natural gas composition across the United States, reconstructing methane, heavier hydrocarbons, and non-hydrocarbon species using spatio-temporal interpolation and oil-and-gas production patterns. Our approach is able to reduce composition prediction errors by 39% in terms of Mean Absolute Error (MAE) compared to standard techniques and reveals that methane loss rates have been underestimated by more than 50% in some regions. Beyond methane, we uncover substantial variability in co-emitted gases, exposing blind spots in current emissions inventories and emissions management frameworks. Our work enables more accurate emissions assessments,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9nz8n48r</guid>
      <pubDate>Wed, 14 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Burdeau, Philippine M</name>
      </author>
      <author>
        <name>Sherwin, Evan D</name>
        <uri>https://orcid.org/0000-0003-2180-4297</uri>
      </author>
      <author>
        <name>Biraud, Sébastien C</name>
      </author>
      <author>
        <name>Berman, Elena SF</name>
      </author>
      <author>
        <name>Brandt, Adam R</name>
      </author>
    </item>
    <item>
      <title>Nutrient limitation shapes functional traits of mycorrhizal fungi and phosphorus-cycling bacteria across an elevation gradient</title>
      <link>https://escholarship.org/uc/item/35n0m2rk</link>
      <description>In nutrient-limited high-elevation ecosystems, plants rely on arbuscular mycorrhizal (AM) fungi to provide mineral phosphorus (P) in the form of phosphate (PO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;3-&lt;/sup&gt;). AM fungi gather these nutrients from phosphorus-cycling bacteria (PCBs) that can mineralize PO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;3-&lt;/sup&gt; from organic matter and solubilize mineral-bound P. How climate, soil factors, and nutrient limitation influence AM fungi and PCB assembly remains unclear. We collected soil from montane meadows across a 1,000-m elevation gradient on three replicate mountainsides and analyzed AM fungal marker genes, P-cycling genes from shotgun metagenomes, and edaphic measurements. High-elevation soils had nearly 50-fold less soil PO₄³⁻ and 60% more AM fungal hyphae than low-elevation soils. AM fungal turnover was linked to changes in pH, organic carbon, and PO₄³&lt;sup&gt;-&lt;/sup&gt;. The composition of 198 P-cycling genes was influenced by the AM fungal community structure. Drivers of individual PCB...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/35n0m2rk</guid>
      <pubDate>Wed, 14 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Shulman, Hannah B</name>
      </author>
      <author>
        <name>Pyle, Jessica AM</name>
      </author>
      <author>
        <name>Classen, Aimée T</name>
      </author>
      <author>
        <name>Inouye, David W</name>
      </author>
      <author>
        <name>Simberloff, Ruth</name>
      </author>
      <author>
        <name>Sorensen, Patrick O</name>
        <uri>https://orcid.org/0000-0002-0558-2789</uri>
      </author>
      <author>
        <name>Thomas, William</name>
      </author>
      <author>
        <name>Rudgers, Jennifer A</name>
      </author>
      <author>
        <name>Kivlin, Stephanie N</name>
      </author>
    </item>
    <item>
      <title>Observations and modeling reveal that heatwaves reduce photosynthesis, plant carbon reserves, and net carbon uptake</title>
      <link>https://escholarship.org/uc/item/014942qn</link>
      <description>Heatwaves threaten ecosystem carbon balances, yet the mechanisms driving short-term carbon flux responses remain poorly understood. Here, integrating high-frequency eddy covariance (EC) data from 140 global flux tower sites (872 site-years) with detailed process-based modeling, we examine ecosystem responses during and immediately after heatwaves. We show that heatwaves caused a −40% (range [−29%, −128%]) reduction in net ecosystem productivity (NEP) compared to pre-heatwave values, with this reduction persisting over the following two weeks (−38% range [+3%, −154%]). We attributed NEP decreases to photosynthesis decreases more than to ecosystem respiration (RE) increases. Forest sites had greater NEP decreases during heatwaves than non-forest sites, but remained carbon sinks afterwards, indicating resilience. Our modeling analysis of extreme heatwaves at selected EC sites shows that decreased photosynthesis, increased maintenance respiration, and decreased plant non-structural...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/014942qn</guid>
      <pubDate>Wed, 14 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Mekonnen, Zelalem A</name>
        <uri>https://orcid.org/0000-0002-2647-0671</uri>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Still, Christopher J</name>
      </author>
      <author>
        <name>Grant, Robert F</name>
      </author>
    </item>
    <item>
      <title>Using Machine Learning to Discover Parsimonious and Physically‐Interpretable Representations of Catchment‐Scale Rainfall‐Runoff Dynamics</title>
      <link>https://escholarship.org/uc/item/7jf0c27n</link>
      <description>Abstract Due largely to challenges associated with physical interpretability of machine learning (ML) methods, and because model interpretability is key to credibility in management applications, many scientists and practitioners are hesitant to discard traditional physical‐conceptual modeling approaches despite their poorer predictive performance. Here, we examine how to develop parsimonious minimally‐optimal representations that can facilitate better insight regarding system functioning. The term “minimally‐optimal” indicates that the desired outcome can be achieved with the smallest possible effort and resources, while “parsimony” is widely held to support understanding. Accordingly, we suggest that ML‐based modeling should use computational units that are inherently physically‐interpretable, and explore how generic network architectures comprised of Mass‐Conserving‐Perceptron can be used to model dynamical systems in a physically‐interpretable manner. In the context of spatially‐lumped...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7jf0c27n</guid>
      <pubDate>Tue, 13 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Wang, Yuan‐Heng</name>
        <uri>https://orcid.org/0000-0002-9360-6639</uri>
      </author>
      <author>
        <name>Gupta, Hoshin V</name>
      </author>
    </item>
    <item>
      <title>Tropical intertidal microbiome response to the 2024 Marine Honour oil spill</title>
      <link>https://escholarship.org/uc/item/052047nc</link>
      <description>Marine fuel oil (MFO) spills in tropical coastal environments are under-characterized despite increasing risk from maritime activities. Microbial and geochemical responses to the June 2024 Marine Honour MFO spill on Singapore's intertidal sediments were analyzed in real time over 185 days. Using metagenomics and hydrocarbon profiling, microbial community shifts and hydrocarbon degradation were quantified across visibly oiled (high-impact) and clean (low-impact) sites. Microbiomes at all sites adapted rapidly to the spill through increased diversity and abundance of genes encoding alkane and aromatic compound degradation, detoxification, and biosurfactant production. The dominant hydrocarbon-degrading bacteria differed markedly from those reported in other crude oil spills and in regions with different climates. Oil deposition intensity strongly influenced microbial succession and hydrocarbon-degrading gene profiles, and this reflected early toxicity constraints in heavily oiled...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/052047nc</guid>
      <pubDate>Tue, 13 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>George, Christaline</name>
      </author>
      <author>
        <name>Dharan, Hashani M</name>
      </author>
      <author>
        <name>Drescher, Lynn</name>
      </author>
      <author>
        <name>Lee, Jenelle</name>
      </author>
      <author>
        <name>Qi, Yan</name>
      </author>
      <author>
        <name>Wang, Yijin</name>
      </author>
      <author>
        <name>Chang, Ying</name>
      </author>
      <author>
        <name>Teo, Serena Lay Ming</name>
      </author>
      <author>
        <name>Wainwright, Benjamin J</name>
      </author>
      <author>
        <name>Yung, Charmaine</name>
      </author>
      <author>
        <name>Lauro, Federico M</name>
      </author>
      <author>
        <name>Hazen, Terry C</name>
        <uri>https://orcid.org/0000-0002-2536-9993</uri>
      </author>
      <author>
        <name>Pointing, Stephen B</name>
      </author>
    </item>
    <item>
      <title>A worldwide climatology of extreme air masses</title>
      <link>https://escholarship.org/uc/item/4bm4v9s7</link>
      <description>Extreme temperature events are among the most damaging weather phenomena. In a warming world, more heat extremes and fewer cold extremes are expected in most regions in the future, a trade-off that warrants further understanding of such events. Here, we track and analyze large, persistent areas of hot and cold extreme temperatures in parallel, relative to the location and time of year, to quantify overall regional exposure to extreme temperatures. To accomplish this, we compare the frequencies, movements, trends, and sources/sinks in each type of extreme air mass, calling them extreme cold or extreme hot air masses (ECAMs/EHAMs). For most land regions, ECAMs occur more often than EHAMs, and ECAMs are more common in each hemisphere’s winter, when cold-air advection is strongest and most widespread. Average movement of ECAMs has a stronger equatorward component in winter than in summer, while movement of EHAMs is eastward all year, with less meridional movement than ECAMs. EHAMs...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4bm4v9s7</guid>
      <pubDate>Mon, 12 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Ryan, James M</name>
      </author>
      <author>
        <name>Kravitz, Ben</name>
      </author>
      <author>
        <name>O’Brien, Travis A</name>
      </author>
      <author>
        <name>Robeson, Scott M</name>
      </author>
      <author>
        <name>Staten, Paul W</name>
      </author>
    </item>
    <item>
      <title>Implementation and Evaluation of Emission‐Driven Land‐Atmosphere Coupled Simulation in E3SMv2.1</title>
      <link>https://escholarship.org/uc/item/02v1587q</link>
      <description>Abstract  Emissions‐driven (prognostic CO 2 ) simulations are essential for representing two‐way carbon‐climate feedback in Earth System Models. We present an emissions‐driven land–atmosphere coupled biogeochemistry (BGC) configuration (BGCLNDATM_progCO2) in version 2.1 of the Energy Exascale Earth System Model (E3SMv2.1). This is the first E3SM configuration that performs land‐atmosphere emission‐hindcasts. Here, we document its implementation, evaluate the model's performance against observations and other models, and propose a structured evaluation protocol for such emissions‐driven simulations. We conducted transient historical simulations (1850–2014) with BGCLNDATM_progCO2 and compare them to reference simulations—a land‐atmosphere coupled simulation without BGC and a standalone land simulation with BGC, both using prescribed CO 2 concentrations—and to observations. BGCLNDATM_progCO2 overestimates atmospheric CO 2 concentrations by 11–23&amp;nbsp;ppm yet stays within the 40‐ppm...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/02v1587q</guid>
      <pubDate>Mon, 12 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Sha</name>
      </author>
      <author>
        <name>Harrop, Bryce E</name>
      </author>
      <author>
        <name>Ricciuto, Daniel M</name>
      </author>
      <author>
        <name>Burrows, Susannah M</name>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Lin, Wuyin</name>
      </author>
      <author>
        <name>Collier, Nathan</name>
      </author>
      <author>
        <name>Bond‐Lamberty, Ben</name>
      </author>
      <author>
        <name>Zhang, Chengzhu</name>
      </author>
      <author>
        <name>Forsyth, Ryan M</name>
      </author>
      <author>
        <name>Wolfe, Jonathan D</name>
      </author>
      <author>
        <name>Shi, Xiaoying</name>
      </author>
      <author>
        <name>Thornton, Peter E</name>
      </author>
      <author>
        <name>Takano, Yohei</name>
      </author>
      <author>
        <name>Maltrud, Mathew E</name>
      </author>
      <author>
        <name>Singh, Balwinder</name>
      </author>
      <author>
        <name>Fang, Yilin</name>
      </author>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Jeffery, Nicole</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
    </item>
    <item>
      <title>Seasonality and Declining Intensity of Methane Emissions from the Permian and Nearby US Oil and Gas Basins</title>
      <link>https://escholarship.org/uc/item/4vt1d7fh</link>
      <description>We quantify weekly methane emissions and trends from oil and gas production in the US Permian Basin for 2019-2023, and in nearby basins for 2022-2023, by analytical inversion of Tropospheric Monitoring Instrument (TROPOMI) satellite observations with the Integrated Methane Inversion (IMI) at 25 km resolution. Permian oil and gas emissions averaged 4.0 ± 1.1 Tg a&lt;sup&gt;-1&lt;/sup&gt; over 2019-2023, with large seasonal variation but little interannual variability. Methane intensity fell from 5.2 to 3.2% as production surged. Intensity in the New Mexico Permian fell from 4.5 to 2.1%, approaching the state's 2026 target of &amp;lt;2%. Emissions were on average 50 ± 10% higher in winter than summer, which we corroborate with Permian Basin Tower Network measurements, Insight M aircraft data, and GHGSat satellite observations. This seasonality may be driven in part by higher winter emissions from liquid storage tanks due to decreased separator efficiency in cold conditions. Similar but weaker seasonality...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4vt1d7fh</guid>
      <pubDate>Fri, 9 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Varon, Daniel J</name>
      </author>
      <author>
        <name>Jacob, Daniel J</name>
      </author>
      <author>
        <name>Estrada, Lucas A</name>
      </author>
      <author>
        <name>Balasus, Nicholas</name>
      </author>
      <author>
        <name>East, James D</name>
      </author>
      <author>
        <name>Pendergrass, Drew C</name>
      </author>
      <author>
        <name>Chen, Zichong</name>
      </author>
      <author>
        <name>Sulprizio, Melissa</name>
      </author>
      <author>
        <name>Omara, Mark</name>
      </author>
      <author>
        <name>Gautam, Ritesh</name>
      </author>
      <author>
        <name>Barkley, Zachary R</name>
      </author>
      <author>
        <name>Saldaña, Felipe J Cardoso</name>
      </author>
      <author>
        <name>Reidy, Emily K</name>
      </author>
      <author>
        <name>Kamdar, Harshil</name>
      </author>
      <author>
        <name>Sherwin, Evan D</name>
        <uri>https://orcid.org/0000-0003-2180-4297</uri>
      </author>
      <author>
        <name>Biraud, Sebastien C</name>
      </author>
      <author>
        <name>Jervis, Dylan</name>
      </author>
      <author>
        <name>Pandey, Sudhanshu</name>
      </author>
      <author>
        <name>Worden, John R</name>
      </author>
      <author>
        <name>Bowman, Kevin W</name>
      </author>
      <author>
        <name>Maasakkers, Joannes D</name>
      </author>
      <author>
        <name>Kleinberg, Robert L</name>
      </author>
    </item>
    <item>
      <title>Multidecadal Fluctuations in the Observed ENSO‐Tropical Cyclone Teleconnection</title>
      <link>https://escholarship.org/uc/item/7nj33170</link>
      <description>Abstract El Niño‐Southern Oscillation (ENSO) is a skillful predictor for seasonal tropical cyclone (TC) activity in most TC basins. This study examines recent changes in the observed ENSO‐TC teleconnection strength, as measured by ENSO modulation of hurricane frequency. We find that the ENSO‐North Atlantic TC teleconnection fluctuated over time, with the strongest relationship occurring from the 1980s to the mid‐2000s. In the western and eastern North Pacific, the ENSO‐TC teleconnection has strengthened in recent decades. Periods with a strong ENSO‐TC teleconnection are associated with more favorable environmental conditions for TCs, with higher values of genesis potential indices. Positive phases of the Atlantic Multidecadal Oscillation coincided with periods of strong ENSO‐TC teleconnections in the Atlantic and North Pacific basins. A weaker Atlantic ENSO‐TC relationship was associated with negative phases of the Pacific Decadal Oscillation and the North Atlantic Oscillation....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7nj33170</guid>
      <pubDate>Tue, 23 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Sena, ACT</name>
      </author>
      <author>
        <name>Patricola‐DiRosario, Christina M</name>
      </author>
      <author>
        <name>Klotzbach, PJ</name>
      </author>
      <author>
        <name>Camargo, SJ</name>
      </author>
      <author>
        <name>Lee, C‐Y</name>
      </author>
      <author>
        <name>Tippett, MK</name>
      </author>
    </item>
    <item>
      <title>A Climatology and Life‐Cycle Characteristics of Atmospheric Fronts and Their Associated Precipitation</title>
      <link>https://escholarship.org/uc/item/3kr618df</link>
      <description>Abstract Atmospheric fronts are one of the main sources of mid‐latitude variability. We employ a novel method for identifying and tracking fronts and frontal precipitation. Thermal and dynamical variables are used to identify fronts as areal objects in space, which are tracked in time using the open‐source TempestExtremes software package. Precipitation objects are co‐located to identify frontal precipitation. The method is subjected to validation and sensitivity tests using manually curated data from the National Weather Service. Climatologies of fronts and frontal precipitation are computed from reanalysis and observations; fronts are present upwards of 14% of the time in the storm tracks, and represent the majority (up to 90%) of total and extreme precipitation. Novel aspects of the method are showcased through the lifetime characteristics of fronts across North America. Three sets of warm and cold fronts were discovered, and their duration, distance‐traveled, and translation...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3kr618df</guid>
      <pubDate>Tue, 23 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Landy, John</name>
      </author>
      <author>
        <name>Reed, Kevin A</name>
      </author>
      <author>
        <name>Rhoades, Alan M</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Ullrich, Paul A</name>
        <uri>https://orcid.org/0000-0003-4118-4590</uri>
      </author>
    </item>
    <item>
      <title>Evaluating Mean State Cloud Properties in the Simple Cloud‐Resolving E3SM Atmosphere Model (SCREAM)</title>
      <link>https://escholarship.org/uc/item/4k24k10m</link>
      <description>Abstract Accurately simulating clouds remains a key challenge in global climate models, primarily because cloud formation involves sub‐grid processes that are parameterized and crudely represented in models. This study examines the performance of DOE's Simple Cloud‐Resolving Energy Exascale Earth System (E3SM) Atmosphere Model (SCREAM) in simulating cloud properties and their spatio‐temporal distribution by comparing against satellite observations. Two horizontal resolutions of SCREAM (3 and 12&amp;nbsp;km) are examined, and both depict a realistic spatial structure of mean‐state cloud cover but underestimate its global mean magnitude. SCREAM 3&amp;nbsp;km reasonably reproduces the distribution of mean‐state cloud properties across various cloud optical thickness and cloud‐top pressure regimes, with performance comparable to CMIP5 and CMIP6 ensemble and marginally outperforming SCREAM 12&amp;nbsp;km. Still, SCREAM 3&amp;nbsp;km tends to underpredict low clouds and optically thin clouds, highlighting...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4k24k10m</guid>
      <pubDate>Fri, 19 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chao, Li‐Wei</name>
      </author>
      <author>
        <name>Zelinka, Mark D</name>
      </author>
      <author>
        <name>Terai, Christopher R</name>
      </author>
      <author>
        <name>Beydoun, Hassan</name>
      </author>
      <author>
        <name>Hillman, Benjamin R</name>
      </author>
      <author>
        <name>Keen, Noel D</name>
        <uri>https://orcid.org/0000-0003-3607-3554</uri>
      </author>
      <author>
        <name>Caldwell, Peter M</name>
      </author>
      <author>
        <name>Klein, Stephen A</name>
      </author>
    </item>
    <item>
      <title>Atmospheric Feedbacks Reverse the Sensitivity of Modeled Photosynthesis to Stomatal Function</title>
      <link>https://escholarship.org/uc/item/8tz9f800</link>
      <description>Abstract Stomata mediate fluxes of carbon and water between terrestrial plants and the atmosphere. These fluxes are governed by stomatal function and can be modulated in many Earth system models by an empirical parameter within the calculation of stomatal conductance, the stomatal slope . Intuitively, represents the marginal water cost of carbon, relating it to the emergent plant property of water use efficiency. Observations show that can range widely across and within plant types in varying environments, and this distribution of is not captured within Earth system models which represent each plant type with a single value. Here we examine how influences photosynthesis using coupled Earth system model simulations by perturbing to observed and percentiles for each plant type. We find that high reduces photosynthesis nearly everywhere, while low has regionally dependent responses. Under fixed atmospheric conditions, low increases photosynthesis in the Amazon and central North America...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8tz9f800</guid>
      <pubDate>Wed, 17 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Liu, Amy X</name>
      </author>
      <author>
        <name>Zarakas, Claire M</name>
      </author>
      <author>
        <name>Buchovecky, Benjamin G</name>
      </author>
      <author>
        <name>Hawkins, Linnia R</name>
      </author>
      <author>
        <name>Cordak, Alana S</name>
      </author>
      <author>
        <name>Cornish, Ashley E</name>
      </author>
      <author>
        <name>Haagsma, Marja</name>
      </author>
      <author>
        <name>Kooperman, Gabriel J</name>
      </author>
      <author>
        <name>Still, Chris J</name>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Turner, Alexander J</name>
      </author>
      <author>
        <name>Battisti, David S</name>
      </author>
      <author>
        <name>Randerson, James T</name>
        <uri>https://orcid.org/0000-0001-6559-7387</uri>
      </author>
      <author>
        <name>Hoffman, Forrest M</name>
      </author>
      <author>
        <name>Swann, Abigail LS</name>
      </author>
    </item>
    <item>
      <title>High Performance, High Fidelity: A GPU‐Accelerated Doubly‐Periodic Configuration of the Simple Cloud‐Resolving E3SM Atmosphere Model Version 1 (DP‐SCREAMv1)</title>
      <link>https://escholarship.org/uc/item/2h53h92v</link>
      <description>Abstract The development of the Simplified Cloud Resolving Energy Exascale Earth System Atmosphere Model (SCREAMv1) enables global storm‐resolving simulations on modern GPU‐based supercomputers. However, the high computational cost of SCREAMv1 limits its routine use for process‐level studies, creating a need for efficient proxy configurations. This study addresses this gap by introducing DP‐SCREAMv1, a doubly periodic cloud‐resolving model designed to be fully consistent with SCREAMv1 while enabling high‐resolution, long‐duration simulations at significantly reduced computational expense by simulating a limited doubly periodic domain rather than the entire globe. Built on a C++/Kokkos architecture, DP‐SCREAMv1 achieves exceptional performance scalability on GPU systems and includes a rich library of cases for validation and scientific exploration. In this work, we demonstrate short wall‐clock times at SCREAMv1's default resolution and show that DP‐SCREAMv1 supports routine execution...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2h53h92v</guid>
      <pubDate>Wed, 17 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Bogenschutz, PA</name>
      </author>
      <author>
        <name>Clevenger, TC</name>
      </author>
      <author>
        <name>Bradley, AM</name>
      </author>
      <author>
        <name>Caldwell, PM</name>
      </author>
      <author>
        <name>Beydoun, H</name>
      </author>
      <author>
        <name>Mahfouz, N</name>
      </author>
      <author>
        <name>Keen, ND</name>
        <uri>https://orcid.org/0000-0003-3607-3554</uri>
      </author>
      <author>
        <name>Guba, O</name>
      </author>
      <author>
        <name>Bertagna, L</name>
      </author>
      <author>
        <name>Foucar, J</name>
      </author>
      <author>
        <name>Zhang, J</name>
      </author>
      <author>
        <name>Donahue, AS</name>
      </author>
    </item>
    <item>
      <title>Soil oxygen dynamics: a key mediator of tile drainage impacts on coupled hydrological, biogeochemical, and crop systems</title>
      <link>https://escholarship.org/uc/item/02p902ch</link>
      <description>Abstract. Tile drainage removes excess water and is an essential, widely adopted management practice to enhance crop productivity in the US&amp;nbsp;Midwest and throughout the world. Tile drainage has been shown to significantly change hydrological and biogeochemical cycles by lowering the water table and reducing the residence time of soil water, although examining the complex interactions and feedbacks in an integrated hydrology–biogeochemistry–crop system remains elusive. Oxygen dynamics are critical to unraveling these interactions and have been ignored or oversimplified in existing models. Understanding these impacts is essential, particularly so because tile drainage has been highlighted as an adaptation under projected wetter springs and drier summers in the changing climate in the US&amp;nbsp;Midwest. We used the ecosys model that uniquely incorporates first-principle soil oxygen dynamics and crop oxygen uptake mechanisms to quantify the impacts of tile drainage on hydrological...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/02p902ch</guid>
      <pubDate>Wed, 17 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Ma, Zewei</name>
      </author>
      <author>
        <name>Guan, Kaiyu</name>
      </author>
      <author>
        <name>Peng, Bin</name>
      </author>
      <author>
        <name>Zhou, Wang</name>
      </author>
      <author>
        <name>Grant, Robert</name>
      </author>
      <author>
        <name>Tang, Jinyun</name>
        <uri>https://orcid.org/0000-0002-4792-1259</uri>
      </author>
      <author>
        <name>Sivapalan, Murugesu</name>
      </author>
      <author>
        <name>Pan, Ming</name>
      </author>
      <author>
        <name>Li, Li</name>
      </author>
      <author>
        <name>Jin, Zhenong</name>
      </author>
    </item>
    <item>
      <title>Modelling the Effects of Wetland Restoration on Coastal Hydrology: A Case Study of Elkhorn Slough Watershed, California</title>
      <link>https://escholarship.org/uc/item/9xp1s1n9</link>
      <description>ABSTRACT Coastal wetlands, some of the most productive ecosystems on Earth, provide critical ecosystem services, including support of biodiversity, carbon sequestration and flood protection. In recent decades, these ecosystems have experienced extensive coastal wetland loss. Coastal wetland restoration provides a beacon of hope, offering a chance to reclaim these important habitats. However, even with billions of dollars invested worldwide in restoring coastal wetlands, we still lack comprehensive knowledge about the effectiveness of these restoration efforts in recovering wetland ecosystem functions and how future climate change may affect these efforts. The ability to evaluate how these ecosystems will function in the future is vital for examining current investments and developing future protection and management plans. We selected Elkhorn Slough, a tidal estuary, in California, to investigate the impact of wetland restoration and sea level rise (SLR) on coastal hydrology using...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9xp1s1n9</guid>
      <pubDate>Tue, 16 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Xu, Yi</name>
      </author>
      <author>
        <name>Zhang, Yu</name>
      </author>
      <author>
        <name>Moulton, J David</name>
      </author>
      <author>
        <name>Brereton, Ashley</name>
      </author>
      <author>
        <name>Mekonnen, Zelalem A</name>
        <uri>https://orcid.org/0000-0002-2647-0671</uri>
      </author>
      <author>
        <name>Arora, Bhavna</name>
      </author>
      <author>
        <name>Endris, Charlie</name>
      </author>
      <author>
        <name>Haskins, John</name>
      </author>
      <author>
        <name>Paytan, Adina</name>
        <uri>https://orcid.org/0000-0001-8360-4712</uri>
      </author>
    </item>
    <item>
      <title>Regional-scale soil carbon predictions can be enhanced by transferring global-scale soil–environment relationships</title>
      <link>https://escholarship.org/uc/item/05j3c4qt</link>
      <description>Accurate modelling and mapping soil organic carbon are crucial for supporting soil health restoration and climate change mitigation at both regional and global scales. However, regional soil predictions often suffer from data scarcity and high prediction uncertainty. Utilizing a pre-trained global-to-regional soil carbon predictive model can be a potential solution to address this challenge. Despite its promise, how to construct and apply the global-scale model to enhance regional-scale soil carbon mapping remains largely unexplored. Here, we propose the Global Soil Carbon Pre-trained Model (GSoilCPM), a deep-learning-based domain adaptative model, to enhance regional-scale soil carbon predictions. Based on large amount of environmental covariate data and 106,167 soil samples across the globe, we verify our hypothesis of the effectiveness of this 'global-to-regional' modelling strategy. The pre-trained model can be then transferred and fine-tuned to bridge the regional- and global-scale...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/05j3c4qt</guid>
      <pubDate>Fri, 12 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zhang, Lei</name>
        <uri>https://orcid.org/0000-0002-1090-6338</uri>
      </author>
      <author>
        <name>Yang, Lin</name>
      </author>
      <author>
        <name>Ma, Yuxin</name>
      </author>
      <author>
        <name>Zhu, A-Xing</name>
      </author>
      <author>
        <name>Wei, Ren</name>
      </author>
      <author>
        <name>Liu, Jie</name>
      </author>
      <author>
        <name>Greve, Mogens H</name>
      </author>
      <author>
        <name>Zhou, Chenghu</name>
      </author>
    </item>
    <item>
      <title>The Remarkable 2024 North Atlantic Mid‐Season Hurricane Lull</title>
      <link>https://escholarship.org/uc/item/836446m0</link>
      <description>Abstract The 2024 North Atlantic (hereafter Atlantic) hurricane season started quickly, with the earliest Category 5 on record (Beryl) and three hurricanes forming through 14 August. Following Ernesto's dissipation on 20 August, the Atlantic hurricane season became extremely quiet during the climatological peak of hurricane season, with only one Category 2 hurricane (Francine) and one tropical storm through 23 September. Several environmental factors likely contributed to this unexpected, prolonged lull. During mid‐to‐late August, subseasonal conditions were broadly favorable for Atlantic hurricanes, but a northward shift in African easterly wave emergence latitude yielded fewer tropical cyclone seed disturbances that also traversed unfavorably cool ocean water. During early‐to‐mid September, subseasonal variability driven by the Madden‐Julian oscillation was less conducive to hurricane activity, with several bouts of increased vertical wind shear across the central Atlantic....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/836446m0</guid>
      <pubDate>Wed, 10 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Klotzbach, PJ</name>
      </author>
      <author>
        <name>Bercos‐Hickey, E</name>
      </author>
      <author>
        <name>Wood, KM</name>
      </author>
      <author>
        <name>Schreck, CJ</name>
      </author>
      <author>
        <name>Bell, MM</name>
      </author>
      <author>
        <name>Blake, ES</name>
      </author>
      <author>
        <name>Bowen, SG</name>
      </author>
      <author>
        <name>Caron, L‐P</name>
      </author>
      <author>
        <name>Chavas, DR</name>
      </author>
      <author>
        <name>Collins, JM</name>
      </author>
      <author>
        <name>Gibney, EJ</name>
      </author>
      <author>
        <name>Hansen, KA</name>
      </author>
      <author>
        <name>Hazelton, AT</name>
      </author>
      <author>
        <name>Jones, JJ</name>
      </author>
      <author>
        <name>Lowry, MR</name>
      </author>
      <author>
        <name>Nieves‐Jimenez, AT</name>
      </author>
      <author>
        <name>Patricola, CM</name>
      </author>
      <author>
        <name>Silvers, LG</name>
      </author>
      <author>
        <name>Truchelut, RE</name>
      </author>
      <author>
        <name>Uehling, J</name>
      </author>
    </item>
    <item>
      <title>Demography, dynamics and data: building confidence for simulating changes in the world's forests</title>
      <link>https://escholarship.org/uc/item/3gx8z77m</link>
      <description>Vegetation demographic models (VDMs) are advanced tools for simulating forest responses to climate and land-use changes, and are essential for projecting carbon cycling and large-scale forest management strategies. Despite their increasing incorporation into Earth System Models, VDMs differ in their demographic assumptions, with no prior quantitative comparison of their performance. We benchmarked nine VDMs against observational data from boreal, temperate and tropical sites, assessing their accuracy in predicting tree growth, carbon turnover, biomass stocks and size distributions. Models were simulated under consistent climate conditions with postdisturbance recovery monitored for at least 420 yr. Postdisturbance carbon recovery trajectories showed significant variability while remaining within observational ranges. Initial regrowth rates varied substantially (0.03-0.60, 0.18-0.70 and 0.35-1.10 kgCm&lt;sup&gt;-2&lt;/sup&gt; yr&lt;sup&gt;-1&lt;/sup&gt; for boreal, temperate and tropical sites, respectively),...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3gx8z77m</guid>
      <pubDate>Thu, 4 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Eckes‐Shephard, Annemarie H</name>
      </author>
      <author>
        <name>Argles, Arthur PK</name>
      </author>
      <author>
        <name>Brzeziecki, Bogdan</name>
      </author>
      <author>
        <name>Cox, Peter M</name>
      </author>
      <author>
        <name>De Kauwe, Martin G</name>
      </author>
      <author>
        <name>Esquivel‐Muelbert, Adriane</name>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Hurtt, George C</name>
      </author>
      <author>
        <name>Knauer, Jürgen</name>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Lehtonen, Aleksi</name>
      </author>
      <author>
        <name>Luyssaert, Sebastiaan</name>
      </author>
      <author>
        <name>Marqués, Laura</name>
      </author>
      <author>
        <name>Ma, Lei</name>
      </author>
      <author>
        <name>Marie, Guillaume</name>
      </author>
      <author>
        <name>Moore, Jonathan R</name>
      </author>
      <author>
        <name>Needham, Jessica F</name>
        <uri>https://orcid.org/0000-0003-3653-3848</uri>
      </author>
      <author>
        <name>Olin, Stefan</name>
      </author>
      <author>
        <name>Peltoniemi, Mikko</name>
      </author>
      <author>
        <name>Piltz, Karl</name>
      </author>
      <author>
        <name>Sato, Hisashi</name>
      </author>
      <author>
        <name>Sitch, Stephen</name>
      </author>
      <author>
        <name>Stocker, Benjamin D</name>
      </author>
      <author>
        <name>Weng, Ensheng</name>
      </author>
      <author>
        <name>Zuleta, Daniel</name>
      </author>
      <author>
        <name>Pugh, Thomas AM</name>
      </author>
    </item>
    <item>
      <title>Brief communication: Decadal changes in topography, surface water and subsurface structure across an Arctic coastal tundra site</title>
      <link>https://escholarship.org/uc/item/4cx3d3wf</link>
      <description>Abstract. In ice-rich polygonal tundra, spatiotemporal heterogeneity in ground-ice melt reshapes topography, impacting infrastructure, water and carbon cycles. This study evaluates changes in topography and subsurface structure at a coastal Arctic site by comparing data from two surveys conducted a decade apart. Each survey includes electrical resistivity tomography, active layer thickness, photogrammetry, and topographic data. Results reveal subsidence and decrease in permafrost table elevation with varying intensity and spatial distribution across polygons, alongside diverse thermal-hydrological responses, such as thermokarst pool formation in high-centered-polygons and more even subsidence in flat-centered-polygons. The study also underscores the value and limitations of sporadic surveys.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4cx3d3wf</guid>
      <pubDate>Mon, 1 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Bachman, Jonathan A</name>
      </author>
      <author>
        <name>Lamb, John</name>
      </author>
      <author>
        <name>Ulrich, Craig</name>
        <uri>https://orcid.org/0000-0002-4114-7039</uri>
      </author>
      <author>
        <name>Taş, Neslihan</name>
        <uri>https://orcid.org/0000-0001-7525-2331</uri>
      </author>
      <author>
        <name>Dafflon, Baptiste</name>
        <uri>https://orcid.org/0000-0001-9871-5650</uri>
      </author>
    </item>
    <item>
      <title>Belowground cross-trophic networks impact CH4 and CO2 emissions in degraded alpine peatlands</title>
      <link>https://escholarship.org/uc/item/33m3c36s</link>
      <description>Belowground organisms forming complex cross-trophic ecological networks are essential for maintaining peatland carbon stability and energy flow. However, how peatland degradation affects the biodiversity and cross-trophic ecological networks of soil communities remains poorly understood. Here, we examined the degradation effects on soil prokaryotes (i.e., bacteria, archaea), fungi and nematodes in alpine peatlands on the eastern Tibetan Plateau, characterized by varying water table depths (indicating degradation levels). We found that peatland degradation, accompanied by significant shifts in soil moisture and pH (P&amp;nbsp;&amp;lt;&amp;nbsp;0.05), reduced the taxonomic richness and phylogenetic diversity of prokaryotes, fungi, and nematodes, particularly in deeper soil layers (20–50&amp;nbsp;cm). Crucially, peatland degradation weakened potential cross-trophic interactions within bipartite networks of prokaryotes-nematodes and fungi-nematodes, resulting in less than 6.5&amp;nbsp;%–28.8&amp;nbsp;% of...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/33m3c36s</guid>
      <pubDate>Fri, 21 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chen, Dengbo</name>
      </author>
      <author>
        <name>Sun, Feng</name>
      </author>
      <author>
        <name>Qiu, Qiongyi</name>
      </author>
      <author>
        <name>Huang, Xueli</name>
      </author>
      <author>
        <name>Xu, Weitong</name>
      </author>
      <author>
        <name>Liu, Suo</name>
      </author>
      <author>
        <name>He, Songbing</name>
      </author>
      <author>
        <name>Zhao, Mengying</name>
      </author>
      <author>
        <name>Fu, Shuai</name>
      </author>
      <author>
        <name>Zeng, Yufei</name>
      </author>
      <author>
        <name>Yang, Yunfeng</name>
      </author>
      <author>
        <name>Ning, Daliang</name>
        <uri>https://orcid.org/0000-0002-3368-5988</uri>
      </author>
      <author>
        <name>Zhou, Jizhong</name>
        <uri>https://orcid.org/0000-0003-2014-0564</uri>
      </author>
      <author>
        <name>Wang, Mei</name>
      </author>
      <author>
        <name>Guo, Xue</name>
      </author>
    </item>
    <item>
      <title>Improving the Integration of Diversity, Equity, Inclusion, and Justice Goals in Total Maximum Daily Load Model Implementation for Water Quality Management</title>
      <link>https://escholarship.org/uc/item/0c51z2p0</link>
      <description>Water quality modeling is used globally to assess surface water impairment and manage watershed pollution in formal programs like the United States' (US) total maximum daily load and in less structured initiatives elsewhere. Despite these programs, progress toward realizing equitable water quality benefits to society is stymied through an inability to recognize, plan, and incorporate diversity, equity, inclusion, and justice (DEIJ) principles in the modeling efforts. In this paper, we describe the major barriers and limitations to the inclusion of DEIJ principles in the design and implementation of pollution load reduction programs in the US. We offer a blueprint to embrace participatory modeling approaches to engage more openly, honestly, and fairly with relevant participants (stakeholders) to achieve just and equitable water quality outcomes and upgrade water quality management principles nationwide. We provide case studies where the DEIJ principles have been applied and synthesized,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0c51z2p0</guid>
      <pubDate>Fri, 21 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Quinn, Nigel WT</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
      <author>
        <name>Sridharan, Vamsi Krishna</name>
      </author>
      <author>
        <name>Babbar-Sebens, Meghna</name>
      </author>
      <author>
        <name>Zellner, Moira</name>
      </author>
      <author>
        <name>Lott, Craig</name>
      </author>
      <author>
        <name>Guzmán, Sandra M</name>
      </author>
      <author>
        <name>Kumar, Saurav</name>
      </author>
      <author>
        <name>Ahmadisharaf, Ebrahim</name>
      </author>
      <author>
        <name>Rabby, Sumon Hossain</name>
      </author>
      <author>
        <name>Helgeson, Jennifer</name>
      </author>
    </item>
    <item>
      <title>A minor respiratory process with major global implications: is atmospheric methane oxidation in tree stems driven by stem respiration rather than microbial methanotrophy?</title>
      <link>https://escholarship.org/uc/item/7kc4p1rs</link>
      <description>Tree stem surfaces are widely recognized as sites of carbon dioxide (CO₂) efflux and oxygen (O₂) influx, reflecting the dynamics of aerobic respiration of photosynthate substrates, such as sugars, delivered via the phloem. Stems are also largely considered passive conduits for methane (CH₄) produced in anoxic soils via microbial methanogenesis, where CH₄ is thought to be transported upward through the transpiration stream and/or diffusion and emitted through stem surfaces and the canopy. However, recent observations from dynamic stem chambers suggest that stems may also act as active sinks for atmospheric CH₄. Despite these findings, the extent and drivers of stem CH₄ consumption remain poorly characterized across biomes, species, and environmental gradients, and its quantitative relationship to stem respiration has not been established. Moreover, previous studies captured only snapshot fluxes, leaving diurnal patterns of CH₄ exchange uncharacterized. Here, we address these limitations...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7kc4p1rs</guid>
      <pubDate>Thu, 20 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Boko, Tandeka</name>
      </author>
      <author>
        <name>Biraud, Sebastian</name>
      </author>
      <author>
        <name>Keppler, Frank</name>
      </author>
    </item>
    <item>
      <title>The Role of Wind‐Moisture Characteristics in Shaping Atmospheric River Flood Hazards</title>
      <link>https://escholarship.org/uc/item/9hg7c97s</link>
      <description>Abstract Atmospheric rivers (ARs) are key drivers of extreme precipitation in the Western U.S. Using regionally downscaled thermodynamic global warming (TGW) simulations, we examine how ARs with varying wind and moisture characteristics respond to warming. We classified 812 historical AR events into Gusty‐Wet, Gusty‐Dry, Calm‐Wet, and Calm‐Dry groups to evaluate differences in precipitation behavior. ARs with stronger winds and higher moisture content exhibit higher precipitation efficiency (PE) and greater integrated water vapor (IWV). Regionally, Calm ARs show higher IWV accumulation due to slower inland transport and reduced PE. Projections indicate increases in storm‐total (sub‐Clausius‐Clapeyron (CC) scaling) and maximum 3‐hourly precipitation (super‐CC scaling) across all groups, with the most pronounced changes in Gusty‐Wet and Calm‐Wet ARs. Spatial differences in surface runoff, PE, and inland reach highlight the importance of AR subtype in shaping future flood hazards....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9hg7c97s</guid>
      <pubDate>Tue, 18 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zhou, Yang</name>
        <uri>https://orcid.org/0000-0003-2835-4081</uri>
      </author>
      <author>
        <name>Wehner, Michael M</name>
        <uri>https://orcid.org/0000-0001-8423-7870</uri>
      </author>
      <author>
        <name>Rhoades, Alan M</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Jones, Andrew D</name>
        <uri>https://orcid.org/0000-0002-1913-7870</uri>
      </author>
    </item>
    <item>
      <title>Huge ensembles – Part 2: Properties of a huge ensemble of hindcasts generated with spherical Fourier neural operators</title>
      <link>https://escholarship.org/uc/item/53f2p5xt</link>
      <description>Abstract. In Part&amp;nbsp;1, we created an ensemble based on spherical Fourier neural operators. As initial condition perturbations, we used bred vectors, and as model perturbations, we used multiple checkpoints trained independently from scratch. Based on diagnostics that assess the ensemble's physical fidelity, our ensemble has comparable performance to operational weather forecasting systems. However, it requires orders-of-magnitude fewer computational resources. Here in Part 2, we generate a huge ensemble (HENS), with 7424 members initialized each day of summer 2023. We enumerate the technical requirements for running huge ensembles at this scale. HENS precisely samples the tails of the forecast distribution and presents a detailed sampling of internal variability. HENS has two primary applications: (1)&amp;nbsp;as a large dataset with which to study the statistics and drivers of extreme weather and (2)&amp;nbsp;as a weather forecasting system. For extreme climate statistics, HENS samples...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/53f2p5xt</guid>
      <pubDate>Mon, 17 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Mahesh, Ankur</name>
      </author>
      <author>
        <name>Collins, William D</name>
        <uri>https://orcid.org/0000-0002-4463-9848</uri>
      </author>
      <author>
        <name>Bonev, Boris</name>
      </author>
      <author>
        <name>Brenowitz, Noah</name>
      </author>
      <author>
        <name>Cohen, Yair</name>
      </author>
      <author>
        <name>Harrington, Peter</name>
      </author>
      <author>
        <name>Kashinath, Karthik</name>
      </author>
      <author>
        <name>Kurth, Thorsten</name>
      </author>
      <author>
        <name>North, Joshua</name>
      </author>
      <author>
        <name>O'Brien, Travis A</name>
        <uri>https://orcid.org/0000-0002-6643-1175</uri>
      </author>
      <author>
        <name>Pritchard, Michael</name>
      </author>
      <author>
        <name>Pruitt, David</name>
      </author>
      <author>
        <name>Risser, Mark</name>
        <uri>https://orcid.org/0000-0003-1956-1783</uri>
      </author>
      <author>
        <name>Subramanian, Shashank</name>
      </author>
      <author>
        <name>Willard, Jared</name>
      </author>
    </item>
    <item>
      <title>Huge ensembles – Part 1: Design of ensemble weather forecasts using spherical Fourier neural operators</title>
      <link>https://escholarship.org/uc/item/09f7p278</link>
      <description>Abstract. Simulating low-likelihood high-impact extreme weather events in a warming world is a significant and challenging task for current ensemble forecasting systems. While these systems presently use up to 100 members, larger ensembles could enrich the sampling of internal variability. They may capture the long tails associated with climate hazards better than traditional ensemble sizes. Due to computational constraints, it is infeasible to generate huge ensembles (comprised of 1000–10 000 members) with traditional, physics-based numerical models. In this two-part paper, we replace traditional numerical simulations with machine learning (ML) to generate hindcasts of huge ensembles. In Part&amp;nbsp;1, we construct an ensemble weather forecasting system based on spherical Fourier neural operators (SFNOs), and we discuss important design decisions for constructing such an ensemble. The ensemble represents model uncertainty through perturbed-parameter techniques, and it represents...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/09f7p278</guid>
      <pubDate>Mon, 17 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Mahesh, Ankur</name>
      </author>
      <author>
        <name>Collins, William D</name>
        <uri>https://orcid.org/0000-0002-4463-9848</uri>
      </author>
      <author>
        <name>Bonev, Boris</name>
      </author>
      <author>
        <name>Brenowitz, Noah</name>
      </author>
      <author>
        <name>Cohen, Yair</name>
      </author>
      <author>
        <name>Elms, Joshua</name>
      </author>
      <author>
        <name>Harrington, Peter</name>
      </author>
      <author>
        <name>Kashinath, Karthik</name>
      </author>
      <author>
        <name>Kurth, Thorsten</name>
      </author>
      <author>
        <name>North, Joshua</name>
      </author>
      <author>
        <name>O'Brien, Travis</name>
        <uri>https://orcid.org/0000-0002-6643-1175</uri>
      </author>
      <author>
        <name>Pritchard, Michael</name>
      </author>
      <author>
        <name>Pruitt, David</name>
      </author>
      <author>
        <name>Risser, Mark</name>
        <uri>https://orcid.org/0000-0003-1956-1783</uri>
      </author>
      <author>
        <name>Subramanian, Shashank</name>
      </author>
      <author>
        <name>Willard, Jared</name>
      </author>
    </item>
    <item>
      <title>AmeriFlux BADM: Implementing lessons from 12 years of long-tail data management into next generation earth science systems</title>
      <link>https://escholarship.org/uc/item/38q3q585</link>
      <description>AmeriFlux is a community of scientists measuring ecosystem carbon, water, and energy fluxes across the Americas with eddy covariance techniques. The network’s data team collects flux data for quality assessment and provides standardized data products to the earth science research community. Critical for scientists’ use of the flux data are the supporting Biological, Ancillary, Disturbance and Metadata (BADM) that provide context, such as measurement heights, instrument operations, and disturbance events. Managing and collating BADM into standardized data products are challenging due to their inherent long-tail data characteristics, i.e., they are diverse, free-formed, and infrequently measured.
Over the past 12 years, we have worked with the community to standardize and then manage BADM using a SQL database with strong data quality criteria. BADM’s inherent nature demands rigorous quality checks of submitted data. Some of these checks provide feedback to data providers for correction,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/38q3q585</guid>
      <pubDate>Fri, 31 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Cheah, You-Wei</name>
        <uri>https://orcid.org/0000-0003-2241-4901</uri>
      </author>
      <author>
        <name>Christianson, Danielle</name>
      </author>
      <author>
        <name>Chu, Housen</name>
        <uri>https://orcid.org/0000-0002-8131-4938</uri>
      </author>
      <author>
        <name>Pastorello, Gilberto</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>O'Brien, Fianna</name>
      </author>
      <author>
        <name>Ong, Yeongshnn</name>
      </author>
      <author>
        <name>van Ingen, Catharine</name>
      </author>
      <author>
        <name>Torn, Margaret</name>
        <uri>https://orcid.org/0000-0002-8174-0099</uri>
      </author>
      <author>
        <name>Agarwal, Deb</name>
        <uri>https://orcid.org/0000-0001-5045-2396</uri>
      </author>
    </item>
    <item>
      <title>Investigating the Global Biogeophysical Impact of Area and Mass Based Wood Harvest in a Vegetation Demography Model</title>
      <link>https://escholarship.org/uc/item/70w229vm</link>
      <description>Abstract Wood harvesting alters land surface properties and energy redistribution, but there is a lack of studies estimating these changes on a global scale. We coupled a vegetation demographic model, the Functionally Assembled Terrestrial Ecosystem Simulator, with the E3SM land model to perform offline model simulation to investigate the land biogeophysical responses, including canopy coverage, leaf area index, albedo, surface roughness length, and energy fluxes, to historical wood harvest on the global scale. In this study, we found 50% less harvested carbon (C) when choosing the area‐based harvest rate as driving data that has not been spatially harmonized, compared to reharmonized mass‐based harvesting. By considering the uncertainty from reconstruction of historical wood harvest time series and the choice of wood harvest approach in the model, continuous wood harvest (1850–2015) results in 5%–10% of canopy coverage loss, contributing 0.5%–1% increase of albedo over disturbed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/70w229vm</guid>
      <pubDate>Tue, 21 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Shu, Shijie</name>
      </author>
      <author>
        <name>Di Vittorio, Alan</name>
        <uri>https://orcid.org/0000-0002-8139-4640</uri>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Huang, Maoyi</name>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Lemieux, Gregory</name>
        <uri>https://orcid.org/0000-0001-5304-8938</uri>
      </author>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
    </item>
    <item>
      <title>Future Intensity‐Duration‐Frequency Curves of Extreme Precipitation in the Midwest United States From Convection‐Permitting Modeling</title>
      <link>https://escholarship.org/uc/item/1xv259v6</link>
      <description>Abstract During the last four decades, global warming has statistically significant intensified extreme precipitation events in the Midwestern United States (defined here as the region covering Illinois, Indiana, Ohio, and Kentucky), leading to increased risks to human life, property, and infrastructure. To enable climate change adaptation and resilience across various economic and social sectors in this region, updated information about future climate changes, specifically at finer spatial scales, is essential. Leveraging a new 150‐year dynamical downscaling data set at convection‐permitting resolution, this study introduces a framework to construct the projected future intensity‐duration‐frequency (IDF) curves of heavy precipitation, which are prominent tools for infrastructure design and water resources management. This framework generates IDF curves at both sub‐daily and multi‐day duration utilizing hourly in situ observations as well as quantile‐based statistical techniques...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1xv259v6</guid>
      <pubDate>Fri, 10 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Nguyen, Trung</name>
      </author>
      <author>
        <name>Kravitz, Ben</name>
      </author>
      <author>
        <name>O’Brien, Travis A</name>
      </author>
      <author>
        <name>Ficklin, Darren L</name>
      </author>
      <author>
        <name>Rasmussen, Kristen L</name>
      </author>
      <author>
        <name>Kruczkiewicz, Andrew</name>
      </author>
      <author>
        <name>Huang, Jiyun</name>
      </author>
      <author>
        <name>Li, Tony</name>
      </author>
      <author>
        <name>Lauer, Abraham</name>
      </author>
    </item>
    <item>
      <title>Toward a Cenozoic history of atmospheric CO2</title>
      <link>https://escholarship.org/uc/item/0tz7h903</link>
      <description>The geological record encodes the relationship between climate and atmospheric carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) over long and short timescales, as well as potential drivers of evolutionary transitions. However, reconstructing CO&lt;sub&gt;2&lt;/sub&gt; beyond direct measurements requires the use of paleoproxies and herein lies the challenge, as proxies differ in their assumptions, degree of understanding, and even reconstructed values. In this study, we critically evaluated, categorized, and integrated available proxies to create a high-fidelity and transparently constructed atmospheric CO&lt;sub&gt;2&lt;/sub&gt; record spanning the past 66 million years. This newly constructed record provides clearer evidence for higher Earth system sensitivity in the past and for the role of CO&lt;sub&gt;2&lt;/sub&gt; thresholds in biological and cryosphere evolution.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0tz7h903</guid>
      <pubDate>Thu, 9 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Consortium*†, The Cenozoic CO2 Proxy Integration Project</name>
      </author>
      <author>
        <name>Hönisch, Bärbel</name>
      </author>
      <author>
        <name>Royer, Dana L</name>
      </author>
      <author>
        <name>Breecker, Daniel O</name>
      </author>
      <author>
        <name>Polissar, Pratigya J</name>
        <uri>https://orcid.org/0000-0001-5483-1625</uri>
      </author>
      <author>
        <name>Bowen, Gabriel J</name>
      </author>
      <author>
        <name>Henehan, Michael J</name>
      </author>
      <author>
        <name>Cui, Ying</name>
      </author>
      <author>
        <name>Steinthorsdottir, Margret</name>
      </author>
      <author>
        <name>McElwain, Jennifer C</name>
      </author>
      <author>
        <name>Kohn, Matthew J</name>
      </author>
      <author>
        <name>Pearson, Ann</name>
      </author>
      <author>
        <name>Phelps, Samuel R</name>
      </author>
      <author>
        <name>Uno, Kevin T</name>
      </author>
      <author>
        <name>Ridgwell, Andy</name>
        <uri>https://orcid.org/0000-0003-2333-0128</uri>
      </author>
      <author>
        <name>Anagnostou, Eleni</name>
      </author>
      <author>
        <name>Austermann, Jacqueline</name>
      </author>
      <author>
        <name>Badger, Marcus PS</name>
      </author>
      <author>
        <name>Barclay, Richard S</name>
      </author>
      <author>
        <name>Bijl, Peter K</name>
      </author>
      <author>
        <name>Chalk, Thomas B</name>
      </author>
      <author>
        <name>Scotese, Christopher R</name>
      </author>
      <author>
        <name>de la Vega, Elwyn</name>
      </author>
      <author>
        <name>DeConto, Robert M</name>
      </author>
      <author>
        <name>Dyez, Kelsey A</name>
      </author>
      <author>
        <name>Ferrini, Vicki</name>
      </author>
      <author>
        <name>Franks, Peter J</name>
      </author>
      <author>
        <name>Giulivi, Claudia F</name>
      </author>
      <author>
        <name>Gutjahr, Marcus</name>
      </author>
      <author>
        <name>Harper, Dustin T</name>
      </author>
      <author>
        <name>Haynes, Laura L</name>
      </author>
      <author>
        <name>Huber, Matthew</name>
      </author>
      <author>
        <name>Snell, Kathryn E</name>
      </author>
      <author>
        <name>Keisling, Benjamin A</name>
      </author>
      <author>
        <name>Konrad, Wilfried</name>
      </author>
      <author>
        <name>Lowenstein, Tim K</name>
      </author>
      <author>
        <name>Malinverno, Alberto</name>
      </author>
      <author>
        <name>Guillermic, Maxence</name>
      </author>
      <author>
        <name>Mejía, Luz María</name>
      </author>
      <author>
        <name>Milligan, Joseph N</name>
      </author>
      <author>
        <name>Morton, John J</name>
      </author>
      <author>
        <name>Nordt, Lee</name>
      </author>
      <author>
        <name>Whiteford, Ross</name>
      </author>
      <author>
        <name>Roth-Nebelsick, Anita</name>
      </author>
      <author>
        <name>Rugenstein, Jeremy KC</name>
      </author>
      <author>
        <name>Schaller, Morgan F</name>
      </author>
      <author>
        <name>Sheldon, Nathan D</name>
      </author>
      <author>
        <name>Sosdian, Sindia</name>
      </author>
      <author>
        <name>Wilkes, Elise B</name>
      </author>
      <author>
        <name>Witkowski, Caitlyn R</name>
      </author>
      <author>
        <name>Zhang, Yi Ge</name>
      </author>
      <author>
        <name>Anderson, Lloyd</name>
      </author>
      <author>
        <name>Beerling, David J</name>
      </author>
      <author>
        <name>Bolton, Clara</name>
      </author>
      <author>
        <name>Cerling, Thure E</name>
      </author>
      <author>
        <name>Cotton, Jennifer M</name>
      </author>
      <author>
        <name>Da, Jiawei</name>
      </author>
      <author>
        <name>Ekart, Douglas D</name>
      </author>
      <author>
        <name>Foster, Gavin L</name>
      </author>
      <author>
        <name>Greenwood, David R</name>
      </author>
      <author>
        <name>Hyland, Ethan G</name>
      </author>
      <author>
        <name>Jagniecki, Elliot A</name>
      </author>
      <author>
        <name>Jasper, John P</name>
      </author>
      <author>
        <name>Kowalczyk, Jennifer B</name>
        <uri>https://orcid.org/0000-0003-2978-1237</uri>
      </author>
      <author>
        <name>Kunzmann, Lutz</name>
      </author>
      <author>
        <name>Kürschner, Wolfram M</name>
      </author>
      <author>
        <name>Lawrence, Charles E</name>
      </author>
      <author>
        <name>Lear, Caroline H</name>
      </author>
      <author>
        <name>Martínez-Botí, Miguel A</name>
      </author>
      <author>
        <name>Maxbauer, Daniel P</name>
      </author>
      <author>
        <name>Montagna, Paolo</name>
      </author>
      <author>
        <name>Naafs, B David A</name>
      </author>
      <author>
        <name>Rae, James WB</name>
      </author>
      <author>
        <name>Raitzsch, Markus</name>
      </author>
      <author>
        <name>Retallack, Gregory J</name>
      </author>
      <author>
        <name>Ring, Simon J</name>
      </author>
      <author>
        <name>Seki, Osamu</name>
      </author>
      <author>
        <name>Sepúlveda, Julio</name>
      </author>
      <author>
        <name>Sinha, Ashish</name>
      </author>
      <author>
        <name>Tesfamichael, Tekie F</name>
      </author>
      <author>
        <name>Tripati, Aradhna</name>
        <uri>https://orcid.org/0000-0002-1695-1754</uri>
      </author>
      <author>
        <name>van der Burgh, Johan</name>
      </author>
      <author>
        <name>Yu, Jimin</name>
      </author>
      <author>
        <name>Zachos, James C</name>
      </author>
      <author>
        <name>Zhang, Laiming</name>
      </author>
    </item>
    <item>
      <title>Climate models show colorado drying sooner and with greater certainty east of the continental divide</title>
      <link>https://escholarship.org/uc/item/7wx0q0z3</link>
      <description>Many studies have examined the aridity of the Colorado River Basin and the possible impacts of climate change which could further strain already over-allocated water resources in the region. Fewer studies have examined the multiple Colorado Rocky Mountain headwater regions specifically. This is especially true of areas East of the Continental Divide, despite water originating there being critical to cities and agriculture in Eastern Colorado and further downstream. This paper explores and compares drying trends in the Eastern and Western Colorado Rocky Mountains using single-model initial-condition large ensembles from ten global climate models. The use of multiple models allows us to identify signals that are consistent across different physics parameterizations, model grids, and other model intricacies. The large ensembles also allow us to quantify the time of emergence of these climate change signals--that is, when did (or when will) the long term change due to anthropogenic...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7wx0q0z3</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Rugg, Allyson</name>
      </author>
      <author>
        <name>McCrary, Rachel</name>
      </author>
      <author>
        <name>Rhoades, Alan</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Yates, David</name>
      </author>
      <author>
        <name>Abel, Mimi</name>
      </author>
      <author>
        <name>Devineni, Naresh</name>
      </author>
    </item>
    <item>
      <title>flat10MIP: an emissions-driven experiment to diagnose the climate response to positive, zero and negative CO2 emissions</title>
      <link>https://escholarship.org/uc/item/5qg0m83w</link>
      <description>Abstract. The proportionality between global mean temperature and cumulative emissions of CO2 predicted in Earth system models (ESMs) is the foundation of carbon budgeting frameworks. Deviations from this behavior could impact estimates of required net-zero timings and negative emissions requirements to meet the Paris Agreement climate targets. However, existing ESM diagnostic experiments do not allow for direct estimation of these deviations as a function of defined emissions pathways. Here, we perform a set of climate model diagnostic experiments for the assessment of transient climate response to cumulative CO2 emissions (TCRE), the Zero Emissions Commitment (ZEC), and climate reversibility metrics in an emissions-driven framework. The emissions-driven experiments provide consistent independent variables simplifying simulation, analysis and interpretation, with emissions rates more comparable to recent levels than existing protocols using model-specific compatible emissions...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5qg0m83w</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Sanderson, Benjamin M</name>
      </author>
      <author>
        <name>Brovkin, Victor</name>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Hohn, David</name>
      </author>
      <author>
        <name>Ilyina, Tatiana</name>
      </author>
      <author>
        <name>Jones, Chris D</name>
      </author>
      <author>
        <name>Koenigk, Torben</name>
      </author>
      <author>
        <name>Koven, Charles</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Li, Hongmei</name>
      </author>
      <author>
        <name>Lawrence, David M</name>
      </author>
      <author>
        <name>Lawrence, Peter</name>
      </author>
      <author>
        <name>Liddicoat, Spencer</name>
      </author>
      <author>
        <name>MacDougall, Andrew H</name>
      </author>
      <author>
        <name>Mengis, Nadine</name>
      </author>
      <author>
        <name>Nicholls, Zebedee</name>
      </author>
      <author>
        <name>O'Rourke, Eleanor</name>
      </author>
      <author>
        <name>Romanou, Anastasia</name>
      </author>
      <author>
        <name>Sandstad, Marit</name>
      </author>
      <author>
        <name>Schwinger, Jörg</name>
      </author>
      <author>
        <name>Séférian, Roland</name>
      </author>
      <author>
        <name>Sentman, Lori T</name>
      </author>
      <author>
        <name>Simpson, Isla R</name>
      </author>
      <author>
        <name>Smith, Chris</name>
      </author>
      <author>
        <name>Steinert, Norman J</name>
      </author>
      <author>
        <name>Swann, Abigail LS</name>
      </author>
      <author>
        <name>Tjiputra, Jerry</name>
      </author>
      <author>
        <name>Ziehn, Tilo</name>
      </author>
    </item>
    <item>
      <title>Orphaned oil and gas well methane emission rates quantified using Gaussian plume inversions of ambient observations</title>
      <link>https://escholarship.org/uc/item/01k5269m</link>
      <description>Abstract. Annually, ∼ 3.6&amp;nbsp;million abandoned oil and gas wells in the US emit a combined ∼ 2.6 Tg methane (CH4), adversely affecting climate and regional air quality. However, these estimates depend on emission factors derived from measuring subpopulations of wells that vary by orders of magnitude due to very limited field sampling and poorly characterized distributions. Currently, US protocols to remediate orphaned wells lacks standardized quantification methods needed to both prioritize plugging and account for emission reductions. Therefore, sensitive, reliable, affordable, and scalable CH4 flux quantification methods are needed. We report the use of a simple Gaussian plume method where the dispersion parameters are constrained by in situ ground measurements of CH4 concentration at four locations 7.5–49 m downwind of the orphan well as well as local winds to estimate the leak rate from an orphan well. We derive a flux of 10.53 ± 1.16 kg CH4 h−1 during a venting procedure...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/01k5269m</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Follansbee, Emily</name>
      </author>
      <author>
        <name>Lee, James E</name>
      </author>
      <author>
        <name>Dubey, Mohit L</name>
      </author>
      <author>
        <name>Dooley, Jonathan F</name>
      </author>
      <author>
        <name>Shuck, Curtis</name>
      </author>
      <author>
        <name>Minschwaner, Ken</name>
      </author>
      <author>
        <name>Santos, Andre</name>
        <uri>https://orcid.org/0000-0002-7320-7649</uri>
      </author>
      <author>
        <name>Biraud, Sebastien C</name>
      </author>
      <author>
        <name>Dubey, Manvendra K</name>
      </author>
    </item>
    <item>
      <title>Climate-carbon feedback tradeoff between Arctic and alpine permafrost under warming</title>
      <link>https://escholarship.org/uc/item/5w2185tp</link>
      <description>Whether greenhouse gas (GHG) emissions from permafrost will trigger positive climate feedbacks under warming remains unknown. Here, we synthesized the response of growing season carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;), methane (CH&lt;sub&gt;4&lt;/sub&gt;), and nitrous oxide (N&lt;sub&gt;2&lt;/sub&gt;O) emissions to experimentally manipulated warming of ~2°C for permafrost in alpine and Arctic regions. Warming weakened the GHG sink of alpine permafrost, thereby increasing (13%) its global warming potential, but strengthened the GHG sink of Arctic permafrost and decreased (-10%) its global warming potential. When warming caused drying of alpine permafrost soils, the CO&lt;sub&gt;2&lt;/sub&gt; sink weakened but the CH&lt;sub&gt;4&lt;/sub&gt; sink increased. In contrast, warming of relatively wet Arctic permafrost increased the CO&lt;sub&gt;2&lt;/sub&gt; sink and CH&lt;sub&gt;4&lt;/sub&gt; source. Warming led to much stronger increases of the N&lt;sub&gt;2&lt;/sub&gt;O source in alpine than Arctic permafrost. Although keeping additional warming below 2°C in permafrost regions...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5w2185tp</guid>
      <pubDate>Tue, 7 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Bao, Tao</name>
      </author>
      <author>
        <name>Xu, Xiyan</name>
      </author>
      <author>
        <name>Jia, Gensuo</name>
      </author>
      <author>
        <name>Zhu, Xingru</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Yang, Yuanhe</name>
      </author>
    </item>
    <item>
      <title>Breaking the reproducibility barrier with standardized protocols for plant–microbiome research</title>
      <link>https://escholarship.org/uc/item/3f14n3jm</link>
      <description>Inter-laboratory replicability is crucial yet challenging in microbiome research. Leveraging microbiomes to promote soil health and plant growth requires understanding underlying molecular mechanisms using reproducible experimental systems. In a global collaborative effort involving five laboratories, we aimed to help advance reproducibility in microbiome studies by testing our ability to replicate synthetic community assembly experiments. Our study compared fabricated ecosystems constructed using two different synthetic bacterial communities, the model grass Brachypodium distachyon, and sterile EcoFAB 2.0 devices. All participating laboratories observed consistent inoculum-dependent changes in plant phenotype, root exudate composition, and final bacterial community structure, where Paraburkholderia sp. OAS925 could dramatically shift microbiome composition. Comparative genomics and exudate utilization linked the pH-dependent colonization ability of Paraburkholderia, which was...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3f14n3jm</guid>
      <pubDate>Tue, 23 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Novak, Vlastimil</name>
        <uri>https://orcid.org/0000-0001-7890-4593</uri>
      </author>
      <author>
        <name>Andeer, Peter F</name>
      </author>
      <author>
        <name>King, Eoghan</name>
      </author>
      <author>
        <name>Calabria, Jacob</name>
      </author>
      <author>
        <name>Fitzpatrick, Connor</name>
      </author>
      <author>
        <name>Kelm, Jana M</name>
      </author>
      <author>
        <name>Wippel, Kathrin</name>
      </author>
      <author>
        <name>Kosina, Suzanne M</name>
      </author>
      <author>
        <name>Bowen, Benjamin P</name>
      </author>
      <author>
        <name>Daum, Chris</name>
      </author>
      <author>
        <name>Zane, Matthew</name>
      </author>
      <author>
        <name>Yadav, Archana</name>
      </author>
      <author>
        <name>Chen, Mingfei</name>
        <uri>https://orcid.org/0000-0002-6281-2480</uri>
      </author>
      <author>
        <name>Russ, Dor</name>
      </author>
      <author>
        <name>Adams, Catharine A</name>
      </author>
      <author>
        <name>Owens, Trenton K</name>
      </author>
      <author>
        <name>Lee, Bradie</name>
      </author>
      <author>
        <name>Ding, Yezhang</name>
      </author>
      <author>
        <name>Sordo, Zineb</name>
      </author>
      <author>
        <name>Chakraborty, Romy</name>
      </author>
      <author>
        <name>Roux, Simon</name>
      </author>
      <author>
        <name>Deutschbauer, Adam M</name>
      </author>
      <author>
        <name>Ushizima, Daniela</name>
        <uri>https://orcid.org/0000-0002-7363-9468</uri>
      </author>
      <author>
        <name>Zengler, Karsten</name>
      </author>
      <author>
        <name>Arsova, Borjana</name>
      </author>
      <author>
        <name>Dangl, Jeffery L</name>
      </author>
      <author>
        <name>Schulze-Lefert, Paul</name>
      </author>
      <author>
        <name>Watt, Michelle</name>
      </author>
      <author>
        <name>Vogel, John P</name>
      </author>
      <author>
        <name>Northen, Trent R</name>
      </author>
    </item>
    <item>
      <title>Simulation of Flow and Salinity in a Large Seasonally Managed Wetland Complex</title>
      <link>https://escholarship.org/uc/item/43s324xx</link>
      <description>Seasonally managed wetlands in the San Joaquin River (SJR) watershed in California provide important benefits to wildlife and humans but are threatened through anthropogenic activity. Wetlands in the SJR are subject to salinity regulation, which poses challenges for wetland management. Salinity management in the SJR basin is supported by a process-based model, the Watershed Analysis Risk Management Framework (WARMF). Wetlands are simulated with a “bathtub” analog where water levels are assumed to be the same over one model compartment and the storage volume depends on depth. The complexity and extent of hydrological features pose challenges for input data acquisition. Two approaches to estimating inflow and pond depth and determining water sources were assessed. Approach 1 used mostly monitored data, while Approach 2 used wetland manager knowledge. Approach 2 predicted outflow and salinity better than Approach 1, and an important benefit was the simulation of water reuse within...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/43s324xx</guid>
      <pubDate>Fri, 12 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Helmrich, Stefanie</name>
      </author>
      <author>
        <name>Quinn, Nigel WT</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
      <author>
        <name>Beutel, Marc W</name>
        <uri>https://orcid.org/0000-0003-2549-8127</uri>
      </author>
      <author>
        <name>O’Day, Peggy A</name>
      </author>
    </item>
    <item>
      <title>Advances in Total Maximum Daily Load Implementation Planning by Modeling Best Management Practices and Green Infrastructures</title>
      <link>https://escholarship.org/uc/item/1xn0z0j0</link>
      <description>In this paper, a review of advances in total maximum daily load (TMDL) implementation planning by modeling best management practices (BMPs) and green infrastructure (GI) practices along with enhanced (hybrid/streamlining) approaches is presented. The review emanates from Chapter 12 of the recent ASCE Manual of Practice on TMDLs. The latest models and modeling tools, specifically the United States Environmental Protection Agency's (USEPA's) GI Modeling Toolkit and the Landscape and Green Infrastructure Design (L-GrlD) model for formulating GI strategies with flexibility to support stakeholder engagement, are reviewed. In addition, other decision support tools that can help advance the state-of-the-practice of TMDL implementation are included in the synthesis. Advances in incorporating model uncertainties related to BMPs and GI practices in TMDL analysis are briefly discussed. Furthermore, enhanced approaches to cost-effective TMDL implementation measures are discussed, which can...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1xn0z0j0</guid>
      <pubDate>Fri, 12 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Borah, Deva K</name>
      </author>
      <author>
        <name>Zhang, Harry X</name>
      </author>
      <author>
        <name>Zellner, Moira</name>
      </author>
      <author>
        <name>Ahmadisharaf, Ebrahim</name>
      </author>
      <author>
        <name>Babbar-Sebens, Meghna</name>
      </author>
      <author>
        <name>Quinn, Nigel WT</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
      <author>
        <name>Kumar, Saurav</name>
      </author>
      <author>
        <name>Sridharan, Vamsi Krishna</name>
      </author>
      <author>
        <name>Leelaruban, Navaratnam</name>
      </author>
      <author>
        <name>Lott, Craig</name>
      </author>
    </item>
    <item>
      <title>Breaking the reproducibility barrier with standardized protocols for plant–microbiome research</title>
      <link>https://escholarship.org/uc/item/7n07963x</link>
      <description>Inter-laboratory replicability is crucial yet challenging in microbiome research. Leveraging microbiomes to promote soil health and plant growth requires understanding underlying molecular mechanisms using reproducible experimental systems. In a global collaborative effort involving five laboratories, we aimed to help advance reproducibility in microbiome studies by testing our ability to replicate synthetic community assembly experiments. Our study compared fabricated ecosystems constructed using two different synthetic bacterial communities, the model grass Brachypodium distachyon, and sterile EcoFAB 2.0 devices. All participating laboratories observed consistent inoculum-dependent changes in plant phenotype, root exudate composition, and final bacterial community structure, where Paraburkholderia sp. OAS925 could dramatically shift microbiome composition. Comparative genomics and exudate utilization linked the pH-dependent colonization ability of Paraburkholderia, which was...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7n07963x</guid>
      <pubDate>Thu, 11 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Novak, Vlastimil</name>
        <uri>https://orcid.org/0000-0001-7890-4593</uri>
      </author>
      <author>
        <name>Andeer, Peter F</name>
      </author>
      <author>
        <name>King, Eoghan</name>
      </author>
      <author>
        <name>Calabria, Jacob</name>
      </author>
      <author>
        <name>Fitzpatrick, Connor</name>
      </author>
      <author>
        <name>Kelm, Jana M</name>
      </author>
      <author>
        <name>Wippel, Kathrin</name>
      </author>
      <author>
        <name>Kosina, Suzanne M</name>
      </author>
      <author>
        <name>Bowen, Benjamin P</name>
      </author>
      <author>
        <name>Daum, Chris</name>
      </author>
      <author>
        <name>Zane, Matthew</name>
      </author>
      <author>
        <name>Yadav, Archana</name>
      </author>
      <author>
        <name>Chen, Mingfei</name>
        <uri>https://orcid.org/0000-0002-6281-2480</uri>
      </author>
      <author>
        <name>Russ, Dor</name>
      </author>
      <author>
        <name>Adams, Catharine A</name>
      </author>
      <author>
        <name>Owens, Trenton K</name>
      </author>
      <author>
        <name>Lee, Bradie</name>
      </author>
      <author>
        <name>Ding, Yezhang</name>
      </author>
      <author>
        <name>Sordo, Zineb</name>
      </author>
      <author>
        <name>Chakraborty, Romy</name>
      </author>
      <author>
        <name>Roux, Simon</name>
        <uri>https://orcid.org/0000-0002-5831-5895</uri>
      </author>
      <author>
        <name>Deutschbauer, Adam M</name>
      </author>
      <author>
        <name>Ushizima, Daniela</name>
        <uri>https://orcid.org/0000-0002-7363-9468</uri>
      </author>
      <author>
        <name>Zengler, Karsten</name>
      </author>
      <author>
        <name>Arsova, Borjana</name>
      </author>
      <author>
        <name>Dangl, Jeffery L</name>
      </author>
      <author>
        <name>Schulze-Lefert, Paul</name>
      </author>
      <author>
        <name>Watt, Michelle</name>
      </author>
      <author>
        <name>Vogel, John P</name>
      </author>
      <author>
        <name>Northen, Trent R</name>
      </author>
    </item>
    <item>
      <title>A Review of Abrupt Permafrost Thaw: Definitions, Usage, and a Proposed Conceptual Framework</title>
      <link>https://escholarship.org/uc/item/9x04n0w7</link>
      <description>Purpose of ReviewWe review how ‘abrupt thaw’ has been used in published studies, compare these definitions to abrupt processes in other Earth science disciplines, and provide a definitive framework for how abrupt thaw should be used in the context of permafrost science.Recent FindingsWe address several aspects of permafrost systems necessary for abrupt thaw to occur and propose a framework for classifying permafrost processes as abrupt thaw in the future. Based on a literature review and our collective expertise, we propose that abrupt thaw refers to thaw processes that lead to a substantial persistent environmental change within a few decades. Abrupt thaw typically occurs in ice-rich permafrost but may be initiated in ice-poor permafrost by external factors such as hydrologic change (i.e., increased streamflow, soil moisture fluctuations, altered groundwater recharge) or wildfire.SummaryPermafrost thaw alters greenhouse gas emissions, soil and vegetation properties, and hydrologic...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9x04n0w7</guid>
      <pubDate>Tue, 9 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Webb, Hailey</name>
      </author>
      <author>
        <name>Fuchs, Matthias</name>
      </author>
      <author>
        <name>Abbott, Benjamin W</name>
      </author>
      <author>
        <name>Douglas, Thomas A</name>
      </author>
      <author>
        <name>Elder, Clayton D</name>
      </author>
      <author>
        <name>Ernakovich, Jessica Gilman</name>
      </author>
      <author>
        <name>Euskirchen, Eugenie S</name>
      </author>
      <author>
        <name>Göckede, Mathias</name>
      </author>
      <author>
        <name>Grosse, Guido</name>
      </author>
      <author>
        <name>Hugelius, Gustaf</name>
      </author>
      <author>
        <name>Jones, Miriam C</name>
      </author>
      <author>
        <name>Koven, Charles</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Kropp, Heather</name>
      </author>
      <author>
        <name>Lathrop, Emma</name>
      </author>
      <author>
        <name>Li, WenWen</name>
      </author>
      <author>
        <name>Loranty, Michael M</name>
      </author>
      <author>
        <name>Natali, Susan M</name>
      </author>
      <author>
        <name>Olefeldt, David</name>
      </author>
      <author>
        <name>Schädel, Christina</name>
      </author>
      <author>
        <name>Schuur, Edward AG</name>
      </author>
      <author>
        <name>Sonnentag, Oliver</name>
      </author>
      <author>
        <name>Strauss, Jens</name>
      </author>
      <author>
        <name>Virkkala, Anna-Maria</name>
      </author>
      <author>
        <name>Turetsky, Merritt R</name>
      </author>
    </item>
    <item>
      <title>Shrub Expansion Can Counteract Carbon Losses From Warming Tundra</title>
      <link>https://escholarship.org/uc/item/8qd596gn</link>
      <description>Abstract  Arctic warming is causing substantial compositional, structural, and functional changes in tundra vegetation including shrub and tree‐line expansion and densification. However, predicting the carbon trajectories of the changing Arctic is challenging due to interacting feedbacks between vegetation composition and structure, and surface characteristics. We conduct a sensitivity analysis of the current‐date to 2100 projected surface energy fluxes, soil carbon pools, and CO 2 fluxes to different shrub expansion rates under future emission scenarios (intermediate—RCP4.5, and high—RCP8.5) using the Arctic‐focused configuration of E3SM Land Model (ELM). We focus on Trail Valley Creek (TVC), an upland tundra site in the western Canadian Arctic, which is experiencing shrub densification and expansion. We find that shrub expansion did not significantly alter the modeled surface energy and water budgets. However, the carbon balance was sensitive to shrub expansion, which drove...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8qd596gn</guid>
      <pubDate>Tue, 9 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Yazbeck, Theresia</name>
      </author>
      <author>
        <name>Bohrer, Gil</name>
      </author>
      <author>
        <name>Sonnentag, Oliver</name>
      </author>
      <author>
        <name>Qu, Bo</name>
      </author>
      <author>
        <name>Detto, Matteo</name>
      </author>
      <author>
        <name>Hould‐Gosselin, Gabriel</name>
      </author>
      <author>
        <name>Graveline, Vincent</name>
      </author>
      <author>
        <name>Alcock, Haley</name>
      </author>
      <author>
        <name>Lecavalier, Bruno</name>
      </author>
      <author>
        <name>Marsh, Philip</name>
      </author>
      <author>
        <name>Cannon, Alex</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Yuan, Fengming</name>
      </author>
      <author>
        <name>Sulman, Benjamin</name>
      </author>
    </item>
    <item>
      <title>Rethinking TMDLs: Perspective Based on Community Survey</title>
      <link>https://escholarship.org/uc/item/8c7824pg</link>
      <description>The study investigated the perspectives of professionals involved in total maximum daily load (TMDL) development. A survey instrument was developed to understand the challenges and advancements necessary to enhance water quality management. This survey explored various dimensions of TMDL development, including identifying impaired waterbodies, water quality modeling, implementation, postimplementation assessment, and stakeholder engagement. Thirty-seven professionals involved in TMDL development took the survey. The results indicated a consensus on the need to reassess existing methodologies, particularly in the postimplementation phase, with a strong emphasis on the importance of sufficient funding for data collection. Limited resources, computational challenges, and a lack of trust in advanced models were identified as barriers to advancing water quality modeling. The participants also recognized the urgency of incorporating more validation data, especially through conventional...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8c7824pg</guid>
      <pubDate>Tue, 9 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Kumar, Saurav</name>
      </author>
      <author>
        <name>Imen, Sanaz</name>
      </author>
      <author>
        <name>Ahmadisharaf, Ebrahim</name>
      </author>
      <author>
        <name>Barranco, Raquel Neri</name>
      </author>
      <author>
        <name>Rabby, Sumon Hossain</name>
      </author>
      <author>
        <name>Ramirez-Avila, John J</name>
      </author>
      <author>
        <name>Sridharan, Vamsi</name>
      </author>
      <author>
        <name>Lott, Craig</name>
      </author>
      <author>
        <name>La Plante, Rosanna</name>
      </author>
      <author>
        <name>Zhang, Harry X</name>
      </author>
      <author>
        <name>Quinn, Nigel WT</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
    </item>
    <item>
      <title>A novel approach to increase accuracy in remotely sensed evapotranspiration through basin water balance and flux tower constraints</title>
      <link>https://escholarship.org/uc/item/3nw6f5r6</link>
      <description>Remote sensing-derived evapotranspiration (RSET) products capture the spatiotemporal variations of evapotranspiration (ET) from field to basin scales with unprecedented details. However, their accuracy varies across RSET estimation methods and diverse hydroclimate regions. While ET modeling efforts to account for biophysical processes and controlling parameters have made good progress in recent years, a parallel approach of integrating in-situ ET with RSET could reduce biases in RSET products. Basin water balance ET (WBET) and flux tower ET are widely applied to evaluate RSET accuracy, yet such ET measurements are rarely used for RSET bias corrections, especially for large area applications. To address this issue, we propose a novel approach: the water balance equivalence (WABE) method, which generates spatially continuous WBET for correcting biases in RSET products. The WABE method computes synthetic WBET by integrating observed WBET and flux tower-derived FLUXCOM ET, which fills...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3nw6f5r6</guid>
      <pubDate>Tue, 9 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Khand, Kul</name>
      </author>
      <author>
        <name>Senay, Gabriel B</name>
      </author>
      <author>
        <name>Friedrichs, MacKenzie</name>
      </author>
      <author>
        <name>Yi, Koong</name>
      </author>
      <author>
        <name>Fisher, Joshua B</name>
        <uri>https://orcid.org/0000-0003-4734-9085</uri>
      </author>
      <author>
        <name>Wang, Lixin</name>
      </author>
      <author>
        <name>Suvočarev, Kosana</name>
      </author>
      <author>
        <name>Ahmadi, Arman</name>
      </author>
      <author>
        <name>Chu, Housen</name>
        <uri>https://orcid.org/0000-0002-8131-4938</uri>
      </author>
      <author>
        <name>Good, Stephen</name>
      </author>
      <author>
        <name>Mallick, Kanishka</name>
      </author>
      <author>
        <name>Missik, Justine</name>
      </author>
      <author>
        <name>Nelson, Jacob A</name>
      </author>
      <author>
        <name>Reed, David E</name>
      </author>
      <author>
        <name>Wang, Tianxin</name>
      </author>
      <author>
        <name>Xiao, Xiangming</name>
      </author>
    </item>
    <item>
      <title>Central Valley Hydrologic Model Version 2 (CVHM2): Decision Support Tool for Groundwater and Land Subsidence Management</title>
      <link>https://escholarship.org/uc/item/2dk476js</link>
      <description>The San Joaquin Valley (SJV) of California is one of the world’s most productive agricultural regions. Reliance on groundwater has led to some of the greatest rates of human-induced land subsidence in the world in the 20th century, as well as more recently. The United States Geological Survey (USGS) has recently developed an integrated surface–subsurface hydrologic model, the Central Valley Hydrologic Model 2 (CVHM2), that represents the major components of the hydrologic system of California’s Central Valley. In this study, CVHM2 was applied as a decision support tool while simulating various management strategies to mitigate the land subsidence caused by the extraction of groundwater. CVHM2 was extended through to 2073 and applied to simulate management scenarios in terms of three primary drivers and their impact on subsidence along the Delta–Mendota Canal (DMC), a critical piece of infrastructure in the western SJV. The drivers considered were agricultural water demands, managed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2dk476js</guid>
      <pubDate>Tue, 9 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Nelson, Kirk</name>
      </author>
      <author>
        <name>Quinn, Nigel</name>
        <uri>https://orcid.org/0000-0003-3333-4763</uri>
      </author>
      <author>
        <name>Traum, Jonathan</name>
      </author>
    </item>
    <item>
      <title>A stable 15-member bacterial SynCom promotes Brachypodium growth under drought stress</title>
      <link>https://escholarship.org/uc/item/52q5c76b</link>
      <description>Introduction: Rhizosphere microbiomes are known to drive soil nutrient cycling and influence plant fitness during adverse environmental conditions. Field-derived robust Synthetic Communities (SynComs) of microbes mimicking the diversity of rhizosphere microbiomes can greatly advance a deeper understanding of such processes. However, assembling stable, genetically tractable, reproducible, and scalable SynComs remains challenging.
Methods: Here, we present a systematic approach using a combination of network analysis and cultivation-guided methods to construct a 15-member SynCom from the rhizobiome of &lt;i&gt;Brachypodium distachyon&lt;/i&gt;. This SynCom incorporates diverse strains from five bacterial phyla. Genomic analysis of the individual strains was performed to reveal encoded plant growth-promoting traits, including genes for the synthesis of osmoprotectants (trehalose and betaine) and Na&lt;sup&gt;+&lt;/sup&gt;/K&lt;sup&gt;+&lt;/sup&gt; transporters, and some predicted traits were validated by laboratory...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/52q5c76b</guid>
      <pubDate>Mon, 8 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Yadav, Archana</name>
      </author>
      <author>
        <name>Chen, Mingfei</name>
        <uri>https://orcid.org/0000-0002-6281-2480</uri>
      </author>
      <author>
        <name>Acharya, Shwetha M</name>
      </author>
      <author>
        <name>Kim, Grace</name>
      </author>
      <author>
        <name>Yang, Yuguo</name>
        <uri>https://orcid.org/0000-0001-5801-6257</uri>
      </author>
      <author>
        <name>Zhao, Tiffany Z</name>
      </author>
      <author>
        <name>Tsang, Eunice</name>
      </author>
      <author>
        <name>Chakraborty, Romy</name>
      </author>
    </item>
    <item>
      <title>One‐at‐a‐Time Parameter Perturbation Ensemble of the Community Land Model, Version 5.1</title>
      <link>https://escholarship.org/uc/item/0561v5ct</link>
      <description>Abstract Comprehensive land models are subject to significant parametric uncertainty, which can be hard to quantify due to the large number of parameters and high model computational costs. We constructed a large parameter perturbation ensemble (PPE) for the Community Land Model version 5.1 with biogeochemistry configuration (CLM5.1‐BGC). We performed more than 2,000 simulations perturbing 211 parameters across six forcing scenarios. This provides an expansive data set, which can be used to identify the most influential parameters on a wide range of output variables globally, by biome, or by plant functional type. We found that parameter effects can exceed scenario effects and that a small number of parameters explains a large fraction of variance across our ensemble. The most important parameters can differ regionally and also based on the forcing scenario. The software infrastructure developed for this experiment has greatly reduced the human and computer time needed for CLM...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0561v5ct</guid>
      <pubDate>Mon, 8 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Kennedy, D</name>
      </author>
      <author>
        <name>Dagon, K</name>
      </author>
      <author>
        <name>Lawrence, DM</name>
      </author>
      <author>
        <name>Fisher, RA</name>
      </author>
      <author>
        <name>Sanderson, BM</name>
      </author>
      <author>
        <name>Collier, N</name>
      </author>
      <author>
        <name>Hoffman, FM</name>
      </author>
      <author>
        <name>Koven, CD</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Kluzek, E</name>
      </author>
      <author>
        <name>Levis, S</name>
      </author>
      <author>
        <name>Lu, X</name>
      </author>
      <author>
        <name>Oleson, KW</name>
      </author>
      <author>
        <name>Zarakas, CM</name>
      </author>
      <author>
        <name>Cheng, Y</name>
      </author>
      <author>
        <name>Foster, AC</name>
      </author>
      <author>
        <name>Fowler, MD</name>
      </author>
      <author>
        <name>Hawkins, LR</name>
      </author>
      <author>
        <name>Kavoo, T</name>
      </author>
      <author>
        <name>Kumar, S</name>
      </author>
      <author>
        <name>Newman, AJ</name>
      </author>
      <author>
        <name>Lawrence, PJ</name>
      </author>
      <author>
        <name>Li, F</name>
      </author>
      <author>
        <name>Lombardozzi, DL</name>
      </author>
      <author>
        <name>Luo, Y</name>
      </author>
      <author>
        <name>Shuman, JK</name>
      </author>
      <author>
        <name>Swann, ALS</name>
      </author>
      <author>
        <name>Swenson, SC</name>
      </author>
      <author>
        <name>Tang, G</name>
      </author>
      <author>
        <name>Wieder, WR</name>
      </author>
      <author>
        <name>Wood, AW</name>
      </author>
    </item>
    <item>
      <title>Unraveling the ecological success of Iodidimonas in a bioreactor treating oil and gas produced water</title>
      <link>https://escholarship.org/uc/item/2w81k291</link>
      <description>&lt;i&gt;Iodidimonas&lt;/i&gt; sp., a bacterium found in bioreactors treating oil and gas produced water as well as iodide-rich brines, has garnered attention for its unique ability to oxidize iodine. However, little is known about the metabolic capabilities that enable &lt;i&gt;Iodidimonas&lt;/i&gt; sp. to thrive in certain unique ecological niches. In this study, we isolated, characterized, and sequenced three strains belonging to the &lt;i&gt;Iodidimonas&lt;/i&gt; genus from the sludge of a membrane bioreactor used for produced water treatment. We investigated the genomic features of these isolates and compared them with the four publicly available isolate genomes from this genus, as well as a metagenome-assembled genome from the source bioreactor. Our &lt;i&gt;Iodidimonas&lt;/i&gt; isolates had several genes associated with mitigating salinity, heavy metal, and organic compound stress, which likely help these bacteria to survive in produced water. Phenotyping tests revealed that while the isolates could utilize a wide variety...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2w81k291</guid>
      <pubDate>Fri, 5 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Acharya, Shwetha M</name>
      </author>
      <author>
        <name>Yang, Yuguo</name>
        <uri>https://orcid.org/0000-0001-5801-6257</uri>
      </author>
      <author>
        <name>Enalls, Brandon C</name>
      </author>
      <author>
        <name>Walian, Peter J</name>
      </author>
      <author>
        <name>Van Houghton, Brett D</name>
      </author>
      <author>
        <name>Rosenblum, James S</name>
      </author>
      <author>
        <name>Cath, Tzahi Y</name>
      </author>
      <author>
        <name>Tringe, Susannah G</name>
        <uri>https://orcid.org/0000-0001-6479-8427</uri>
      </author>
      <author>
        <name>Chakraborty, Romy</name>
      </author>
    </item>
    <item>
      <title>Global variation in vegetation carbon use efficiency inferred from eddy covariance observations</title>
      <link>https://escholarship.org/uc/item/612206qk</link>
      <description>Terrestrial ecosystems have been serving as a strong carbon sink that offsets one-quarter of anthropogenic CO2 emissions. Carbon use efficiency (CUE), the percentage of photosynthesized carbon that is available for biomass production and other secondary carbon products, is one factor determining the carbon sink size. The global variation in CUE remains unclear, however, as recent reports disagree over the responses of CUE to temperature, dryness, forest types and stand age, and there are limited direct observations to constrain the related uncertainty. Here, we propose to infer CUE from spatially distributed observations of land–atmosphere CO2 exchange from global eddy covariance sites based on the degree of ecosystem respiration–photosynthesis coupling. Across 2,737 site-years, CUE derived from eddy covariance observations is 0.43 ± 0.12, consistent with previous inventory-based estimates (0.47 ± 0.12, n = 301) but with a better representation of spatial–temporal variation in...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/612206qk</guid>
      <pubDate>Thu, 28 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Luo, Xiangzhong</name>
      </author>
      <author>
        <name>Zhao, Ruiying</name>
      </author>
      <author>
        <name>Chu, Housen</name>
        <uri>https://orcid.org/0000-0002-8131-4938</uri>
      </author>
      <author>
        <name>Collalti, Alessio</name>
      </author>
      <author>
        <name>Fatichi, Simone</name>
      </author>
      <author>
        <name>Keenan, Trevor F</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
      <author>
        <name>Lu, Xinchen</name>
      </author>
      <author>
        <name>Nguyen, Ngoc</name>
      </author>
      <author>
        <name>Prentice, I Colin</name>
      </author>
      <author>
        <name>Sun, Wu</name>
      </author>
      <author>
        <name>Yu, Kailiang</name>
      </author>
      <author>
        <name>Yu, Liyao</name>
      </author>
    </item>
    <item>
      <title>Widespread underestimation of rain-induced soil carbon emissions from global drylands</title>
      <link>https://escholarship.org/uc/item/37r947zw</link>
      <description>Dryland carbon fluxes, particularly those driven by ecosystem respiration, are highly sensitive to water availability and rain pulses. However, the magnitude of rain-induced carbon emissions remains unclear globally. Here we quantify the impact of rain-pulse events on the carbon balance of global drylands and characterize their spatiotemporal controls. Using eddy-covariance observations of carbon, water and energy fluxes from 34 dryland sites worldwide, we produce an inventory of over 1,800 manually identified rain-induced CO2 pulse events. Based on this inventory, a machine learning algorithm is developed to automatically detect rain-induced CO2 pulse events. Our findings show that existing partitioning methods underestimate ecosystem respiration and photosynthesis by up to 30% during rain-pulse events, which annually contribute 16.9 ± 2.8% of ecosystem respiration and 9.6 ± 2.2% of net ecosystem productivity. We show that the carbon loss intensity correlates most strongly with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/37r947zw</guid>
      <pubDate>Thu, 28 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Nguyen, Ngoc B</name>
      </author>
      <author>
        <name>Migliavacca, Mirco</name>
      </author>
      <author>
        <name>Bassiouni, Maoya</name>
        <uri>https://orcid.org/0000-0001-5795-9894</uri>
      </author>
      <author>
        <name>Baldocchi, Dennis D</name>
        <uri>https://orcid.org/0000-0003-3496-4919</uri>
      </author>
      <author>
        <name>Gherardi, Laureano A</name>
      </author>
      <author>
        <name>Green, Julia K</name>
      </author>
      <author>
        <name>Papale, Dario</name>
      </author>
      <author>
        <name>Reichstein, Markus</name>
      </author>
      <author>
        <name>Cohrs, Kai-Hendrik</name>
      </author>
      <author>
        <name>Cescatti, Alessandro</name>
      </author>
      <author>
        <name>Nguyen, Tuan Dung</name>
      </author>
      <author>
        <name>Nguyen, Hoang H</name>
      </author>
      <author>
        <name>Nguyen, Quang Minh</name>
      </author>
      <author>
        <name>Keenan, Trevor F</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
    </item>
    <item>
      <title>Exploration of volatile organic compounds (VOCs) from trees in Central Amazonian, Brazil</title>
      <link>https://escholarship.org/uc/item/5241f7r0</link>
      <description>The Amazon rainforest is a critical ecosystem renowned for its biodiversity and substantial contributions to the global climate system. Among the various processes occurring within this environment, the emission of volatile organic compounds (VOCs) plays diverse roles, including functioning as plant defense mechanisms against herbivores and pathogens, facilitating ecological interactions, and providing potential applications for chemotaxonomy. This study examined the VOCs profiles of forest species in Central Amazonia to assess their chemotyping potential. Samples were collected from permanent plots at the Tropical Silviculture Experimental Station (Amazonas, Brazil), and a thermal desorption gas chromatography–mass spectrometry system was used to detect the compounds. A total of 28 volatile were identified, encompassing monoterpenes, sesquiterpenes, aldehydes, alcohols, isoprenes, acids, and heterocyclic aromatics. The Burseraceae family presented the greatest diversity of compounds,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5241f7r0</guid>
      <pubDate>Tue, 26 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>da Silva Menezes, Valdiek</name>
      </author>
      <author>
        <name>Jardine, Kolby Jeremiah</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>do Nascimento, Cristiano Souza</name>
      </author>
      <author>
        <name>de Oliveira Piva, Luani Rosa</name>
      </author>
      <author>
        <name>Durgante, Flavia Machado</name>
      </author>
      <author>
        <name>Lima, Adriano José Nogueira</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
    </item>
    <item>
      <title>Evolutionary and functional relationships between plant and microbial C1 metabolism in terrestrial ecosystems</title>
      <link>https://escholarship.org/uc/item/39v634bh</link>
      <description>One-carbon (C&lt;sub&gt;1&lt;/sub&gt;) metabolism, centered on the universal methyl donor S-adenosyl methionine (SAM), plays critical roles in biosynthesis, redox regulation, and stress responses across plants and microbes. A recently proposed photosynthetic C&lt;sub&gt;1&lt;/sub&gt; pathway links SAM methyl groups directly to RuBisCO-mediated CO&lt;sub&gt;2&lt;/sub&gt; assimilation and integrates with nitrogen and sulfur metabolism. Light-dependent SAM synthesis may regulate the methylation of biopolymers and specialized metabolites and help mitigate photorespiratory stress under elevated temperature and drought. Phylogenetic analysis of two core enzymes suggests evolutionary continuity from methylotrophic microbes to land plants, supporting microbial origins via endosymbiotic gene transfer. Beyond intracellular roles, C&lt;sub&gt;1&lt;/sub&gt; metabolism drives biosphere-atmosphere exchange via gases such as methane, methanol, formic acid, and formaldehyde, and numerous specialized volatiles synthesized through SAM methylation....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/39v634bh</guid>
      <pubDate>Tue, 26 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Honeker, Linnea K</name>
      </author>
      <author>
        <name>Zhang, Zhaoxin</name>
      </author>
      <author>
        <name>Kengdo, Steve Kwatcho</name>
      </author>
      <author>
        <name>Yang, Yuguo</name>
        <uri>https://orcid.org/0000-0001-5801-6257</uri>
      </author>
      <author>
        <name>Roscioli, Joseph</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
    </item>
    <item>
      <title>Real-Time Partitioning of Diurnal Stem CO2 Efflux into Local Stem Respiration and Xylem Transport Processes</title>
      <link>https://escholarship.org/uc/item/06p7s99v</link>
      <description>The apparent respiratory quotient (ARQ) of tree stems, defined as the ratio of net stem CO2 efflux (ES_CO2) to net stem O2 influx (ES_O2), offers insights into the balance between local respiratory CO2 production and CO2 transported via the xylem. Traditional static chamber methods for measuring ARQ can introduce artifacts and obscure natural diurnal variations. Here, we employed an open flow-through stem chamber with ambient air coupled with cavity ring-down spectrometry, which uses the molecular properties of CO2 and O2 molecules to continuously measure ES_CO2, ES_O2, and ARQ, at the base of a California cherry tree (Prunus ilicifolia) during the 2024 growing season. Measurements across three stem chambers over 3–11-day periods revealed strong correlations between ES_CO2 and ES_O2 and mean ARQ values ranging from 1.3 to 2.9, far exceeding previous reports. Two distinct diurnal ARQ patterns were observed: daytime suppression with nighttime recovery, and a morning peak followed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/06p7s99v</guid>
      <pubDate>Tue, 26 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Oliveira, Regison</name>
      </author>
      <author>
        <name>Ajami, Parsa</name>
      </author>
      <author>
        <name>Knox, Ryan</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Koven, Charlie</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Gimenez, Bruno</name>
      </author>
      <author>
        <name>Spanner, Gustavo</name>
      </author>
      <author>
        <name>Warren, Jeffrey</name>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Tcherkez, Guillaume</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
    </item>
    <item>
      <title>Vulnerability of mineral-organic associations in the rhizosphere</title>
      <link>https://escholarship.org/uc/item/6cn3q2tj</link>
      <description>The majority of soil carbon (C) is stored in organic matter associated with reactive minerals. These mineral-organic associations (MOAs) inhibit microbial and enzymatic access to organic matter, suggesting that organic&amp;nbsp;C within MOAs is resistant to decomposition. However, plant roots and rhizosphere microbes are known to transform minerals through dissolution and exchange reactions, implying that MOAs in the rhizosphere can be dynamic. Here we identify key drivers, mechanisms, and controls of MOA disruption in the rhizosphere and present a new conceptual framework for the vulnerability of soil&amp;nbsp;C within MOAs. We introduce a vulnerability spectrum that highlights how MOAs characteristic of certain ecosystems are particularly susceptible to specific root-driven disruption mechanisms. This vulnerability spectrum provides a framework for critically assessing the importance of MOA disruption mechanisms at the ecosystem scale. Comprehensive representation of not only root-driven...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6cn3q2tj</guid>
      <pubDate>Thu, 14 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Bölscher, Tobias</name>
      </author>
      <author>
        <name>Cardon, Zoe G</name>
      </author>
      <author>
        <name>Garcia Arredondo, Mariela</name>
      </author>
      <author>
        <name>Grand, Stéphanie</name>
      </author>
      <author>
        <name>Griffen, Gabriella</name>
      </author>
      <author>
        <name>Hestrin, Rachel</name>
      </author>
      <author>
        <name>Imboden, Josephine</name>
      </author>
      <author>
        <name>Jamoteau, Floriane</name>
      </author>
      <author>
        <name>Lacroix, Emily M</name>
      </author>
      <author>
        <name>Pérez Castro, Sherlynette</name>
      </author>
      <author>
        <name>Persson, Per</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Keiluweit, Marco</name>
      </author>
    </item>
    <item>
      <title>Evaluating How Climate Adaptation Measures Affect the Interconnected Water‐Energy Resource Systems of the Western United States</title>
      <link>https://escholarship.org/uc/item/0jn752fw</link>
      <description>Abstract The Western US faces increasing water stress from the impacts of climate change, making it difficult to meet water demands for the region's cities, agriculture, and hydropower generators. Existing literature suggests that climate adaptation measures such as water conservation, cropland retirement, wastewater recycling, and managed aquifer recharge can alleviate some of these challenges. Few analyses, however, compare the relative efficacy and system‐wide effects of these adaptations under different climate projections across the entire Western United States. Here we use a Western US‐wide water systems model to evaluate, by sector and sub‐region, how the widespread implementation of these adaptive measures impacts water demands, water deliveries, and electricity use related to the water system for three different climate projections. We find that wastewater recycling has greater potential to lower unmet indoor water demands than urban indoor water conservation measures....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0jn752fw</guid>
      <pubDate>Thu, 14 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Singhal, A</name>
      </author>
      <author>
        <name>Szinai, JK</name>
        <uri>https://orcid.org/0000-0003-2030-3642</uri>
      </author>
      <author>
        <name>Yates, D</name>
      </author>
      <author>
        <name>Jones, AD</name>
        <uri>https://orcid.org/0000-0002-1913-7870</uri>
      </author>
    </item>
    <item>
      <title>The effect of African Easterly Wave suppression by periodicity on Atlantic tropical cyclones</title>
      <link>https://escholarship.org/uc/item/8198r202</link>
      <description>Research has shown that suppressing African Easterly Waves (AEWs) does not reduce basin-wide North Atlantic tropical cyclone (TC) frequency but can enhance TC environmental favorability. We investigated the AEW-TC relationship further by examining the effects of suppressing the two AEW periodicities individually on TC activity. Using regional model simulations, AEWs were prescribed or suppressed in the 2–6 d or 6–10 d ranges through the lateral boundary conditions. Seasonal TC frequency increased significantly when either AEW periodicity was suppressed, with a larger increase when the 2–6 d waves were suppressed. We also found that suppressing the 2–6 d waves increased mid-tropospheric moisture by up to 8%, as well as overall atmospheric instability, near the western coast of northern Africa. Furthermore, the convective disturbances that developed into TCs exhibited stronger rotation, increased ascending motion, and higher rainfall. Our results suggest that reduced 2–6 d AEW activity...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8198r202</guid>
      <pubDate>Wed, 13 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Danso, Derrick K</name>
      </author>
      <author>
        <name>Patricola-DiRosario, Christina M</name>
      </author>
      <author>
        <name>Bercos-Hickey, Emily</name>
        <uri>https://orcid.org/0000-0002-4935-6556</uri>
      </author>
      <author>
        <name>Lavaysse, Christophe</name>
      </author>
    </item>
    <item>
      <title>Regional and Temporal Variability of Atmospheric River Seasonality: Influences of Detection Algorithms and Moisture Transport Dynamics</title>
      <link>https://escholarship.org/uc/item/3n25k0bm</link>
      <description>Abstract Understanding the regional and temporal variability of atmospheric river (AR) seasonality is crucial for preparedness and mitigation of extreme events. While ARs were thought to peak in winter, recent research shows they exhibit region‐specific seasonality and are heavily influenced by the chosen detection algorithm. This study examines the link between the year‐to‐year consistency of peak‐AR activity to the presence of a dominant seasonal pattern, considering both location and algorithm choice. Regions are categorized by their temporal characteristics: consistent patterns (e.g., East Asia), patterns with occasional outliers (e.g., British Columbia coast), and regions lacking a clear dominant peak season (e.g., South Atlantic, parts of Australia). Hence, not all regions display a consistent seasonal cycle of AR activity. This study quantifies the extent to which a region experiences a dominant peak season of AR activity (or lacks one) and offers insights to enhance decision‐making...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3n25k0bm</guid>
      <pubDate>Wed, 13 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Kamnani, Diya</name>
      </author>
      <author>
        <name>O’Brien, Travis A</name>
      </author>
      <author>
        <name>Smith, Samuel</name>
      </author>
      <author>
        <name>Staten, Paul W</name>
      </author>
      <author>
        <name>Shields, Christine A</name>
      </author>
    </item>
    <item>
      <title>Network of networks: Time series clustering of AmeriFlux sites</title>
      <link>https://escholarship.org/uc/item/0z1776kn</link>
      <description>Environmental observation networks, such as AmeriFlux, are foundational for monitoring ecosystem response to climate change, management practices, and natural disturbances; however, their effectiveness depends on their representativeness for the regions or continents. We proposed an empirical, time series approach to quantify the similarity of ecosystem fluxes across AmeriFlux sites. We extracted the diel and seasonal characteristics (i.e., amplitudes, phases) from carbon dioxide, water vapor, energy, and momentum fluxes, which reflect the effects of climate, plant phenology, and ecophysiology on the observations, and explored the potential aggregations of AmeriFlux sites through hierarchical clustering. While net radiation and temperature showed latitudinal clustering as expected, flux variables revealed a more uneven clustering with many small (number of sites &amp;lt; 5), unique groups and a few large (&amp;gt; 100) to intermediate (15–70) groups, highlighting the significant ecological...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0z1776kn</guid>
      <pubDate>Wed, 13 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Reed, David E</name>
      </author>
      <author>
        <name>Chu, Housen</name>
        <uri>https://orcid.org/0000-0002-8131-4938</uri>
      </author>
      <author>
        <name>Peter, Brad G</name>
      </author>
      <author>
        <name>Chen, Jiquan</name>
      </author>
      <author>
        <name>Abraha, Michael</name>
      </author>
      <author>
        <name>Amiro, Brian</name>
      </author>
      <author>
        <name>Anderson, Ray G</name>
        <uri>https://orcid.org/0000-0002-6202-5890</uri>
      </author>
      <author>
        <name>Arain, M Altaf</name>
      </author>
      <author>
        <name>Arruda, Paulo</name>
      </author>
      <author>
        <name>Barron-Gafford, Greg A</name>
      </author>
      <author>
        <name>Bernacchi, Carl</name>
      </author>
      <author>
        <name>Beverly, Daniel P</name>
      </author>
      <author>
        <name>Biraud, Sebastien C</name>
      </author>
      <author>
        <name>Black, T Andrew</name>
      </author>
      <author>
        <name>Blanken, Peter D</name>
      </author>
      <author>
        <name>Bohrer, Gil</name>
      </author>
      <author>
        <name>Bowler, Rebecca</name>
      </author>
      <author>
        <name>Bowling, David R</name>
      </author>
      <author>
        <name>Bret-Harte, M Syndonia</name>
      </author>
      <author>
        <name>Bretfeld, Mario</name>
      </author>
      <author>
        <name>Brunsell, Nathaniel A</name>
      </author>
      <author>
        <name>Bullock, Stephen H</name>
      </author>
      <author>
        <name>Celis, Gerardo</name>
      </author>
      <author>
        <name>Chen, Xingyuan</name>
      </author>
      <author>
        <name>Classen, Aimee T</name>
      </author>
      <author>
        <name>Cook, David R</name>
      </author>
      <author>
        <name>Cueva, Alejandro</name>
      </author>
      <author>
        <name>Dalmagro, Higo J</name>
      </author>
      <author>
        <name>Davis, Kenneth</name>
      </author>
      <author>
        <name>Desai, Ankur</name>
      </author>
      <author>
        <name>Duff, Alison J</name>
      </author>
      <author>
        <name>Dunn, Allison L</name>
      </author>
      <author>
        <name>Durden, David</name>
      </author>
      <author>
        <name>Edgar, Colin W</name>
      </author>
      <author>
        <name>Euskirchen, Eugenie</name>
      </author>
      <author>
        <name>Bracho, Rosvel</name>
      </author>
      <author>
        <name>Ewers, Brent</name>
      </author>
      <author>
        <name>Flanagan, Lawrence B</name>
      </author>
      <author>
        <name>Florian, Christopher</name>
      </author>
      <author>
        <name>Foord, Vanessa</name>
      </author>
      <author>
        <name>Forbrich, Inke</name>
      </author>
      <author>
        <name>Forsythe, Brandon R</name>
      </author>
      <author>
        <name>Frank, John</name>
      </author>
      <author>
        <name>Garatuza-Payan, Jaime</name>
      </author>
      <author>
        <name>Goslee, Sarah</name>
      </author>
      <author>
        <name>Gough, Christopher</name>
      </author>
      <author>
        <name>Green, Mark</name>
      </author>
      <author>
        <name>Griffis, Timothy</name>
      </author>
      <author>
        <name>Helbig, Manuel</name>
      </author>
      <author>
        <name>Hill, Andrew C</name>
      </author>
      <author>
        <name>Hinkle, Ross</name>
      </author>
      <author>
        <name>Horne, Jason</name>
      </author>
      <author>
        <name>Humphreys, Elyn</name>
      </author>
      <author>
        <name>Ikawa, Hiroki</name>
      </author>
      <author>
        <name>Iwahana, Go</name>
      </author>
      <author>
        <name>Jassal, Rachhpal</name>
      </author>
      <author>
        <name>Johnson, Bruce</name>
      </author>
      <author>
        <name>Johnson, Mark</name>
      </author>
      <author>
        <name>Kannenberg, Steven A</name>
      </author>
      <author>
        <name>Kelsey, Eric</name>
      </author>
      <author>
        <name>King, John</name>
      </author>
      <author>
        <name>Knowles, John F</name>
      </author>
      <author>
        <name>Knox, Sara</name>
      </author>
      <author>
        <name>Kobayashi, Hideki</name>
      </author>
      <author>
        <name>Kolb, Thomas</name>
      </author>
      <author>
        <name>Kolka, Randy</name>
      </author>
      <author>
        <name>Krauss, Ken W</name>
      </author>
      <author>
        <name>Kutzbach, Lars</name>
      </author>
      <author>
        <name>Lamb, Brian</name>
      </author>
      <author>
        <name>Law, Beverly</name>
      </author>
      <author>
        <name>Lee, Sung-Ching</name>
      </author>
      <author>
        <name>Lee, Xuhui</name>
      </author>
      <author>
        <name>Liu, Heping</name>
      </author>
      <author>
        <name>Loescher, Henry W</name>
      </author>
      <author>
        <name>Malone, Sparkle L</name>
      </author>
      <author>
        <name>Matamala, Roser</name>
      </author>
      <author>
        <name>Mauritz, Marguerite</name>
      </author>
      <author>
        <name>Metzger, Stefan</name>
      </author>
      <author>
        <name>Meyer, Gesa</name>
      </author>
      <author>
        <name>Mitra, Bhaskar</name>
      </author>
      <author>
        <name>Munger, J William</name>
      </author>
      <author>
        <name>Nesic, Zoran</name>
      </author>
      <author>
        <name>Noormets, Asko</name>
      </author>
      <author>
        <name>O'Halloran, Thomas L</name>
      </author>
      <author>
        <name>O'Keeffe, Patrick T</name>
      </author>
      <author>
        <name>Oberbauer, Steven F</name>
      </author>
      <author>
        <name>Oechel, Walter</name>
      </author>
      <author>
        <name>Oikawa, Patty</name>
      </author>
      <author>
        <name>Olivas, Paulo C</name>
      </author>
      <author>
        <name>Ouimette, Andrew</name>
      </author>
      <author>
        <name>Pastorello, Gilberto</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>Perez-Quezada, Jorge F</name>
      </author>
      <author>
        <name>Phillips, Claire</name>
      </author>
      <author>
        <name>Posse, Gabriela</name>
      </author>
      <author>
        <name>Qu, Bo</name>
      </author>
      <author>
        <name>Quinton, William L</name>
      </author>
      <author>
        <name>Reba, Michele L</name>
      </author>
      <author>
        <name>Richardson, Andrew D</name>
      </author>
      <author>
        <name>Picasso, Valentin</name>
      </author>
      <author>
        <name>Rocha, Adrian V</name>
      </author>
    </item>
    <item>
      <title>Molecular diversity of dissolved organic matter reflects macroecological patterns in river networks</title>
      <link>https://escholarship.org/uc/item/51j8g8rs</link>
      <description>Deciphering dissolved organic matter (DOM) molecular complexity is crucial for understanding ecosystem function. Using the continental-scale Worldwide Hydrobiogeochemistry Observation Network for Dynamic Rivers Systems (WHONDRS) Fourier-transform ion cyclotron resonance mass spectrometry (FTICR-MS) dataset, we reveal fundamental scaling patterns of DOM chemodiversity with watershed characteristics. Analysis of 54 river sites shows local and regional watershed features significantly influence DOM chemodiversity (2500–8718 unique formulae), exhibiting consistent scaling patterns across compound classes and a novel latitudinal gradient (decreasing diversity with increasing latitude). Scaling relationships for DOM composition vary by compound class. Crucially, the scaling parameters (B, baseline chemodiversity; Z, sensitivity) are linearly interrelated. This B–Z relationship is most robust for potentially bio-labile carbohydrates (coefficient of determination R2 ≈ 0.85), diminishing...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/51j8g8rs</guid>
      <pubDate>Fri, 1 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Freeman, Erika C</name>
      </author>
      <author>
        <name>Mudunuru, Maruti K</name>
      </author>
      <author>
        <name>Feeser, Kelli L</name>
      </author>
      <author>
        <name>McClure, Emily Ann</name>
      </author>
      <author>
        <name>González-Pinzón, Ricardo</name>
      </author>
      <author>
        <name>Ward, Christopher S</name>
      </author>
      <author>
        <name>Bottos, Eric M</name>
      </author>
      <author>
        <name>Krause, Stefan</name>
      </author>
      <author>
        <name>Peña, Jasquelin</name>
      </author>
      <author>
        <name>Newcomer, Michelle E</name>
        <uri>https://orcid.org/0000-0001-5138-9026</uri>
      </author>
    </item>
    <item>
      <title>Climate Extremes and Protests in India, Pakistan, and Bangladesh, 1995–2013</title>
      <link>https://escholarship.org/uc/item/59z2j9z8</link>
      <description>Abstract: 

Scientists have shown a relationship between climate conditions and social unrest, specifically related to temperature and precipitation trends. Though deviations from historically normative patterns are becoming more pronounced, it remains unclear how or to what extent they might be linked to protests. Similarly, we know little about the extent to which the relationships between local climate anomalies and protests are contemporaneous versus lagged. To address these questions, we examine correlates of local protest levels between 1995 and 2013 in India, Pakistan, and Bangladesh. Our innovative methodology involves modeling geocoded, media-reported protests (derived from the Integrated Crisis Early Warning System) at 0.5° × 0.5° geospatial resolution, using unobtrusive, satellite-derived data on temperature and precipitation patterns and historical deviations. We also integrate comparable satellite data on nightlight pollution. Properties of our outcome variable require...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/59z2j9z8</guid>
      <pubDate>Tue, 29 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Werum, Regina</name>
      </author>
      <author>
        <name>Hayes, Michael</name>
      </author>
      <author>
        <name>Schaefer, Daniel</name>
      </author>
      <author>
        <name>Zhang, Beichen</name>
        <uri>https://orcid.org/0000-0002-5910-2883</uri>
      </author>
    </item>
    <item>
      <title>Atmospheric River Detection Under Changing Seasonality and Mean‐State Climate: ARTMIP Tier 2 Paleoclimate Experiments</title>
      <link>https://escholarship.org/uc/item/8js796qm</link>
      <description>Abstract  Atmospheric rivers (ARs) are filamentary structures within the atmosphere that account for a substantial portion of poleward moisture transport and play an important role in Earth's hydroclimate. However, there is no one quantitative definition for what constitutes an atmospheric river, leading to uncertainty in quantifying how these systems respond to global change. This study seeks to better understand how different AR detection tools (ARDTs) respond to changes in climate states utilizing single‐forcing climate model experiments under the aegis of the Atmospheric River Tracking Method Intercomparison Project (ARTMIP). We compare a simulation with an early Holocene orbital configuration and another with CO 2 levels of the Last Glacial Maximum to a preindustrial control simulation to test how the ARDTs respond to changes in seasonality and mean climate state, respectively. We find good agreement among the algorithms in the AR response to the changing orbital configuration,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8js796qm</guid>
      <pubDate>Fri, 25 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Rush, WD</name>
      </author>
      <author>
        <name>Lora, JM</name>
      </author>
      <author>
        <name>Skinner, CB</name>
      </author>
      <author>
        <name>Menemenlis, SA</name>
      </author>
      <author>
        <name>Shields, CA</name>
      </author>
      <author>
        <name>Ullrich, P</name>
        <uri>https://orcid.org/0000-0003-4118-4590</uri>
      </author>
      <author>
        <name>O’Brien, TA</name>
      </author>
      <author>
        <name>Brands, S</name>
      </author>
      <author>
        <name>Guan, B</name>
      </author>
      <author>
        <name>Mattingly, KS</name>
      </author>
      <author>
        <name>McClenny, E</name>
      </author>
      <author>
        <name>Nardi, K</name>
      </author>
      <author>
        <name>Nellikkattil, A</name>
      </author>
      <author>
        <name>Ramos, AM</name>
      </author>
      <author>
        <name>Reid, KJ</name>
      </author>
      <author>
        <name>Shearer, E</name>
      </author>
      <author>
        <name>Tomé, R</name>
      </author>
      <author>
        <name>Wille, JD</name>
      </author>
      <author>
        <name>Leung, LR</name>
      </author>
      <author>
        <name>Ralph, FM</name>
      </author>
      <author>
        <name>Rutz, JJ</name>
      </author>
      <author>
        <name>Wehner, M</name>
        <uri>https://orcid.org/0000-0001-8423-7870</uri>
      </author>
      <author>
        <name>Zhang, Z</name>
      </author>
      <author>
        <name>Lu, M</name>
      </author>
      <author>
        <name>Quagraine, KT</name>
      </author>
    </item>
    <item>
      <title>Thermal Adaptation of Enzyme‐Mediated Processes Reduces Simulated Soil CO2 Fluxes Upon Soil Warming</title>
      <link>https://escholarship.org/uc/item/7h95b28x</link>
      <description>Abstract  Understanding factors influencing carbon effluxes from soils to the atmosphere is important in a world experiencing climatic change. Two important uncertainties related to soil organic carbon (SOC) stock responses to a changing climate are (a) whether soil microbial communities acclimate or adapt to changes in soil temperature and (b) how to represent this process in SOC models. To further explore these issues, we included thermal adaptation of enzyme‐mediated processes in a mechanistic SOC model (ReSOM) using the macromolecular rate theory. Thermal adaptation is defined here to encompass all potential responses of soil microbes and microbial communities following a change in temperature. To assess the effects of thermal adaptation of enzyme‐mediated processes on simulated SOC losses, ReSOM was applied to data collected from&amp;nbsp;a 13‐year soil warming experiment. Results show that a model omitting thermal adaptation of enzyme‐mediated processes substantially overestimates...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7h95b28x</guid>
      <pubDate>Fri, 25 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Van de Broek, Marijn</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Tang, Jinyun</name>
        <uri>https://orcid.org/0000-0002-4792-1259</uri>
      </author>
      <author>
        <name>Frey, Serita D</name>
      </author>
      <author>
        <name>Schmidt, Michael WI</name>
      </author>
    </item>
    <item>
      <title>Tree root nutrient uptake kinetics vary with nutrient availability, environmental conditions, and root traits: a global analysis</title>
      <link>https://escholarship.org/uc/item/09x19352</link>
      <description>Root nutrient uptake by trees is a critical process that couples carbon and nutrient cycling in forest ecosystems. Yet, root nutrient uptake traits are poorly constrained, and the dynamics of this process are often not represented in models reflecting sparse measurements and understanding of root nutrient uptake physiology that lags those of aboveground physiology in forest ecosystems. Here, we present a global dataset of published nutrient uptake capacity and affinity values for tree species, with the goal of describing global patterns and evaluating responses to environmental drivers and associations with root traits. The dataset contains observations for ammonium, nitrate, and phosphate uptake spanning 77 tree species. Nutrient uptake capacity and affinity varied by more than an order of magnitude for each nutrient. Notably, tropical forests are underrepresented in these observations. Nutrient uptake capacity was generally diminished under nutrient enrichment but enhanced with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/09x19352</guid>
      <pubDate>Fri, 25 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Craig, Matthew E</name>
      </author>
      <author>
        <name>Walker, Anthony P</name>
      </author>
      <author>
        <name>Iversen, Colleen M</name>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Yaffar, Daniela</name>
      </author>
      <author>
        <name>York, Larry M</name>
      </author>
    </item>
    <item>
      <title>ELM‐Wet: Inclusion of a Wet‐Landunit With Sub‐Grid Representation of Eco‐Hydrological Patches and Hydrological Forcing Improves Methane Emission Estimations in the E3SM Land Model (ELM)</title>
      <link>https://escholarship.org/uc/item/045369xr</link>
      <description>Abstract  Wetlands are the largest emitters of biogenic methane (CH 4 ) and represent the highest source of uncertainty in global CH 4 budgets. Here, we aim to improve the realism of wetland representation in the U.S. Department of Energy's Exascale Earth System Model land surface model, ELM, thereby reducing uncertainty of CH 4 flux predictions. We develop an updated version, ELM‐Wet, where we activate a separate landunit for wetlands that handles multiple wetland‐specific eco‐hydrological patch functional types. We introduce more realistic hydrological forcing through prescribing site‐level constraints on surface water elevation, which allows resolving different sustained inundation depth for different patches, and if data exists, prescribing inundation depth. We modified the calculation of aerenchyma transport diffusivity based on observed conductance per leaf area for different vegetation types. We use Bayesian Optimization to parameterize CO 2 and CH 4 fluxes in the developed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/045369xr</guid>
      <pubDate>Thu, 24 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Yazbeck, Theresia</name>
      </author>
      <author>
        <name>Bohrer, Gil</name>
      </author>
      <author>
        <name>Scyphers, Madeline E</name>
      </author>
      <author>
        <name>Missik, Justine EC</name>
      </author>
      <author>
        <name>Shchehlov, Oleksandr</name>
      </author>
      <author>
        <name>Ward, Eric J</name>
      </author>
      <author>
        <name>Merino, Sergio L</name>
      </author>
      <author>
        <name>Bordelon, Robert</name>
      </author>
      <author>
        <name>Taj, Diana</name>
      </author>
      <author>
        <name>Villa, Jorge A</name>
      </author>
      <author>
        <name>Wrighton, Kelly</name>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
    </item>
    <item>
      <title>Hyperspectral leaf reflectance of grasses varies with evolutionary lineage more than with site</title>
      <link>https://escholarship.org/uc/item/9wj5j03r</link>
      <description>Abstract  To predict ecological responses at broad environmental scales, grass species are commonly grouped into two broad functional types based on photosynthetic pathway. However, closely related species may have distinctive anatomical and physiological attributes that influence ecological responses, beyond those related to photosynthetic pathway alone. Hyperspectral leaf reflectance can provide an integrated measure of covarying leaf traits that may result from phylogenetic trait conservatism and/or environmental conditions. Understanding whether spectra‐trait relationships are lineage specific or reflect environmental variation across sites is necessary for using hyperspectral reflectance to predict plant responses to environmental changes across spatial scales. We measured hyperspectral leaf reflectance (400–2400 nm) and 12 structural, biochemical, and physiological leaf traits from five grass‐dominated sites spanning the Great Plains of North America. We assessed if variation...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9wj5j03r</guid>
      <pubDate>Tue, 22 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Slapikas, Ryan</name>
      </author>
      <author>
        <name>Ho, Che‐Ling</name>
      </author>
      <author>
        <name>Bayliss, Shannon LJ</name>
        <uri>https://orcid.org/0000-0002-3997-8343</uri>
      </author>
      <author>
        <name>Donnelly, Ryan C</name>
      </author>
      <author>
        <name>Abdullahi, Adam</name>
      </author>
      <author>
        <name>Helliker, Brent R</name>
      </author>
      <author>
        <name>Nippert, Jesse B</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Still, Christopher J</name>
      </author>
      <author>
        <name>Wedel, Emily R</name>
      </author>
      <author>
        <name>Griffith, Daniel M</name>
      </author>
    </item>
    <item>
      <title>E3SM‐GCAM: A Synchronously Coupled Human Component in the E3SM Earth System Model Enables Novel Human‐Earth Feedback Research</title>
      <link>https://escholarship.org/uc/item/8j9988sf</link>
      <description>Abstract  Modeling human‐environment feedbacks is critical for assessing the effectiveness of climate change mitigation and adaptation strategies under a changing climate. The Energy Exascale Earth System Model (E3SM) now includes a human component, with the Global Change Analysis Model (GCAM) at its core, that is synchronously coupled with the land and atmosphere components through the E3SM coupling software. Terrestrial productivity is passed from E3SM to GCAM to make climate‐responsive land use and CO 2 emission projections for the next 5‐year period, which are interpolated and passed to E3SM annually. Key variables affected by the incorporation of these feedbacks include land use/cover change, crop prices, terrestrial carbon, local surface temperature, and climate extremes. Regional differences are more pronounced than global differences because the effects are driven primarily by differences in land use. This novel system enables a new type of scenario development and provides...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8j9988sf</guid>
      <pubDate>Tue, 22 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Di Vittorio, Alan V</name>
        <uri>https://orcid.org/0000-0002-8139-4640</uri>
      </author>
      <author>
        <name>Sinha, Eva</name>
      </author>
      <author>
        <name>Hao, Dalei</name>
      </author>
      <author>
        <name>Singh, Balwinder</name>
      </author>
      <author>
        <name>Calvin, Katherine V</name>
      </author>
      <author>
        <name>Shippert, Tim</name>
      </author>
      <author>
        <name>Patel, Pralit</name>
      </author>
      <author>
        <name>Bond‐Lamberty, Ben</name>
      </author>
    </item>
    <item>
      <title>Assessing Simulations of Forest Hurricane Disturbance and Recovery in Puerto Rico by ELM‐FATES Using Field Measurements</title>
      <link>https://escholarship.org/uc/item/5698z3nq</link>
      <description>Abstract In the past three decades, Puerto Rico (PR) experienced five hurricanes that met or exceeded category three, and they caused severe forest structural damage and elevated tree mortality. To improve our mechanistic understanding of hurricane impacts on tropical forests and assess hurricane‐affected forest dynamics in Earth system models, we use in situ forest measurements at the Bisley Experimental Watersheds in Northeast PR to evaluate the Functionally Assembled Terrestrial Ecosystem Simulator coupled with the Energy Exascale Earth System Model Land Model (ELM‐FATES). The observations show that before Hurricane Hugo, 77.3% of the aboveground biomass (AGB) is from the shade‐tolerant plant function type (PFT). The Hugo‐induced mortality rates are over ∼50%, and they induce a ∼39% AGB reduction, which recovers to a level like the pre‐Hugo condition in 2014, following a second, lower intensity hurricane, Georges. We perform numerical experiments that simulate damage from Hugo...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5698z3nq</guid>
      <pubDate>Tue, 22 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Shi, Mingjie</name>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Bomfim, Barbara</name>
      </author>
      <author>
        <name>Kueppers, Lara</name>
        <uri>https://orcid.org/0000-0002-8134-3579</uri>
      </author>
      <author>
        <name>Koven, Charlie</name>
      </author>
      <author>
        <name>Needham, Jessica</name>
        <uri>https://orcid.org/0000-0003-3653-3848</uri>
      </author>
      <author>
        <name>Heartsill‐Scalley, Tamara</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
    </item>
    <item>
      <title>Thermal acclimation of stem respiration implies a weaker carbon-climate feedback</title>
      <link>https://escholarship.org/uc/item/3x12434m</link>
      <description>The efflux of carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) from woody stems, a proxy for stem respiration, is a critical carbon flux from ecosystems to the atmosphere, which increases with temperature on short timescales. However, plants acclimate their respiratory response to temperature on longer timescales, potentially weakening the carbon-climate feedback. The magnitude of this acclimation is uncertain despite its importance for predicting future climate change. We develop an optimality-based theory dynamically linking stem respiration with leaf water supply to predict its thermal acclimation. We show that the theory accurately reproduces observations of spatial and seasonal change. We estimate the global value for current annual stem CO&lt;sub&gt;2&lt;/sub&gt; efflux as 27.4 ± 5.9 PgC. By 2100, incorporating thermal acclimation reduces projected stem respiration without considering acclimation by 24 to 46%, thus reducing land ecosystem carbon emissions.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3x12434m</guid>
      <pubDate>Tue, 22 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zhang, Han</name>
      </author>
      <author>
        <name>Wang, Han</name>
      </author>
      <author>
        <name>Wright, Ian J</name>
      </author>
      <author>
        <name>Prentice, I Colin</name>
      </author>
      <author>
        <name>Harrison, Sandy P</name>
      </author>
      <author>
        <name>Smith, Nicholas G</name>
      </author>
      <author>
        <name>Westerband, Andrea C</name>
      </author>
      <author>
        <name>Rowland, Lucy</name>
      </author>
      <author>
        <name>Plavcová, Lenka</name>
      </author>
      <author>
        <name>Morris, Hugh</name>
      </author>
      <author>
        <name>Reich, Peter B</name>
      </author>
      <author>
        <name>Jansen, Steven</name>
      </author>
      <author>
        <name>Keenan, Trevor</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
      <author>
        <name>Nguyen, Ngoc Bao</name>
      </author>
    </item>
    <item>
      <title>SARS-CoV-2 virus in raw wastewater from student residence halls with concomitant 16S rRNA bacterial community structure changes</title>
      <link>https://escholarship.org/uc/item/8cz054kq</link>
      <description>The detection of severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2) RNA in sewage is well-established, but the concomitant changes in microbial compositions during the pandemic remain insufficiently explored. This study investigates the impact of the SARS-CoV-2 virus on microbial compositions in raw sewage, utilizing high-throughput 16S rRNA amplicon sequencing to analyze wastewater samples collected from six dormitories over a one-year field trial at the University of Tennessee, Knoxville. The concentration of SARS-CoV-2 RNA was assessed using a reverse transcription-quantitative polymerase chain reaction. Significant variations in bacterial composition were evident across the six dormitories, highlighting the importance of independently considering spatial differences when evaluating the raw wastewater microbiome. Positive samples for SARS-CoV-2 exhibited a prominent representation of exclusive species across all dormitories, coupled with significantly reduced bacterial...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8cz054kq</guid>
      <pubDate>Wed, 16 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Li, Ye</name>
      </author>
      <author>
        <name>Ash, Kurt T</name>
      </author>
      <author>
        <name>Joyner, Dominique</name>
      </author>
      <author>
        <name>Williams, Daniel E</name>
      </author>
      <author>
        <name>Hazen, Terry C</name>
        <uri>https://orcid.org/0000-0002-2536-9993</uri>
      </author>
    </item>
    <item>
      <title>Upper bounds for 21st-century surface air temperatures in the Western United States</title>
      <link>https://escholarship.org/uc/item/8rk322qm</link>
      <description>The last decade has seen a large number of severe heatwaves that were unprecedented in the observational record, highlighting challenges associated with observationally-based statistical quantification of the likelihood and magnitude of future extreme temperatures. An alternative to such probabilistic assessments is identification of upper bounds that quantify the hottest surface air temperatures that can possibly be achieved by the end of the 21st century. Theory, simulations, and observational analyses support the existence of a finite upper bound for surface air temperature; however, estimates for future upper-bound values that are realistic and usable for planning remain unavailable. Here, we combine atmospheric theory with large ensembles of dynamically downscaled projections to estimate historical and end-of-century upper bounds for surface air temperatures. A number of physical mechanisms can influence upper bounds, and at the end of the 21st century, estimates based on...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8rk322qm</guid>
      <pubDate>Tue, 15 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Risser, Mark D</name>
        <uri>https://orcid.org/0000-0003-1956-1783</uri>
      </author>
      <author>
        <name>Feldman, Daniel R</name>
      </author>
      <author>
        <name>Boos, William R</name>
        <uri>https://orcid.org/0000-0001-9076-3551</uri>
      </author>
      <author>
        <name>Rahimi, Stefan</name>
      </author>
    </item>
    <item>
      <title>Understanding drivers and uncertainty in projected African precipitation</title>
      <link>https://escholarship.org/uc/item/16m7p89w</link>
      <description>We investigate the drivers of projected summer precipitation changes and their uncertainties across Africa in the second half of the 21st century under the SSP2-4.5 and SSP5-8.5 scenarios using CMIP6 models. Our results reveal distinct regional precipitation changes, particularly under SSP5-8.5, with robust increases of 75%, 24%, and 17% over the Sahara, South Eastern Africa, and South Central Africa, respectively, and a decline of up to 5% over West Southern Africa (WSAF). In most regions, precipitation increases are driven by enhanced vertical thermodynamic processes associated with temperature-induced moisture increases and enhanced moisture convergence. In contrast, the WSAF decrease is associated with vertical dynamic processes driven by a weakening of the Hadley circulation’s ascending branch. Model uncertainty accounts for over 85% of total projection uncertainty across all regions and is largely due to subgrid-scale parameterizations. Overall, this study enhances our understanding...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/16m7p89w</guid>
      <pubDate>Tue, 15 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Taguela, Thierry N</name>
      </author>
      <author>
        <name>Akinsanola, Akintomide A</name>
      </author>
      <author>
        <name>Adeliyi, Tolulope E</name>
      </author>
      <author>
        <name>Rhoades, Alan</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Nazarian, Robert H</name>
      </author>
    </item>
  </channel>
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