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    <title>Recent uciess items</title>
    <link>https://escholarship.org/uc/uciess/rss</link>
    <description>Recent eScholarship items from Department of Earth System Science</description>
    <pubDate>Fri, 15 May 2026 08:03:35 +0000</pubDate>
    <item>
      <title>Persistence and turnover of soil organic carbon in global drylands.</title>
      <link>https://escholarship.org/uc/item/8w86x2fz</link>
      <description>Reliable predictions of dryland carbon fluxes require understanding the persistence and turnover of soil organic carbon (SOC). We measure radiocarbon to quantify the age of SOC and CO&lt;sub&gt;2&lt;/sub&gt; released from soil respiration at 97 dryland sites across six continents. Here we show that bulk SOC contains little C fixed in the past 60 years, while respired CO&lt;sub&gt;2&lt;/sub&gt; originates from both bomb-derived recent C and millennia-old C, challenging the idea that old C is chemically or physically protected. Radiocarbon suggests mean ages of ~2100 years for bulk SOC and ~520 years for respired CO&lt;sub&gt;2&lt;/sub&gt;, the latter far older than machine-learning (&amp;lt;50 years) or Earth system models predict. Aridity, net primary productivity, and SOC content are dominant predictors for radiocarbon signatures, with abrupt shifts to older C beyond an aridity threshold of ~0.87. Our findings underscore the need to incorporate the vulnerability of older carbon into models and land management strategies.</description>
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      <pubDate>Mon, 27 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Wang, Hui</name>
      </author>
      <author>
        <name>Maestre, Fernando</name>
      </author>
      <author>
        <name>Lu, Nan</name>
      </author>
      <author>
        <name>Zhao, Guang</name>
      </author>
      <author>
        <name>Zhang, Yangjian</name>
      </author>
      <author>
        <name>Asensio, Sergio</name>
      </author>
      <author>
        <name>Bramble, De</name>
      </author>
      <author>
        <name>Chen, Weiliang</name>
      </author>
      <author>
        <name>Dippold, Michaela</name>
      </author>
      <author>
        <name>Eldridge, David</name>
      </author>
      <author>
        <name>Gaitán, Juan</name>
      </author>
      <author>
        <name>García-Gómez, Miguel</name>
      </author>
      <author>
        <name>Gozalo, Beatriz</name>
      </author>
      <author>
        <name>Gross, Nicolas</name>
      </author>
      <author>
        <name>Guirado, Emilio</name>
      </author>
      <author>
        <name>Le Bagousse-Pinguet, Yoann</name>
      </author>
      <author>
        <name>Martínez-Valderrama, Jaime</name>
      </author>
      <author>
        <name>Mendoza, Betty</name>
      </author>
      <author>
        <name>Ochoa, Victoria</name>
      </author>
      <author>
        <name>Plaza, César</name>
      </author>
      <author>
        <name>Saiz, Hugo</name>
      </author>
      <author>
        <name>Schrumpf, Marion</name>
      </author>
      <author>
        <name>Sierra, Carlos</name>
      </author>
      <author>
        <name>Tangarife-Escobar, Andrés</name>
      </author>
      <author>
        <name>Valencia, Enrique</name>
      </author>
      <author>
        <name>von Fromm, Sophie</name>
      </author>
      <author>
        <name>Wang, Cong</name>
      </author>
      <author>
        <name>Wang, Kai</name>
      </author>
      <author>
        <name>Wang, Yunqiang</name>
      </author>
      <author>
        <name>Zaehle, Sönke</name>
      </author>
      <author>
        <name>Fu, Bojie</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
      </author>
      <author>
        <name>Huang, Jianbei</name>
      </author>
    </item>
    <item>
      <title>Widespread windthrow in Southeast Asian tropical forests verified by satellite observations</title>
      <link>https://escholarship.org/uc/item/9jg3r7td</link>
      <description>Windthrow, defined as abrupt tree mortality caused by intense winds, is well documented in the Neotropics but remains largely unverified in Asian tropical forests. Using Landsat 8 imagery for the period 2020-2022 and established spectral (shortwave-infrared, near-infrared, and red band composites) and morphological criteria (fan-shaped geometry and sharp boundaries), this study verified the presence of windthrow across Sumatra, Borneo, and New Guinea and produced the first georeferenced inventory of 60 events in the region. Event sizes were right-skewed, with many small gaps and few large (&amp;gt;200 ha) disturbances. Orientations were anisotropic, with concentrations of windthrow events pointing west to northwest-to-north and eastward, both aligning with known pathways of organized convection in the Maritime Continent of Southeast Asia. Detection was conservatively biased low by cloud cover, long revisit intervals, and the exclusion of land-use areas. This study provides a verified...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9jg3r7td</guid>
      <pubDate>Tue, 31 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
    </item>
    <item>
      <title>Mortality correlates with tree functional traits across a wood density gradient in the Central Amazon</title>
      <link>https://escholarship.org/uc/item/24s457ht</link>
      <description>Introduction: Understanding the mechanisms of tree mortality in tropical ecosystems remains challenging, in part due to the high diversity of tree species and the inherently stochastic nature of mortality. Plant functional traits offer a mechanistic link between plant physiology and performance, yet their ability to predict growth and mortality remains poorly understood. Given recent increases in tree mortality rates in the Amazon forest following extreme drought and wind events, we tested if lower wood density and acquisitive plant functional traits were associated with increased growth and mortality for common co-occurring trees in the Central Amazon.
Methods: Seventeen trees of different species with similar sizes but a range in wood density (WD) and wood traits were felled, then assessed for 27 different individual functional parameters, including whole tree architecture, stem xylem anatomical and hydraulic traits and leaf traits. Traits of the individual trees were related...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/24s457ht</guid>
      <pubDate>Wed, 18 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>da Silva Menezes, Valdiek</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Wright, Cynthia L</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Nascimento, Claudete C</name>
      </author>
      <author>
        <name>Barros, Fernanda B</name>
      </author>
      <author>
        <name>Spanner, Gustavo C</name>
      </author>
      <author>
        <name>Rodrigues, Jardel R</name>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Collins, Adam D</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Newman, Brent D</name>
      </author>
      <author>
        <name>Lima, Adriano José Nogueira</name>
      </author>
      <author>
        <name>Warren, Jeffrey M</name>
      </author>
    </item>
    <item>
      <title>Representing lateral groundwater flow from land to river in Earth system models</title>
      <link>https://escholarship.org/uc/item/1h65734x</link>
      <description>Abstract. Lateral groundwater flow (LGF) is an important hydrologic process in controlling water table dynamics. Due to the relatively coarse spatial resolutions of land surface models, the representation of this process is often overlooked or overly simplified. In this study, we developed a hillslope-based lateral groundwater flow model. Specifically, we first developed a hillslope definition model based on an existing watershed delineation model to represent the subgrid spatial variability in topography. Building upon this hillslope definition, we then developed a physical-based lateral groundwater flow using Darcy’s equation. This model explicitly considers the relationships between the groundwater table along the hillslope and the river water table levels. We coupled this intra-grid model to the land component (E3SM Land Model: ELM) and river component (MOdel for Scale Adaptive River Transport: MOSART) of the Energy Exascale Earth System Model (E3SM). We tested both the hillslope...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1h65734x</guid>
      <pubDate>Mon, 16 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Liao, Chang</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
      <author>
        <name>Fang, Yilin</name>
      </author>
      <author>
        <name>Tesfa, Teklu</name>
      </author>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
    </item>
    <item>
      <title>Widespread forest disturbance from windthrow in central African rainforests</title>
      <link>https://escholarship.org/uc/item/284593vw</link>
      <description>Natural disturbances are major drivers of tropical forest dynamics, yet their role in Central Africa’s old-growth rainforests, the world’s second largest tropical forest block, remains poorly quantified. Here we present the first regional assessment of windthrow, the uprooting or breakage of trees by wind. Using Landsat imagery from 2019 to 2020, we detected 74 windthrow events ≥30 ha, collectively affecting ~18,600 ha. These events were concentrated in eastern regions where mesoscale convective systems and extreme rainfall are most frequent. Sizes of windthrow events followed a Weibull distribution, with a single 3974 ha event accounting for one fifth of the total affected area. Event orientations aligned with prevailing storm outflows, and their timing coincided with peaks in extreme rainfall. For a subset of seven events with adequate temporal coverage before and after disturbance, near-infrared reflectance returned to pre-disturbance levels within months, indicating a rapid...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/284593vw</guid>
      <pubDate>Thu, 12 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Sheil, Douglas</name>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Ordway, Elsa M</name>
        <uri>https://orcid.org/0000-0002-7720-1754</uri>
      </author>
      <author>
        <name>Magnabosco Marra, Daniel</name>
      </author>
      <author>
        <name>Urquiza-Muñoz, Jose D</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>The Role of Canopy Turbulence in Wildland Fire Behavior</title>
      <link>https://escholarship.org/uc/item/6v68j5mb</link>
      <description>Characterizing the physical and dynamic meteorology of wildland fires has obvious socioeconomic importance and is necessary to develop not only firefighting but also mitigation strategies such as prescribed burns and effective fuel management practices such as forest thinning. However, despite significant progress over a century, there are shortcomings in our understanding of the physical processes governing wildland fire behavior. Although some research progress has been made in understanding how fires spread on grasslands, several aspects of fire behavior within the forest canopy environment are still not well-understood. This review is an attempt to organize the fluid mechanics of the mass, momentum, and energy transfer during wildland fire events through the lens of vegetation canopy turbulence. The structure, organization, and progress of the flame front and the buoyant plume through the canopy are shown to be intricately related to the coherent structures associated with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6v68j5mb</guid>
      <pubDate>Wed, 4 Mar 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Banerjee, Tirtha</name>
        <uri>https://orcid.org/0000-0002-5153-9474</uri>
      </author>
    </item>
    <item>
      <title>Transboundary water conflicts, cooperation, and pathways forward</title>
      <link>https://escholarship.org/uc/item/5w15k2g7</link>
      <description>Transboundary water conflicts, cooperation, and pathways forward</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5w15k2g7</guid>
      <pubDate>Wed, 25 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>AghaKouchak, Amir</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
      <author>
        <name>Hjelmstad, Annika</name>
      </author>
      <author>
        <name>Khodkar, Kasra</name>
      </author>
      <author>
        <name>de Oliveira, Debora</name>
      </author>
      <author>
        <name>Aleisa, Esra</name>
      </author>
      <author>
        <name>Alexander, Augustina C</name>
      </author>
      <author>
        <name>Feldman, David Lewis</name>
        <uri>https://orcid.org/0000-0003-2288-5017</uri>
      </author>
      <author>
        <name>Khujanazarov, Temur</name>
      </author>
      <author>
        <name>Madani, Kaveh</name>
      </author>
      <author>
        <name>Mirchi, Ali</name>
      </author>
      <author>
        <name>Placht, Daniel</name>
      </author>
      <author>
        <name>Najib, Dalal</name>
      </author>
    </item>
    <item>
      <title>Evolving approaches and data availability for understanding the impact of land-use change on ecosystem services</title>
      <link>https://escholarship.org/uc/item/4bt2p44r</link>
      <description>Understanding how land-use change alters the flow of ecosystem services is critical for sustainability policy and planning. We conducted a systematic review of 459 peer-reviewed articles published between 2001 and March 2024 to (a) catalogue which ecosystem services have been studied and their geographic distribution, (b) trace methodological innovations in mapping, and (c) assess the integration of emerging data streams. Our analysis identified 23 ecosystem services spanning provisioning (food, water, raw materials), regulating (climate regulation, erosion control, flood protection), and cultural (recreation, aesthetics), with provisioning services most often mapped individually but regulating services dominating in category-level assessments. Regionally, Asia (especially China) contributed over half (51&amp;nbsp;%) of the case studies, while case studies in Europe, Africa, and the Americas are also increasing, aided by international collaborations in nearly 30&amp;nbsp;% of the studies....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4bt2p44r</guid>
      <pubDate>Wed, 25 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Epie, Wesner Njume</name>
      </author>
      <author>
        <name>Stouter, Hannah</name>
      </author>
      <author>
        <name>Lenhardt, Julia</name>
      </author>
      <author>
        <name>Ayompe, Lacour M</name>
      </author>
      <author>
        <name>Ordway, Elsa M</name>
        <uri>https://orcid.org/0000-0002-7720-1754</uri>
      </author>
      <author>
        <name>Crook, Elizabeth D</name>
        <uri>https://orcid.org/0000-0001-5798-2736</uri>
      </author>
      <author>
        <name>Egoh, Benis N</name>
      </author>
    </item>
    <item>
      <title>Transcriptomic, physiological, and biochemical responses of turmeric (Curcuma longa) to heat stress</title>
      <link>https://escholarship.org/uc/item/881511pt</link>
      <description>Turmeric (Curcuma longa) is an economically important crop native to hot and humid regions of India. The current study aims to establish the basis for a multifaceted understanding of turmeric plants’ cellular and physiological responses to heat stress. We combined transcriptomic (RNA-seq) analysis, real-time photosynthesis data, and profiles of emissions of biogenic volatile organic compounds (BVOCs) to interpret the responses of turmeric plants to heat stress. RNAseq data indicated significant differential expression in 41.8% of genes, with photosynthesis-related genes overrepresented. Photosynthetic rate measurements demonstrated an almost complete failure of photosynthesis at 41 °C, followed by incomplete recovery at a normal temperature of 21 °C. Emissions of almost all detected BVOCs increased considerably during periods of heat treatment. The data establishes the ontological gene groups most affected, estimates the temperature tolerance of turmeric, and provides insights...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/881511pt</guid>
      <pubDate>Wed, 11 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Musaev, Kirill</name>
      </author>
      <author>
        <name>Nagalingam, Sanjeevi</name>
      </author>
      <author>
        <name>Duong, Lam</name>
      </author>
      <author>
        <name>Guenther, Alex</name>
      </author>
      <author>
        <name>Mentreddy, Srinivasa Rao</name>
      </author>
      <author>
        <name>Basu, Chhandak</name>
      </author>
    </item>
    <item>
      <title>Gene duplication, horizontal gene transfer, and trait trade-offs drive evolution of postfire resource acquisition in pyrophilous fungi.</title>
      <link>https://escholarship.org/uc/item/3483t48n</link>
      <description>Wildfires significantly alter soil carbon (C) and nitrogen (N), reducing microbial richness and biomass, while selecting for "fire-loving" pyrophilous microbes that drive postfire nutrient cycling. However, the genomic strategies and functional trade-offs (balancing gains in one trait with costs in another) underlying the traits that enable pyrophilous microbes to survive and thrive postfire are virtually unknown. We hypothesized that pyrophilous fungi employ specialized genomic adaptations for C and N cycling, with evolutionary trade-offs between traits governing aromatic C degradation, N acquisition pathways, and rapid growth. To test these hypotheses, we performed complementary comparative genomics, transcriptomics after pyrogenic organic matter amendment, and growth rate bioassays for 18 pyrophilous fungi from five Ascomycota (Eurotiales, Pleosporales, Sordariales, Coniochaetales, and Pezizales) and three Basidiomycota (Agaricales, Holtermanniales, and Geminibasidiales) orders...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3483t48n</guid>
      <pubDate>Thu, 15 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Sari, Ehsan</name>
      </author>
      <author>
        <name>Enright, Dylan J</name>
      </author>
      <author>
        <name>Ordoñez, Maria E</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Homyak, Peter M</name>
        <uri>https://orcid.org/0000-0003-0671-8358</uri>
      </author>
      <author>
        <name>Wilkins, Michael J</name>
      </author>
      <author>
        <name>Glassman, Sydney I</name>
        <uri>https://orcid.org/0000-0001-9115-3026</uri>
      </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>Multi-ignition fire complexes drive extreme fire years and impacts</title>
      <link>https://escholarship.org/uc/item/8f06k30s</link>
      <description>Climate change is intensifying fire behavior, with the largest and fastest-spreading fires causing the greatest impacts on people and ecosystems. Yet the mechanisms driving variability and trends in large fires remain poorly understood. Using 12-hour satellite-derived fire tracking data from 2012 to 2023, we show that the merging of separate ignitions into multi-ignition complexes is a key process amplifying fire size and destructive potential across temperate and boreal ecoregions. Multi-ignition fires account for 31% of the burned area in California and 59% in the Arctic-boreal domain, spread faster and persist longer than single-ignition fires, and disproportionately contribute to extreme fire years in California, Canada, and Siberia. They also generate stronger atmospheric feedbacks, produce more pyrocumulonimbus events, and strain firefighting capacity by dispersing suppression resources. Recognizing and accounting for fire-merging dynamics are critical for improving wildfire...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8f06k30s</guid>
      <pubDate>Tue, 6 Jan 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Scholten, Rebecca C</name>
        <uri>https://orcid.org/0000-0002-0144-0572</uri>
      </author>
      <author>
        <name>Banerjee, Tirtha</name>
      </author>
      <author>
        <name>Chen, Yang</name>
        <uri>https://orcid.org/0000-0002-0993-7081</uri>
      </author>
      <author>
        <name>Delgado, Andrea</name>
      </author>
      <author>
        <name>Desai, Ajinkya</name>
      </author>
      <author>
        <name>Ke, Ziming</name>
      </author>
      <author>
        <name>Liu, Tianjia</name>
        <uri>https://orcid.org/0000-0003-3129-0154</uri>
      </author>
      <author>
        <name>Morton, Douglas C</name>
      </author>
      <author>
        <name>Peterson, David A</name>
      </author>
      <author>
        <name>Tang, Qi</name>
      </author>
      <author>
        <name>Veraverbeke, Sander</name>
      </author>
      <author>
        <name>Zhang, Jishi</name>
      </author>
      <author>
        <name>Randerson, James T</name>
        <uri>https://orcid.org/0000-0001-6559-7387</uri>
      </author>
    </item>
    <item>
      <title>Large role of anthropogenic climate change in driving smoke concentrations across the western United States from 1992 to 2020</title>
      <link>https://escholarship.org/uc/item/3gh322wr</link>
      <description>Wildfire activity has increased dramatically in the western United States over the last three decades, having a significant impact on air quality and human health. However, quantifying the drivers of trends in wildfires and subsequent smoke concentrations is challenging, as both natural variability (NV) and anthropogenic climate change (ACC) play important roles. Here, we devise an approach involving observed meteorology and vegetation and a range of models to determine the relative roles of ACC and NV in driving burned area across the western United States. We also examine the influence of ACC on smoke concentrations. We estimate that ACC accounts for 33 to 82% of observed total burned area, depending on the ecoregion, yielding 65% of total fire emissions on average across the western United States from 1992 to 2020. In all ecoregions except Mediterranean California, ACC contributes to a greater percentage of burned area in lightning-ignited wildfires than in human-ignited wildfires....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3gh322wr</guid>
      <pubDate>Sat, 20 Dec 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Xu</name>
      </author>
      <author>
        <name>Mickley, Loretta J</name>
      </author>
      <author>
        <name>Kaplan, Jed O</name>
      </author>
      <author>
        <name>Kelp, Makoto</name>
      </author>
      <author>
        <name>Li, Yang</name>
      </author>
      <author>
        <name>Liu, Tianjia</name>
        <uri>https://orcid.org/0000-0003-3129-0154</uri>
      </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>Implementation of solar UV and energetic particle precipitation within the LINOZ scheme in ICON-ART</title>
      <link>https://escholarship.org/uc/item/1b94z0jt</link>
      <description>Abstract. We extended the Linearized ozone scheme – LINOZ in the ICON (ICOsahedral Nonhydrostatic) – ART (the extension for Aerosols and Reactive Trace gases) model system to include NOy formed by auroral and medium-energy electrons in the upper mesosphere and lower thermosphere, and the corresponding ozone loss, as well as changes in the rate of ozone formation due to the variability of the solar radiation in the ultraviolet wavelength range. This extension allows us to realistically represent variable solar and geomagnetic forcing in the middle atmosphere using a very simple ozone scheme. The LINOZ scheme is computationally very cheap compared to a full middle atmosphere chemistry scheme, yet provides realistic ozone fields consistent with the stratospheric circulation and temperatures, and can thus be used in climate models instead of prescribed ozone climatologies. To include the reactive nitrogen&amp;nbsp;(NOy) produced by auroral and radiation belt electron precipitation in...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1b94z0jt</guid>
      <pubDate>Wed, 19 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Ziarani, Maryam Ramezani</name>
      </author>
      <author>
        <name>Sinnhuber, Miriam</name>
      </author>
      <author>
        <name>Reddmann, Thomas</name>
      </author>
      <author>
        <name>Funke, Bernd</name>
      </author>
      <author>
        <name>Bender, Stefan</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>Interactive Gas Chemistry for Enhanced Science Capabilities of the Energy Exascale Earth System Model Version 3</title>
      <link>https://escholarship.org/uc/item/9876s69q</link>
      <description>Abstract Atmospheric chemistry plays a crucial role in Earth system models (ESMs), controlling atmospheric composition and radiative balance; it is highly interactive with the physical climate, biogeochemical cycles, and human systems. However, it often imposes computational challenges in an ESM. Here we develop a full troposphere‐stratosphere interactive chemistry module for the US Department of Energy's Energy Exascale Earth System Model (E3SM). We intentionally build a streamlined module based on E3SM version 2 that interacts with other components and maintains all of major chemical and chemistry‐climate feedbacks. The module incorporates a new, highly efficient tracer advection scheme; linearization of stratospheric chemistry; and abridged tropospheric chemical mechanism with 28 reactive tracers. This new model, E3SM‐chem, can readily perform century‐long climate simulations of ozone, methane, and nitrous oxide based on emission scenarios as well as provide hourly budgets...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9876s69q</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Tang, Qi</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Ke, Ziming</name>
      </author>
      <author>
        <name>Xie, Jinbo</name>
      </author>
      <author>
        <name>Lee, Hsiang‐He</name>
      </author>
      <author>
        <name>Wu, Mingxuan</name>
      </author>
      <author>
        <name>Cameron‐Smith, Philip</name>
      </author>
      <author>
        <name>Wang, Hailong</name>
      </author>
      <author>
        <name>Lin, Wuyin</name>
      </author>
      <author>
        <name>Xie, Shaocheng</name>
      </author>
    </item>
    <item>
      <title>Near-term Climate Change: Projections and Predictability</title>
      <link>https://escholarship.org/uc/item/7wk905fv</link>
      <description>Executive Summary This chapter assesses the scientific literature describing expectations for near-term climate (present through mid-century). Unless otherwise stated, ‘near-term’ change and the projected changes below are for the period 2016–2035 relative to the reference period 1986–2005. Atmospheric composition (apart from CO2; see Chapter 12) and air quality projections through to 2100 are also assessed. Decadal Prediction The nonlinear and chaotic nature of the climate system imposes natual limits on the extent to which skilful predictions of climate statistics may be made. Model-based ‘predictability’ studies, which probe these limits and investigate the physical mechanisms involved, support the potential for the skilful prediction of annual to decadal average temperature and, to a lesser extent precipitation. Predictions for averages of temperature, over large regions of the planet and for the global mean, exhibit positive skill when verified against observations for forecast...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7wk905fv</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Kirtman, Ben</name>
      </author>
      <author>
        <name>Power, Scott B</name>
      </author>
      <author>
        <name>Adedoyin, Akintayo John</name>
      </author>
      <author>
        <name>Boer, George J</name>
      </author>
      <author>
        <name>Bojariu, Roxana</name>
      </author>
      <author>
        <name>Camilloni, Ines</name>
      </author>
      <author>
        <name>Doblas-Reyes, Francisco</name>
      </author>
      <author>
        <name>Fiore, Arlene M</name>
      </author>
      <author>
        <name>Kimoto, Masahide</name>
      </author>
      <author>
        <name>Meehl, Gerald</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Sarr, Abdoulaye</name>
      </author>
      <author>
        <name>Schar, Christoph</name>
      </author>
      <author>
        <name>Sutton, Rowan</name>
      </author>
      <author>
        <name>van Oldenborgh, Geert Jan</name>
      </author>
      <author>
        <name>Vecchi, Gabriel</name>
      </author>
      <author>
        <name>Wang, Hui-Jun</name>
      </author>
      <author>
        <name>Bindoff, Nathaniel L</name>
      </author>
      <author>
        <name>Cameron-Smith, Philip</name>
      </author>
      <author>
        <name>Chikamoto, Yoshimitsu</name>
      </author>
      <author>
        <name>Clifton, Olivia</name>
      </author>
      <author>
        <name>Corti, Susanna</name>
      </author>
      <author>
        <name>Durack, Paul J</name>
      </author>
      <author>
        <name>Fichefet, Thierry</name>
      </author>
      <author>
        <name>Garcia-Serrano, Javier</name>
      </author>
      <author>
        <name>Ginoux, Paul</name>
      </author>
      <author>
        <name>Gray, Lesley</name>
      </author>
      <author>
        <name>Guemas, Virginie</name>
      </author>
      <author>
        <name>Hawkins, Ed</name>
      </author>
      <author>
        <name>Holland, Marika</name>
      </author>
      <author>
        <name>Holmes, Christopher</name>
      </author>
      <author>
        <name>Infanti, Johnna</name>
      </author>
      <author>
        <name>Ishii, Masayoshi</name>
      </author>
      <author>
        <name>Jacob, Daniel</name>
      </author>
      <author>
        <name>John, Jasmin</name>
      </author>
      <author>
        <name>Klimont, Zbigniew</name>
      </author>
      <author>
        <name>Knutson, Thomas</name>
      </author>
      <author>
        <name>Krinner, Gerhard</name>
      </author>
      <author>
        <name>Lawrence, David</name>
      </author>
      <author>
        <name>Lu, Jian</name>
      </author>
      <author>
        <name>Murphy, Daniel</name>
      </author>
      <author>
        <name>Naik, Vaishali</name>
      </author>
      <author>
        <name>Robock, Alan</name>
      </author>
      <author>
        <name>Rodrigues, Luis</name>
      </author>
      <author>
        <name>Sedlacek, Jan</name>
      </author>
      <author>
        <name>Slater, Andrew</name>
      </author>
      <author>
        <name>Smith, Doug</name>
      </author>
      <author>
        <name>Stevenson, David S</name>
      </author>
      <author>
        <name>van den Hurk, Bart</name>
      </author>
      <author>
        <name>van Noije, Twan</name>
      </author>
      <author>
        <name>Vavrus, Steve</name>
      </author>
      <author>
        <name>Voulgarakis, Apostolos</name>
      </author>
      <author>
        <name>Weisheimer, Antje</name>
      </author>
      <author>
        <name>Wild, Oliver</name>
      </author>
      <author>
        <name>Woollings, Tim</name>
      </author>
      <author>
        <name>Young, Paul</name>
      </author>
    </item>
    <item>
      <title>Global nitrous oxide budget (1980–2020)</title>
      <link>https://escholarship.org/uc/item/7nv7t738</link>
      <description>Abstract. Nitrous oxide&amp;nbsp;(N2O) is a long-lived potent greenhouse gas and stratospheric ozone-depleting substance that has been accumulating in the atmosphere since the preindustrial period. The mole fraction of atmospheric N2O has increased by nearly 25 % from 270 ppb (parts per billion) in&amp;nbsp;1750 to 336 ppb in&amp;nbsp;2022, with the fastest annual growth rate since&amp;nbsp;1980 of more than 1.3 ppb yr−1 in both&amp;nbsp;2020 and&amp;nbsp;2021. According to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change&amp;nbsp;(IPCC&amp;nbsp;AR6), the relative contribution of N2O to the total enhanced effective radiative forcing of greenhouse gases was 6.4 % for 1750–2022. As a core component of our global greenhouse gas assessments coordinated by the Global Carbon Project&amp;nbsp;(GCP), our global N2O budget incorporates both natural and anthropogenic sources and sinks and accounts for the interactions between nitrogen additions and the biogeochemical processes that control N2O...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7nv7t738</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Tian, Hanqin</name>
      </author>
      <author>
        <name>Pan, Naiqing</name>
      </author>
      <author>
        <name>Thompson, Rona L</name>
      </author>
      <author>
        <name>Canadell, Josep G</name>
      </author>
      <author>
        <name>Suntharalingam, Parvadha</name>
      </author>
      <author>
        <name>Regnier, Pierre</name>
      </author>
      <author>
        <name>Davidson, Eric A</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Ciais, Philippe</name>
      </author>
      <author>
        <name>Muntean, Marilena</name>
      </author>
      <author>
        <name>Pan, Shufen</name>
      </author>
      <author>
        <name>Winiwarter, Wilfried</name>
      </author>
      <author>
        <name>Zaehle, Sönke</name>
      </author>
      <author>
        <name>Zhou, Feng</name>
      </author>
      <author>
        <name>Jackson, Robert B</name>
      </author>
      <author>
        <name>Bange, Hermann W</name>
      </author>
      <author>
        <name>Berthet, Sarah</name>
      </author>
      <author>
        <name>Bian, Zihao</name>
      </author>
      <author>
        <name>Bianchi, Daniele</name>
      </author>
      <author>
        <name>Bouwman, Alexander F</name>
      </author>
      <author>
        <name>Buitenhuis, Erik T</name>
      </author>
      <author>
        <name>Dutton, Geoffrey</name>
      </author>
      <author>
        <name>Hu, Minpeng</name>
      </author>
      <author>
        <name>Ito, Akihiko</name>
      </author>
      <author>
        <name>Jain, Atul K</name>
      </author>
      <author>
        <name>Jeltsch-Thömmes, Aurich</name>
      </author>
      <author>
        <name>Joos, Fortunat</name>
      </author>
      <author>
        <name>Kou-Giesbrecht, Sian</name>
      </author>
      <author>
        <name>Krummel, Paul B</name>
      </author>
      <author>
        <name>Lan, Xin</name>
      </author>
      <author>
        <name>Landolfi, Angela</name>
      </author>
      <author>
        <name>Lauerwald, Ronny</name>
      </author>
      <author>
        <name>Li, Ya</name>
      </author>
      <author>
        <name>Lu, Chaoqun</name>
      </author>
      <author>
        <name>Maavara, Taylor</name>
      </author>
      <author>
        <name>Manizza, Manfredi</name>
      </author>
      <author>
        <name>Millet, Dylan B</name>
      </author>
      <author>
        <name>Mühle, Jens</name>
      </author>
      <author>
        <name>Patra, Prabir K</name>
      </author>
      <author>
        <name>Peters, Glen P</name>
      </author>
      <author>
        <name>Qin, Xiaoyu</name>
      </author>
      <author>
        <name>Raymond, Peter</name>
      </author>
      <author>
        <name>Resplandy, Laure</name>
      </author>
      <author>
        <name>Rosentreter, Judith A</name>
      </author>
      <author>
        <name>Shi, Hao</name>
      </author>
      <author>
        <name>Sun, Qing</name>
      </author>
      <author>
        <name>Tonina, Daniele</name>
      </author>
      <author>
        <name>Tubiello, Francesco N</name>
      </author>
      <author>
        <name>van der Werf, Guido R</name>
      </author>
      <author>
        <name>Vuichard, Nicolas</name>
      </author>
      <author>
        <name>Wang, Junjie</name>
      </author>
      <author>
        <name>Wells, Kelley C</name>
      </author>
      <author>
        <name>Western, Luke M</name>
      </author>
      <author>
        <name>Wilson, Chris</name>
      </author>
      <author>
        <name>Yang, Jia</name>
      </author>
      <author>
        <name>Yao, Yuanzhi</name>
      </author>
      <author>
        <name>You, Yongfa</name>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
    </item>
    <item>
      <title>A multi-model assessment of the Global Warming Potential of hydrogen</title>
      <link>https://escholarship.org/uc/item/6bj539cw</link>
      <description>With increasing global interest in molecular hydrogen to replace fossil fuels, more attention is being paid to potential leakages of hydrogen into the atmosphere and its environmental consequences. Hydrogen is not directly a greenhouse gas, but its chemical reactions change the abundances of the greenhouse gases methane, ozone, and stratospheric water vapor, as well as aerosols. Here, we use a model ensemble of five global atmospheric chemistry models to estimate the 100-year time-horizon Global Warming Potential (GWP100) of hydrogen. We estimate a hydrogen GWP100 of 11.6 ± 2.8 (one standard deviation). The uncertainty range covers soil uptake, photochemical production of hydrogen, the lifetimes of hydrogen and methane, and the hydroxyl radical feedback on methane and hydrogen. The hydrogen-induced changes are robust across the different models. It will be important to keep hydrogen leakages at a minimum to accomplish the benefits of switching to a hydrogen economy.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6bj539cw</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Sand, Maria</name>
      </author>
      <author>
        <name>Skeie, Ragnhild Bieltvedt</name>
      </author>
      <author>
        <name>Sandstad, Marit</name>
      </author>
      <author>
        <name>Krishnan, Srinath</name>
      </author>
      <author>
        <name>Myhre, Gunnar</name>
      </author>
      <author>
        <name>Bryant, Hannah</name>
      </author>
      <author>
        <name>Derwent, Richard</name>
      </author>
      <author>
        <name>Hauglustaine, Didier</name>
      </author>
      <author>
        <name>Paulot, Fabien</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Stevenson, David</name>
      </author>
    </item>
    <item>
      <title>Data-rate-aware FPGA-based Acceleration Framework for Streaming Applications</title>
      <link>https://escholarship.org/uc/item/5qc6s3rx</link>
      <description>In heterogeneous architectures, FPGAs are not only expected to provide higher performance, but also to provide a more energy efficient solution for computationally intensive tasks. While parallelism and pipelining enhance performance on FPGA platforms, the data transfer rate from/to off-chip memory can cause performance degradation. We propose an automated high-level synthesis framework for FPGA-based acceleration of nested loops on large multidimensional input data sets. Given the high-level of parallelism in such applications, our proposed data prefetching algorithm determines the data rate for each parallel datapath. The empirical results on a case study in scientific computing show that FPGA mapping of such nested loops accelerates the application compared to traditional mapping on multicores. The FPGA-accelerated computation results in 3x speedup in runtime and 27x energy-delay-product savings compared to multicore computation.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5qc6s3rx</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Rezaei, Siavash</name>
      </author>
      <author>
        <name>Hernandez-Calderon, Cesar-Alejandro</name>
      </author>
      <author>
        <name>Mirzamohammadi, Saeed</name>
      </author>
      <author>
        <name>Bozorgzadeh, Eli</name>
      </author>
      <author>
        <name>Veeidenbaum, Alexander</name>
      </author>
      <author>
        <name>Nicolau, Alex</name>
        <uri>https://orcid.org/0009-0003-9833-8455</uri>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>Point of Departure</title>
      <link>https://escholarship.org/uc/item/0mz1f2h6</link>
      <description>1.1. The Setting This chapter describes the information basis for the Fifth Assessment Report (AR5) of IPCC Working Group II (WGII) and the rationale for its structure. As the starting point of WGII AR5, the chapter begins with an analysis of how the literature for the assessment has developed through time and proceeds with an overview of how the framing and content of the WGII reports have changed since the first IPCC report was published in 1990. The future climate scenarios used in AR5 are a marked change from those used in the Third (TAR, 2001) and Fourth (AR4, 2007) Assessment Reports; this shift is described here, along with the new AR5 guidance for communicating scientific uncertainty. The chapter provides a summary of the most relevant key findings from the IPCC Special Report on Renewable Energy Sources and Climate Change Mitigation (IPCC, 2011), the IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation (IPCC, 2012),...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0mz1f2h6</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Burkett, Virginia R</name>
      </author>
      <author>
        <name>Suarez, Avelino G</name>
      </author>
      <author>
        <name>Bindi, Marco</name>
      </author>
      <author>
        <name>Conde, Cecilia</name>
      </author>
      <author>
        <name>Mukerji, Rupa</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>St Clair, Asuncion Lera</name>
      </author>
      <author>
        <name>Yohe, Gary W</name>
      </author>
      <author>
        <name>Cornell, Sarah</name>
      </author>
      <author>
        <name>Mach, Katharine J</name>
      </author>
      <author>
        <name>Mastrandrea, Michael D</name>
      </author>
      <author>
        <name>Minx, Jan</name>
      </author>
      <author>
        <name>Pravettoni, Riccardo</name>
      </author>
      <author>
        <name>Seyboth, Kristin</name>
      </author>
      <author>
        <name>von Stechow, Christoph</name>
      </author>
    </item>
    <item>
      <title>The Energy Exascale Earth System Model Version 3: 1. Overview of the Atmospheric Component</title>
      <link>https://escholarship.org/uc/item/0c1886x4</link>
      <description>Abstract This paper describes the atmospheric component of the US Department of Energy's Energy Exascale Earth System Model (E3SM) version 3. Significant updates have been made to the atmospheric physics compared to earlier versions. Specifically, interactive gas chemistry has been implemented, along with improved representations of aerosols and dust emissions. A new stratiform cloud microphysics scheme more physically treats ice processes and aerosol‐cloud interactions. The deep convection parameterization has been largely improved with sophisticated microphysics for convective clouds, making model convection sensitive to large‐scale dynamics, and incorporating the dynamical and physical effects of organized mesoscale convection. Improvements in aerosol wet removal processes and parameter re‐tuning of key aerosol and cloud processes have improved model aerosol radiative forcing. The model's vertical resolution has increased from 72 to 80 layers with the extra eight layers added...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0c1886x4</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Xie, Shaocheng</name>
      </author>
      <author>
        <name>Terai, Christopher R</name>
      </author>
      <author>
        <name>Wang, Hailong</name>
      </author>
      <author>
        <name>Tang, Qi</name>
      </author>
      <author>
        <name>Fan, Jiwen</name>
      </author>
      <author>
        <name>Burrows, Susannah</name>
      </author>
      <author>
        <name>Lin, Wuyin</name>
      </author>
      <author>
        <name>Wu, Mingxuan</name>
      </author>
      <author>
        <name>Song, Xiaoliang</name>
      </author>
      <author>
        <name>Zhang, Yuying</name>
      </author>
      <author>
        <name>Taylor, Mark A</name>
      </author>
      <author>
        <name>Golaz, Jean‐Christophe</name>
      </author>
      <author>
        <name>Benedict, James J</name>
      </author>
      <author>
        <name>Chen, Chih‐Chieh‐Jack</name>
      </author>
      <author>
        <name>Feng, Yan</name>
      </author>
      <author>
        <name>Hannah, Walter M</name>
      </author>
      <author>
        <name>Ke, Ziming</name>
      </author>
      <author>
        <name>Shan, Yunpeng</name>
      </author>
      <author>
        <name>Larson, Vincent E</name>
      </author>
      <author>
        <name>Liu, Xiaohong</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Richter, Jadwiga H</name>
      </author>
      <author>
        <name>Shrivastava, Manish</name>
      </author>
      <author>
        <name>Wan, Hui</name>
      </author>
      <author>
        <name>Zhang, Guang J</name>
      </author>
      <author>
        <name>Zhang, Kai</name>
      </author>
      <author>
        <name>Bradley, Andrew M</name>
      </author>
      <author>
        <name>Cameron‐Smith, Philip</name>
      </author>
      <author>
        <name>Damiano, Luis</name>
      </author>
      <author>
        <name>Debusschere, Bert J</name>
      </author>
      <author>
        <name>Donahue, Aaron S</name>
      </author>
      <author>
        <name>Easter, Richard C</name>
      </author>
      <author>
        <name>Eldred, Michael S</name>
      </author>
      <author>
        <name>Griffin, Brian M</name>
      </author>
      <author>
        <name>Guba, Oksana</name>
      </author>
      <author>
        <name>Guo, Zhun</name>
      </author>
      <author>
        <name>Huang, Xianglei</name>
      </author>
      <author>
        <name>Lee, Jiwoo</name>
      </author>
      <author>
        <name>Lee, Hsiang‐He</name>
      </author>
      <author>
        <name>Lou, Sijia</name>
      </author>
      <author>
        <name>Mahfouz, Naser</name>
      </author>
      <author>
        <name>Moncrieff, Mitchell</name>
      </author>
      <author>
        <name>Mülmenstädt, Johannes</name>
      </author>
      <author>
        <name>Qian, Yun</name>
      </author>
      <author>
        <name>Rasool, Quazi Z</name>
      </author>
      <author>
        <name>Roberts, Andrew F</name>
      </author>
      <author>
        <name>Santos, Sean Patrick</name>
      </author>
      <author>
        <name>Sargsyan, Khachik</name>
      </author>
      <author>
        <name>Shpund, Jacob</name>
      </author>
      <author>
        <name>Singh, Balwinder</name>
      </author>
      <author>
        <name>Tao, Cheng</name>
      </author>
      <author>
        <name>Xie, Jinbo</name>
      </author>
      <author>
        <name>Yang, Yang</name>
      </author>
      <author>
        <name>Zeng, Xubin</name>
      </author>
      <author>
        <name>Zhang, Chengzhu</name>
      </author>
      <author>
        <name>Zhang, Meng</name>
      </author>
      <author>
        <name>Zhang, Shixuan</name>
      </author>
      <author>
        <name>Zhang, Tao</name>
      </author>
      <author>
        <name>Zheng, Xue</name>
      </author>
      <author>
        <name>Jacob, Robert L</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
      <author>
        <name>McCoy, Renata B</name>
      </author>
      <author>
        <name>Bader, David C</name>
      </author>
    </item>
    <item>
      <title>Uncertain climate effects of anthropogenic reactive nitrogen</title>
      <link>https://escholarship.org/uc/item/0534m4p3</link>
      <description>Uncertain climate effects of anthropogenic reactive nitrogen</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0534m4p3</guid>
      <pubDate>Sat, 8 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Hodnebrog, Øivind</name>
      </author>
      <author>
        <name>Jouan, Caroline</name>
      </author>
      <author>
        <name>Hauglustaine, Didier A</name>
      </author>
      <author>
        <name>Paulot, Fabien</name>
      </author>
      <author>
        <name>Bauer, Susanne E</name>
      </author>
      <author>
        <name>Beaudor, Maureen</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Sandstad, Marit</name>
      </author>
      <author>
        <name>Skeie, Ragnhild B</name>
      </author>
      <author>
        <name>Myhre, Gunnar</name>
      </author>
    </item>
    <item>
      <title>Climate change impacts the non-market value of nature: A case study of birding cultural ecosystem services in South Africa</title>
      <link>https://escholarship.org/uc/item/3cd834ch</link>
      <description>Climate change and human activities are increasingly straining global ecosystems, threatening the essential benefits - ecosystem services - they provide to humanity. Among these, cultural ecosystem services (CES) enhance human well-being by providing non-material non-market value beyond what is accounted for within our market based economies. Measuring the impacts of global change on these benefits remains challenging and underdeveloped. In this study, we quantify the current and future non-market use value of birding CES across South Africa, a biodiversity hotspot, by integrating social sensing data, machine learning, and econometric methods. We reveal national patterns of birding CES use and non-market value, identify beneficiaries, and demonstrate that domestic and international beneficiaries are driven by distinct social-ecological dynamics, leading to differing CES vulnerabilities under future climate and biodiversity scenarios. While most protected areas are projected to...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3cd834ch</guid>
      <pubDate>Wed, 5 Nov 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Manley, Kyle</name>
      </author>
      <author>
        <name>Ayompe, Lacour Mody</name>
      </author>
      <author>
        <name>Egoh, Benis N</name>
      </author>
    </item>
    <item>
      <title>Tipping Points of Amazonian Forests: Beyond Myths and Toward Solutions</title>
      <link>https://escholarship.org/uc/item/8sn4f9wr</link>
      <description>Amazon forests are undergoing rapid transformations driven by deforestation, climate change, fire, and other anthropogenic pressures, leading to the hypothesis that they may be nearing a catastrophic tipping point—beyond which ecosystems could shift to a permanently altered state. This review revisits the concept of an Amazon tipping point and assesses the risk of forest collapse from an ecological perspective. We synthesize evidence showing that environmental stressors can drive critical ecosystem transitions, either gradually through incremental loss of resilience or abruptly via synergistic feedbacks. The interplay between climate and land-use change amplifies risks to biodiversity, ecosystem services, and livelihoods. Yet, there is limited evidence for a single, system-wide tipping point. Instead, the Amazon's resilience—although not unlimited—offers meaningful pathways for recovery. The most immediate and effective strategies to support this resilience include slowing forest...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8sn4f9wr</guid>
      <pubDate>Sat, 25 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Brando, Paulo M</name>
      </author>
      <author>
        <name>Barlow, Jos</name>
      </author>
      <author>
        <name>Macedo, Marcia N</name>
      </author>
      <author>
        <name>Silvério, Divino V</name>
      </author>
      <author>
        <name>Ferreira, Joice N</name>
      </author>
      <author>
        <name>Maracahipes, Leandro</name>
      </author>
      <author>
        <name>Anderson, Liana</name>
      </author>
      <author>
        <name>Morton, Douglas C</name>
      </author>
      <author>
        <name>Alencar, Ane</name>
      </author>
      <author>
        <name>Paolucci, Lucas N</name>
      </author>
      <author>
        <name>Jacobs, Sarah</name>
      </author>
      <author>
        <name>Stouter, Hannah</name>
      </author>
      <author>
        <name>Randerson, Jim</name>
      </author>
      <author>
        <name>Flores, Bernardo M</name>
      </author>
      <author>
        <name>Starinchak, Bela</name>
      </author>
      <author>
        <name>Coe, Michael</name>
      </author>
      <author>
        <name>Pires, Mathias M</name>
      </author>
      <author>
        <name>Rattis, Ludmila</name>
      </author>
      <author>
        <name>Armenteras, Dolors</name>
      </author>
      <author>
        <name>Artaxo, Paulo</name>
      </author>
      <author>
        <name>Ordway, Elsa M</name>
        <uri>https://orcid.org/0000-0002-7720-1754</uri>
      </author>
      <author>
        <name>Trumbore, Susan</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
      <author>
        <name>Staver, Carla</name>
      </author>
      <author>
        <name>Berenguer, Erika</name>
      </author>
      <author>
        <name>Menor, Imma Oliveras</name>
      </author>
      <author>
        <name>Maracahipes-Santos, Leonardo</name>
      </author>
      <author>
        <name>Potter, Nathalia</name>
      </author>
      <author>
        <name>Spracklen, Dominick V</name>
      </author>
      <author>
        <name>Uribe, Maria</name>
      </author>
    </item>
    <item>
      <title>Short‐Term Forecasting of Wind Gusts at Airports Across CONUS Using Machine Learning</title>
      <link>https://escholarship.org/uc/item/2vq0c72q</link>
      <description>Abstract Short‐term forecasting of wind gusts, particularly those of higher intensity, is of great societal importance but is challenging due to the presence of multiple gust generation mechanisms. Wind gust observations from eight high‐passenger‐volume airports across the continental United States (CONUS) are summarized and used to develop predictive models of wind gust occurrence and magnitude. These short‐term (same hour) forecast models are built using multiple logistic and linear regression, as well as artificial neural networks (ANNs) of varying complexity. A suite of 19 upper‐air predictors drawn from the ERA5 reanalysis and an autoregressive (AR) term are used. Stepwise procedures instruct predictor selection, and resampling is used to quantify model stability. All models are developed separately for the warm (April–September) and cold (October–March) seasons. Results show that ANNs of 3–5 hidden layers (HLs) generally exhibit higher hit rates than logistic regression...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2vq0c72q</guid>
      <pubDate>Wed, 22 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Coburn, Jacob</name>
      </author>
      <author>
        <name>Arnheim, Julian</name>
        <uri>https://orcid.org/0000-0001-5204-0838</uri>
      </author>
      <author>
        <name>Pryor, Sara C</name>
      </author>
    </item>
    <item>
      <title>Developing a Disaster-Ready Power Grid Agent Through Geophysically-Informed Fault Event Scenarios</title>
      <link>https://escholarship.org/uc/item/14g2v07r</link>
      <description>Management of the nation’s power grid over the coming decades will need to consider multiple climate-driven threats to the power system that can be stressful or even detrimental to its operations. During disasters, grid operators suffer from cognitive overload where the electric grid is severely impacted by the weather, yet grid operators have limited awareness of these factors. Meanwhile, the electric grid is facing an explosion of data coming from a variety of sources which can enable the operator to evaluate the risks and develop mitigation strategies against hazardous events. In this work, we processed heterogeneous environmental and power grid data to learn and model grid behaviour caused by extreme weather events. In this study, we focused on two weather-driven hazards, hurricanes and wildfires, which were analysed for the electric grid of Texas. We then used this data to train a Reinforcement Learning (RL) agent by analysing and predicting future behaviour of the grid during...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/14g2v07r</guid>
      <pubDate>Wed, 22 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Arnheim, Julian B</name>
        <uri>https://orcid.org/0000-0001-5204-0838</uri>
      </author>
      <author>
        <name>Mortlock, Trier</name>
      </author>
      <author>
        <name>Fathima, Hashmath</name>
      </author>
      <author>
        <name>Pataranutaporn, Pat</name>
      </author>
      <author>
        <name>Ahmed, Nadia</name>
      </author>
      <author>
        <name>Tbaileh, Ahmad</name>
      </author>
      <author>
        <name>Parhizkar, Tarannom</name>
      </author>
    </item>
    <item>
      <title>Near real-time indicators of burn severity in the western U.S. from active fire tracking</title>
      <link>https://escholarship.org/uc/item/0wc3x50m</link>
      <description>BackgroundTimely information on wildfire burn severity is critical to assess and mitigate potential post-fire impacts on soils, vegetation, and hillslope stability. Tracking individual fire spread and intensity using satellite active fire data provides a pathway to near real-time (NRT) information. Here, we generated a large database (n = 2177) of wildfire events in the western United States (U.S.) between 2012 and 2021 using active fire detections from the Visible Infrared Imaging Radiometer Suite (VIIRS) sensor on the Suomi National Polar-orbiting Partnership (SNPP) satellite and the Fire Events Data Suite (FEDS) algorithm to track large fire growth every 12&amp;nbsp;h. We integrated fire tracking data with final fire perimeters and burn severity data from the Monitoring Trends in Burn Severity (MTBS) program to evaluate the relationship between burn severity and fire behavior metrics derived from the fire tracking approach, including the rate of fire spread and average fire radiative...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0wc3x50m</guid>
      <pubDate>Wed, 22 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Orland, Elijah</name>
      </author>
      <author>
        <name>McCabe, Tempest D</name>
      </author>
      <author>
        <name>Chen, Yang</name>
        <uri>https://orcid.org/0000-0002-0993-7081</uri>
      </author>
      <author>
        <name>Scholten, Rebecca C</name>
      </author>
      <author>
        <name>Becker, Zeb</name>
      </author>
      <author>
        <name>Loehman, Rachel A</name>
      </author>
      <author>
        <name>Randerson, James T</name>
      </author>
      <author>
        <name>Coffield, Shane R</name>
      </author>
      <author>
        <name>Liu, Tianjia</name>
      </author>
      <author>
        <name>Shiklomanov, Alexey N</name>
      </author>
      <author>
        <name>Nelson, Kurtis</name>
      </author>
      <author>
        <name>Peterson, Birgit</name>
      </author>
      <author>
        <name>Follette-Cook, Melanie B</name>
      </author>
      <author>
        <name>Morton, Douglas C</name>
      </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>SNICAR-ADv3: a community tool for modeling spectral snow albedo</title>
      <link>https://escholarship.org/uc/item/98p088qf</link>
      <description>The Snow, Ice, and Aerosol Radiative (SNICAR) model has been used in various capacities over the last 15 years to model the spectral albedo of snow with light-absorbing constituents (LACs). Recent studies have extended the model to include an adding-doubling two-stream solver and representations of non-spherical ice particles; carbon dioxide snow; snow algae; and new types of mineral dust, volcanic ash, and brown carbon. New options also exist for ice refractive indices and solar-zenith-angle-dependent surface spectral irradiances used to derive broadband albedo. The model spectral range was also extended deeper into the ultraviolet for studies of extraterrestrial and high-altitude cryospheric surfaces. Until now, however, these improvements and capabilities have not been merged into a unified code base. Here, we document the formulation and evaluation of the publicly available SNICAR-ADv3 source code, web-based model, and accompanying library of constituent optical properties....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/98p088qf</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Flanner, Mark G</name>
      </author>
      <author>
        <name>Arnheim, Julian B</name>
      </author>
      <author>
        <name>Cook, Joseph M</name>
      </author>
      <author>
        <name>Dang, Cheng</name>
      </author>
      <author>
        <name>He, Cenlin</name>
      </author>
      <author>
        <name>Huang, Xianglei</name>
      </author>
      <author>
        <name>Singh, Deepak</name>
      </author>
      <author>
        <name>Skiles, S McKenzie</name>
      </author>
      <author>
        <name>Whicker, Chloe A</name>
      </author>
      <author>
        <name>Zender, Charles S</name>
        <uri>https://orcid.org/0000-0003-0129-8024</uri>
      </author>
    </item>
    <item>
      <title>Contrasting Arctic Amplification Response in the Community Earth System Model Large Ensembles and Implications for the North Atlantic Region</title>
      <link>https://escholarship.org/uc/item/6bt4034d</link>
      <description>The response of the polar jet to climate warming and rapid Arctic change is a leading uncertainty in climate projections and critical to the future of mid-latitude surface weather. Previous studies suggest that CMIP5-6 model projections fall into two groups of either Arctic- or tropically-driven climate change, especially in the North Atlantic. Here, we present distinct warming patterns emerging by the late 21st century between the first two generations of the Community Earth System Model Large Ensemble (CESM-LE) and use daily diagnostics to assess associated changes in mid-latitude circulation. We show that the subsequent versions of CESM represent categorically different storylines of North Atlantic climate change. The first version of CESM-LE (CESM1-LE, hereafter LENS1) exhibits severe Arctic amplification (AA) along with minor reductions in jet waviness. In contrast, CESM2-LE (hereafter LENS2) presents subdued AA, a more pronounced North Atlantic warming hole, and a late-century...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6bt4034d</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Arnheim, JB</name>
      </author>
      <author>
        <name>Peings, Y</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Magnusdottir, G</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>Valuing co-benefits of forest fuels treatment for reducing wildfire risk in California's Sierra Nevada</title>
      <link>https://escholarship.org/uc/item/3nz2j2zv</link>
      <description>As wildfires in the western United States grow in frequency and severity, forest fuels treatment has been increasingly recognized as essential for enhancing forest resilience and mitigating wildfire risks. However, the economic valuation of the treatment's co-benefits remains underexplored, limiting integration into financial and policy decision making. Using highly forested land in California's Sierra Nevada as study areas, this study provides a methodology to quantify the economic benefits of forest fuels treatment in mitigating wildfire-induced losses across multiple ecosystem services, including carbon storage, timber provisioning, erosion regulation, and air-quality regulation. Integrating historical data on forest disturbances, ecological variables, and market-based ecosystem service valuation models, we demonstrate that treatment can substantially reduce wildfire risk and deliver measurable, significant economic benefits at a landscape level. The magnitude of these benefits...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3nz2j2zv</guid>
      <pubDate>Wed, 8 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Guo, Han</name>
      </author>
      <author>
        <name>Goulden, Michael</name>
        <uri>https://orcid.org/0000-0002-9379-3948</uri>
      </author>
      <author>
        <name>Chung, Min Gon</name>
      </author>
      <author>
        <name>Xu, Qingqing</name>
      </author>
      <author>
        <name>Nyelele, Charity</name>
      </author>
      <author>
        <name>Guo, Weichao</name>
      </author>
      <author>
        <name>Egoh, Benis</name>
      </author>
      <author>
        <name>Conklin, Martha</name>
      </author>
      <author>
        <name>Keske, Catherine</name>
        <uri>https://orcid.org/0000-0002-8383-5630</uri>
      </author>
      <author>
        <name>Safeeq, Mohammad</name>
      </author>
      <author>
        <name>Bales, Roger</name>
        <uri>https://orcid.org/0000-0002-0811-8535</uri>
      </author>
    </item>
    <item>
      <title>Disentangling the chemistry and transport impacts of the quasi-biennial oscillation on stratospheric ozone</title>
      <link>https://escholarship.org/uc/item/9jd0v61s</link>
      <description>Abstract. The quasi-biennial oscillation (QBO) in tropical winds perturbs stratospheric ozone throughout much of the atmosphere via changes in transport of ozone and other trace gases, as well as via temperature changes, both of which alter ozone chemistry. Attributing these causes of QBO–ozone variability may provide insights into model-to-model differences that contribute to ozone simulation. Here we develop a novel metric of steady-state ozone (SSO) to separate these effects: SSO calculates the local steady-state response of ozone due to the changes in temperature, chemical species, and overhead ozone column; the response due to circulation change is presumed when SSO shows no response. It is applied to the nudged Department of Energy's Energy Exascale Earth System Model version 2 (E3SMv2) with interactive ozone chemistry to demonstrate its validity. The E3SMv2 simulations nudged to reanalysis data produced reasonable wind and ozone patterns, especially in the tropics. Consistent...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9jd0v61s</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Xie, Jinbo</name>
      </author>
      <author>
        <name>Tang, Qi</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Richter, Jadwiga</name>
      </author>
      <author>
        <name>Zhang, Shixuan</name>
      </author>
    </item>
    <item>
      <title>The NASA Atmospheric Tomography (ATom) Mission: Imaging the Chemistry of the Global Atmosphere</title>
      <link>https://escholarship.org/uc/item/8t75p1td</link>
      <description>This article provides an overview of the NASA Atmospheric Tomography (ATom) mission and a summary of selected scientific findings to date. ATom was an airborne measurements and modeling campaign aimed at characterizing the composition and chemistry of the troposphere over the most remote regions of the Pacific, Southern, Atlantic, and Arctic Oceans, and examining the impact of anthropogenic and natural emissions on a global scale. These remote regions dominate global chemical reactivity and are exceptionally important for global air quality and climate. ATom data provide the in situ measurements needed to understand the range of chemical species and their reactions, and to test satellite remote sensing observations and global models over large regions of the remote atmosphere. Lack of data in these regions, particularly over the oceans, has limited our understanding of how atmospheric composition is changing in response to shifting anthropogenic emissions and physical climate...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8t75p1td</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Thompson, Chelsea R</name>
      </author>
      <author>
        <name>Wofsy, Steven C</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Newman, Paul A</name>
      </author>
      <author>
        <name>Hanisco, Thomas F</name>
      </author>
      <author>
        <name>Ryerson, Thomas B</name>
      </author>
      <author>
        <name>Fahey, David W</name>
      </author>
      <author>
        <name>Apel, Eric C</name>
      </author>
      <author>
        <name>Brock, Charles A</name>
      </author>
      <author>
        <name>Brune, William H</name>
      </author>
      <author>
        <name>Froyd, Karl</name>
      </author>
      <author>
        <name>Katich, Joseph M</name>
      </author>
      <author>
        <name>Nicely, Julie M</name>
      </author>
      <author>
        <name>Peischl, Jeff</name>
      </author>
      <author>
        <name>Ray, Eric</name>
      </author>
      <author>
        <name>Veres, Patrick R</name>
      </author>
      <author>
        <name>Wang, Siyuan</name>
      </author>
      <author>
        <name>Allen, Hannah M</name>
      </author>
      <author>
        <name>Asher, Elizabeth</name>
      </author>
      <author>
        <name>Bian, Huisheng</name>
      </author>
      <author>
        <name>Blake, Donald</name>
        <uri>https://orcid.org/0000-0002-8283-5014</uri>
      </author>
      <author>
        <name>Bourgeois, Ilann</name>
      </author>
      <author>
        <name>Budney, John</name>
      </author>
      <author>
        <name>Bui, T Paul</name>
      </author>
      <author>
        <name>Butler, Amy</name>
      </author>
      <author>
        <name>Campuzano-Jost, Pedro</name>
      </author>
      <author>
        <name>Chang, Cecilia</name>
      </author>
      <author>
        <name>Chin, Mian</name>
      </author>
      <author>
        <name>Commane, Róisín</name>
      </author>
      <author>
        <name>Correa, Gus</name>
      </author>
      <author>
        <name>Crounse, John D</name>
      </author>
      <author>
        <name>Daube, Bruce</name>
      </author>
      <author>
        <name>Dibb, Jack E</name>
      </author>
      <author>
        <name>DiGangi, Joshua P</name>
      </author>
      <author>
        <name>Diskin, Glenn S</name>
      </author>
      <author>
        <name>Dollner, Maximilian</name>
      </author>
      <author>
        <name>Elkins, James W</name>
      </author>
      <author>
        <name>Fiore, Arlene M</name>
      </author>
      <author>
        <name>Flynn, Clare M</name>
      </author>
      <author>
        <name>Guo, Hao</name>
      </author>
      <author>
        <name>Hall, Samuel R</name>
      </author>
      <author>
        <name>Hannun, Reem A</name>
      </author>
      <author>
        <name>Hills, Alan</name>
      </author>
      <author>
        <name>Hintsa, Eric J</name>
      </author>
      <author>
        <name>Hodzic, Alma</name>
      </author>
      <author>
        <name>Hornbrook, Rebecca S</name>
      </author>
      <author>
        <name>Huey, L Greg</name>
      </author>
      <author>
        <name>Jimenez, Jose L</name>
      </author>
      <author>
        <name>Keeling, Ralph F</name>
      </author>
      <author>
        <name>Kim, Michelle J</name>
      </author>
      <author>
        <name>Kupc, Agnieszka</name>
      </author>
      <author>
        <name>Lacey, Forrest</name>
      </author>
      <author>
        <name>Lait, Leslie R</name>
      </author>
      <author>
        <name>Lamarque, Jean-Francois</name>
      </author>
      <author>
        <name>Liu, Junhua</name>
      </author>
      <author>
        <name>McKain, Kathryn</name>
      </author>
      <author>
        <name>Meinardi, Simone</name>
      </author>
      <author>
        <name>Miller, David O</name>
      </author>
      <author>
        <name>Montzka, Stephen A</name>
      </author>
      <author>
        <name>Moore, Fred L</name>
      </author>
      <author>
        <name>Morgan, Eric J</name>
      </author>
      <author>
        <name>Murphy, Daniel M</name>
      </author>
      <author>
        <name>Murray, Lee T</name>
      </author>
      <author>
        <name>Nault, Benjamin A</name>
      </author>
      <author>
        <name>Neuman, J Andrew</name>
      </author>
      <author>
        <name>Nguyen, Louis</name>
      </author>
      <author>
        <name>Gonzalez, Yenny</name>
      </author>
      <author>
        <name>Rollins, Andrew</name>
      </author>
      <author>
        <name>Rosenlof, Karen</name>
      </author>
      <author>
        <name>Sargent, Maryann</name>
      </author>
      <author>
        <name>Schill, Gregory</name>
      </author>
      <author>
        <name>Schwarz, Joshua P</name>
      </author>
      <author>
        <name>Clair, Jason M St</name>
      </author>
      <author>
        <name>Steenrod, Stephen D</name>
      </author>
      <author>
        <name>Stephens, Britton B</name>
      </author>
      <author>
        <name>Strahan, Susan E</name>
      </author>
      <author>
        <name>Strode, Sarah A</name>
      </author>
      <author>
        <name>Sweeney, Colm</name>
      </author>
      <author>
        <name>Thames, Alexander B</name>
      </author>
      <author>
        <name>Ullmann, Kirk</name>
      </author>
      <author>
        <name>Wagner, Nicholas</name>
      </author>
      <author>
        <name>Weber, Rodney</name>
      </author>
      <author>
        <name>Weinzierl, Bernadett</name>
      </author>
      <author>
        <name>Wennberg, Paul O</name>
      </author>
      <author>
        <name>Williamson, Christina J</name>
      </author>
      <author>
        <name>Wolfe, Glenn M</name>
      </author>
      <author>
        <name>Zeng, Linghan</name>
      </author>
    </item>
    <item>
      <title>Trade-offs in aviation impacts on climate favour non-CO2 mitigation</title>
      <link>https://escholarship.org/uc/item/8rd1m47c</link>
      <description>Climate assessments of civil aviation1,2 have consistently quantified the dominant climate-forcing components: (1) CO2 emissions, (2) NOx (NO + NO2) emissions and (3) persistent contrails. All three components exert a positive radiative forcing (RF) and lead to climate warming of similar magnitudes. The aviation community is actively seeking to reduce its climate footprint through advanced engine technologies, more sustainable aviation fuel and optimal routing plans3, 4, 5, 6, 7, 8, 9, 10, 11–12. These approaches usually involve a trade-off of CO2 against NOx or contrails (non-CO2), such as burning 1% more fuel to decrease contrail RF by 4%. Here, we show that a climate-trade-off risk curve derived from uncertainties in the RF components2,13, 14, 15–16 can give the probability that a specified trade-off ratio will produce a climate benefit. For each component, we calculate the integrated effective RF resulting from 1 year of flights: global warming per activity (GWA). The complementary...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8rd1m47c</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Gettelman, Andrew</name>
      </author>
      <author>
        <name>Penner, Joyce E</name>
      </author>
    </item>
    <item>
      <title>CO2 surface variability: from the stratosphere or not?</title>
      <link>https://escholarship.org/uc/item/8124b46c</link>
      <description>Fluctuations in atmospheric CO2 can be measured with great precision and are used to identify human-driven sources as well as natural cycles of ocean and land carbon. One source of variability is the stratosphere, where the influx of aged CO2-depleted air can produce fluctuations at the surface. This process has been speculated to be a potential source of interannual variability (IAV) in CO2 that might obscure the quantification of other sources of IAV. Given the recent success in demonstrating that the stratospheric influx of N2O- and chlorofluorocarbon-depleted air is a dominant source of their surface IAV in the Southern Hemisphere, I apply the same model and measurement analysis here to CO2. Using chemistry-transport modeling or scaling of the observed N2O variability, I find that the stratosphere-driven surface variability in CO2 is at most 10% of the observed IAV and is not an important source. Diagnosing the amplitude of the CO2 annual cycle and its increase from 1985 to...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8124b46c</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>From the middle stratosphere to the surface, using nitrous oxide to constrain the stratosphere–troposphere exchange of ozone</title>
      <link>https://escholarship.org/uc/item/626989bb</link>
      <description>Abstract. Stratosphere–troposphere exchange (STE) is an important source of tropospheric ozone, affecting all of atmospheric chemistry, climate, and air quality. The study of impacts needs STE fluxes to be resolved by latitude and month, and for this, we rely on global chemistry models, whose results diverge greatly. Overall, we lack guidance from model–measurement metrics that inform us about processes and patterns related to the STE flux of ozone (O3). In this work, we use modeled tracers (N2O and CFCl3), whose distributions and budgets can be constrained by satellite and surface observations, allowing us to follow stratospheric signals across the tropopause. The satellite-derived photochemical loss of N2O on annual and quasi-biennial cycles can be matched by the models. The STE flux of N2O-depleted air in our chemistry transport model drives surface variability that closely matches observed fluctuations on both annual and quasi-biennial cycles, confirming the modeled flux....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/626989bb</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Ruiz, Daniel J</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>Deconstruction of tropospheric chemical reactivity using aircraft measurements: the Atmospheric Tomography Mission (ATom) data</title>
      <link>https://escholarship.org/uc/item/5k309741</link>
      <description>The NASA Atmospheric Tomography Mission (ATom) completed four seasonal deployments (August 2016, February 2017, October 2017, May 2018), each with regular 0.2-12 km profiling by transecting the remote Pacific Ocean and Atlantic Ocean basins. Additional data were also acquired for the Southern Ocean, the Arctic basin, and two flights over Antarctica. ATom in situ measurements provide a near-complete chemical characterization of the ∼140 000 10 s (80 m by 2 km) air parcels measured along the flight path. This paper presents the Modeling Data Stream (MDS), a continuous gap-filled record of the 10 s parcels containing the chemical species needed to initialize a gas-phase chemistry model for the budgets of tropospheric ozone and methane. Global 3D models have been used to calculate the Reactivity Data Stream (RDS), which is comprised of the chemical reactivities (production and loss) for methane, ozone, and carbon monoxide, through 24 h integration of the 10 s parcels. These parcels...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5k309741</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Guo, Hao</name>
      </author>
      <author>
        <name>Zhu, Xin</name>
      </author>
    </item>
    <item>
      <title>A Comprehensive Chemistry Evaluation and Diagnostics Package for E3SM – ChemDyg Version 1.1.0</title>
      <link>https://escholarship.org/uc/item/435651wh</link>
      <description>The Chemistry Evaluation and Diagnostics Package (ChemDyg) is an open-source tool designed for the Energy Exascale Earth System Model (E3SM) developed by the U.S. Department of Energy. ChemDyg facilitates routine evaluation, tailored development, and in-depth analysis of atmospheric chemistry through its modular architecture, allowing users to compare model outputs with observational data. Version 1.1.0 introduces a robust set of diagnostic capabilities, including climatology, time evolution of key tracers, diurnal and annual cycle analyses, and extensive budget diagnostics. These features help identify model discrepancies and enhance the representation of atmospheric chemistry in E3SM. Each self-contained diagnostic set includes dedicated scripts and documentation for ease of use. The interactive HTML output improves data accessibility, accelerating chemistry model development. Additionally, ChemDyg's flexible framework allows for customization, enabling users to create unique...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/435651wh</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Lee, Hsiang-He</name>
      </author>
      <author>
        <name>Tang, Qi</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Xie, Jinbo</name>
      </author>
    </item>
    <item>
      <title>Resetting tropospheric OH and CH4 lifetime with ultraviolet H2O absorption</title>
      <link>https://escholarship.org/uc/item/3sv4k2x8</link>
      <description>The decay of methyl chloroform, a banned ozone-depleting substance, has provided a clear observational metric of mean tropospheric hydroxyl radical (OH) abundance. Almost all current global chemistry models calculate about 15% too much OH and thus too rapid methane loss. Methane is a short-lived climate forcer, critical to achieving global warming targets, and this error affects our model projections of climate change. New observations of water vapor absorption in the ultraviolet region (290 to 350 nanometers) imply reductions in sunlight with key photolysis rates decreasing by 8 to 12% in the near-surface tropical atmosphere. Incorporation of this new mechanism in a chemistry-transport model reduces OH and methane loss by only 4%, but combined with other proposed mechanisms, such as tropospheric halogen chemistry (7%), we may be able to resolve this conundrum.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3sv4k2x8</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Zhu, Lei</name>
      </author>
    </item>
    <item>
      <title>Calibrating the Tropospheric Air and Ozone Mass</title>
      <link>https://escholarship.org/uc/item/2kk12099</link>
      <description>Abstract  We divide the atmosphere into distinct spheres based on their physical, chemical, and dynamical traits. In deriving chemical budgets and climate trends, which differ across spheres, we need clearly defined boundaries. Our primary spheres are the troposphere and stratosphere (∼99.9% by mass), and the boundary between them is the tropopause. Every global climate‐weather model has one or more methods to calculate the lapse rate tropopause, but these involve subjective choices and are known to fail near the sub‐tropical jets and polar regions. Age‐of‐air tracers clock the effective time‐distance from the tropopause, allowing unambiguous separation of stratosphere from troposphere in the chaotic jet regions. We apply a global model with synthetic tracer e90 (90‐day e‐folding), focusing on ozone and temperature structures about the tropopause using ozone sonde and satellite observations. We calibrate an observation‐consistent tropopause for e90 using tropics‐plus‐midlatitudes...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2kk12099</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>Gridded surface O3, NOx, and CO abundances for model metrics from the South Korean ground station network</title>
      <link>https://escholarship.org/uc/item/1rw22816</link>
      <description>We present gridded surface air quality datasets over South Korea for three key species - ozone (O3), carbon monoxide (CO), and nitrogen oxides (NOx) - during the time frame of the Korea-US Air Quality (KORUS-AQ) mission (May-June 2016). Mixing ratios for the key species were mapped to 0.1° × 0.1° grid cells (hourly resolution), which were constructed from the 300+ air quality network sites using inverse distance weighting with simple declustering. Cross-comparing the interpolated fields against the site data that were used to create them reveals high prediction skill for O3 (80 %) throughout South Korea and moderate skill (60 %) for CO and NOx on average in densely observed regions after individual mean bias corrections. The gridded O3 and CO interpolations predict the NASA DC-8 observations in the planetary boundary layer (PBL) with high skill (80 %) in the Seoul Metropolitan Area (SMA) after subtracting the mean bias. DC-8 NOx observations were much less predictable on account...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1rw22816</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wilson, Calum P</name>
      </author>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>The Spillover of Tropospheric Ozone Increases Has Hidden the Extent of Stratospheric Ozone Depletion by Halogens</title>
      <link>https://escholarship.org/uc/item/0418t80p</link>
      <description>Stratospheric ozone depletion from halocarbons is partly countered by pollution-driven increases in tropospheric ozone, with transport connecting the two. While recognizing this connection, the ozone assessment's evaluation of observations and processes have often split the chapters at the tropopause boundary. Using a chemistry-transport model we find that air-pollution ozone enhancements in the troposphere spill over into the stratosphere at significant rates, that is, 13%–34% of the excess tropospheric burden appears in the lowermost extra-tropical stratosphere. As we track the anticipated recovery of the observed ozone depletion, we should recognize that two tenths of that recovery may come from the transport of increasing tropospheric ozone into the stratosphere.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0418t80p</guid>
      <pubDate>Mon, 6 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prather, Michael J</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
    </item>
    <item>
      <title>A Framework for Variational Inference and Data Assimilation of Soil Biogeochemical Models Using Normalizing Flows</title>
      <link>https://escholarship.org/uc/item/8fb053sp</link>
      <description>Soil biogeochemical models (SBMs) represent soil variables and their responses to global change. Data assimilation approaches help determine whether SBMs accurately represent soil processes consistent with soil pool and flux measurements. Bayesian inference is commonly used in data assimilation procedures that estimate posterior parameter distributions with Markov chain Monte Carlo (MCMC) methods. The ability to account for data and parameter uncertainty is a strength of MCMC inference, but the computational inefficiency of MCMC methods remains a barrier to their wider application, especially with large data sets. Given the limitations of MCMC approaches, we developed an alternative variational inference framework that uses a method called normalizing flows from the field of machine learning. Normalizing flows rely on deep learning to map probability distributions and approximate SBMs that have been discretized into state space models. As a test of our method, we fit approximated...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8fb053sp</guid>
      <pubDate>Thu, 2 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Xie, HW</name>
      </author>
      <author>
        <name>Sujono, D</name>
      </author>
      <author>
        <name>Ryder, T</name>
      </author>
      <author>
        <name>Sudderth, EB</name>
      </author>
      <author>
        <name>Allison, SD</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
    </item>
    <item>
      <title>Water and climate: Recognize anthropogenic drought</title>
      <link>https://escholarship.org/uc/item/17n220v3</link>
      <description>California's current extreme drought must be a lesson for managing water in a warmer, more densely populated world, say Amir AghaKouchak and colleagues.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/17n220v3</guid>
      <pubDate>Wed, 24 Sep 2025 00:00:00 +0000</pubDate>
      <author>
        <name>AghaKouchak, Amir</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
      <author>
        <name>Feldman, David</name>
        <uri>https://orcid.org/0000-0003-2288-5017</uri>
      </author>
      <author>
        <name>Hoerling, Martin</name>
      </author>
      <author>
        <name>Huxman, Travis</name>
      </author>
      <author>
        <name>Lund, Jay</name>
        <uri>https://orcid.org/0000-0002-7366-3206</uri>
      </author>
    </item>
    <item>
      <title>Opinion: The role of AerChemMIP in advancing climate and air quality research</title>
      <link>https://escholarship.org/uc/item/4463d363</link>
      <description>Opinion: The role of AerChemMIP in advancing climate and air quality research</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4463d363</guid>
      <pubDate>Wed, 27 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Griffiths, Paul T</name>
      </author>
      <author>
        <name>Wilcox, Laura J</name>
      </author>
      <author>
        <name>Allen, Robert J</name>
      </author>
      <author>
        <name>Naik, Vaishali</name>
      </author>
      <author>
        <name>O'Connor, Fiona M</name>
      </author>
      <author>
        <name>Prather, Michael</name>
        <uri>https://orcid.org/0000-0002-9442-8109</uri>
      </author>
      <author>
        <name>Archibald, Alex</name>
      </author>
      <author>
        <name>Brown, Florence</name>
      </author>
      <author>
        <name>Deushi, Makoto</name>
      </author>
      <author>
        <name>Collins, William</name>
      </author>
      <author>
        <name>Fiedler, Stephanie</name>
      </author>
      <author>
        <name>Oshima, Naga</name>
      </author>
      <author>
        <name>Murray, Lee T</name>
      </author>
      <author>
        <name>Samset, Bjørn H</name>
      </author>
      <author>
        <name>Smith, Chris</name>
      </author>
      <author>
        <name>Turnock, Steven</name>
      </author>
      <author>
        <name>Watson-Parris, Duncan</name>
      </author>
      <author>
        <name>Young, Paul J</name>
      </author>
    </item>
    <item>
      <title>Assessment of Submarine Groundwater Discharge (SGD) as a Source of Dissolved Radium and Nutrients to Moorea (French Polynesia) Coastal Waters</title>
      <link>https://escholarship.org/uc/item/9788414b</link>
      <description>Previous work has documented large fluxes of freshwater and nutrients from submarine groundwater discharge (SGD) into the coastal waters of a few volcanic oceanic islands. However, on the majority of such islands, including Moorea (French Polynesia), SGD has not been studied. In this study, we used radium (Ra) isotopes and salinity to investigate SGD and associated nutrient inputs at five coastal sites and Paopao Bay on the north shore of Moorea. Ra activities were highest in coastal groundwater, intermediate in coastal ocean surface water, and lowest in offshore surface water, indicating that high-Ra groundwater was discharging into the coastal ocean. On average, groundwater nitrate and nitrite (N&amp;nbsp;+&amp;nbsp;N), phosphate, ammonium, and silica concentrations were 12, 21, 29, and 33 times greater, respectively, than those in coastal ocean surface water, suggesting that groundwater discharge could be an important source of nutrients to the coastal ocean. Ra and salinity mass balances...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9788414b</guid>
      <pubDate>Mon, 11 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Knee, Karen L</name>
      </author>
      <author>
        <name>Crook, Elizabeth D</name>
        <uri>https://orcid.org/0000-0001-5798-2736</uri>
      </author>
      <author>
        <name>Hench, James L</name>
      </author>
      <author>
        <name>Leichter, James J</name>
      </author>
      <author>
        <name>Paytan, Adina</name>
        <uri>https://orcid.org/0000-0001-8360-4712</uri>
      </author>
    </item>
    <item>
      <title>Analysis of Rare Plant Occurrence Data for Monitoring Prioritization</title>
      <link>https://escholarship.org/uc/item/6nn8r8mj</link>
      <description>Efforts to conserve rare plant species can be limited by a lack of time and funding for monitoring. Understanding species occurrence and distribution patterns within existing protected habitat and throughout the entire species range can help stewards prioritize rare plant monitoring. We created a database of rare plant occurrences from public, private, and research sources to analyze the distribution of rare plant species throughout the existing protected area within the Nature Reserve of Orange County in California, USA. We analyzed species occurrence relative to the urban edge, roads, trails, and mean high tide line. We also determined the vegetation community with the highest number of rare plant species to help prioritize habitats for conservation and restoration. We found that some parts of protected areas have more rare plant species and we also found sampling biases on the location of occurrence data. We found that rare species occur close to roads and trails and the mean...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6nn8r8mj</guid>
      <pubDate>Mon, 11 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Laskey, Hailey</name>
      </author>
      <author>
        <name>Crook, Elizabeth D</name>
        <uri>https://orcid.org/0000-0001-5798-2736</uri>
      </author>
      <author>
        <name>Kimball, Sarah</name>
        <uri>https://orcid.org/0000-0003-3789-4741</uri>
      </author>
    </item>
    <item>
      <title>Combined impacts of sea level rise and invasive species on Cordylanthus maritimus (Salt Marsh Bird’s Beak) in Upper Newport Bay, California</title>
      <link>https://escholarship.org/uc/item/67972223</link>
      <description>From Central California to Northern Baja California, Salt Marsh Bird's Beak (Cordylanthus maritimus subsp. Maritimus; C. maritimus) is an annual hemiparasitic halophyte that is endemic to coastal salt marshes and is both state and federally endangered in the US and Mexico. By the year 2100, sea level is projected to rise by nearly a meter, which will decrease the biodiversity of salt marshes and lead to changes in plant community assemblages, impacting the narrow ecological niche of C. maritimus. Here, we address how sea level rise will impact the preferred elevation range of C. maritimus, and we examine how these impacts will be compounded by the presence of an invasive perennial plant species, Algerian sea lavender (Limonium ramosissimum; L. ramossisimum). We used LiDAR data, plant distributions, and sea level rise projections for the Upper Newport Bay Ecological Reserve to create simplified species distribution models and map current and future ranges for both species, serving...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/67972223</guid>
      <pubDate>Mon, 11 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Spear, Hannah V</name>
      </author>
      <author>
        <name>Zhuang, Zheyuan</name>
      </author>
      <author>
        <name>Selby, Chloe</name>
      </author>
      <author>
        <name>Nicoll, Faith</name>
      </author>
      <author>
        <name>Bañuelas, David C</name>
      </author>
      <author>
        <name>Arenas, Alys</name>
      </author>
      <author>
        <name>Swanson, Amanda</name>
      </author>
      <author>
        <name>Crook, Elizabeth D</name>
        <uri>https://orcid.org/0000-0001-5798-2736</uri>
      </author>
    </item>
    <item>
      <title>Insect-based organic waste management: a sustainable pathway to enhanced ecosystem services and food security</title>
      <link>https://escholarship.org/uc/item/4n0819rr</link>
      <description>Insect-based organic waste management (IBOWM) is revolutionary for tackling organic waste disposal and fostering sustainable food production. This review examines the multifaceted benefits of IBOWM, including its capacity to reduce landfill waste, decrease greenhouse gas emissions, and improve soil health through the practical application of nutrient-rich insect frass. A major contribution of this study is developing a comprehensive framework that illustrates how insect farming enhances ecosystem services by bolstering biodiversity and optimizing nutrient cycling. Drawing on current research and diverse regional case studies, the paper highlights successful IBOWM implementations while also identifying major challenges such as regulatory barriers and public acceptance issues. The economic implications are also explored, with an emphasis on job creation and sustainable livelihoods, particularly in rural communities. Additionally, the review underscores the critical need for supportive...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4n0819rr</guid>
      <pubDate>Mon, 11 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Ayompe, Lacour M</name>
      </author>
      <author>
        <name>Masso, Cargele</name>
      </author>
      <author>
        <name>Epie, Wesner N</name>
      </author>
      <author>
        <name>Crook, Elizabeth D</name>
        <uri>https://orcid.org/0000-0001-5798-2736</uri>
      </author>
      <author>
        <name>Egoh, Benis N</name>
      </author>
    </item>
    <item>
      <title>Historical changes in overtopping probability of dams in the United States</title>
      <link>https://escholarship.org/uc/item/2661h976</link>
      <description>With concerns about aging dams and nonstationary changes in hydrologic extremes (e.g., flooding), questions arise about whether existing dams may be at risk of failure and pose threats to society. Here, we analyzed 33 dams across the United States to investigate temporal trends in dam overtopping probabilities of annual maximum dam water levels. These dams were selected because of the availability of public domain long-term time series of uncontrolled water levels (50 years or longer). We applied updated stationary frequency analyses using generalized extreme value distributions on 30-year rolling periods from 1973 to 2022. The results revealed an overall increasing trend in the number of dams exhibiting critical overtopping probabilities (i.e., low, moderate and high) alongside a decline in the number of non-critical overtopping probabilities (i.e., very low) over time. This approach uncovered overtopping probabilities that traditional analyses based solely on dam&amp;nbsp;water...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2661h976</guid>
      <pubDate>Mon, 4 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Cho, Eunsaem</name>
      </author>
      <author>
        <name>Ahmadisharaf, Ebrahim</name>
      </author>
      <author>
        <name>Villarini, Gabriele</name>
      </author>
      <author>
        <name>AghaKouchak, Amir</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
    </item>
    <item>
      <title>Global Change Asymmetrically Rewires Ecosystems</title>
      <link>https://escholarship.org/uc/item/1r59t4qq</link>
      <description>Global change is complex and multidimensional, making it challenging to understand how human activities affect ecosystem processes. A critical gap in this understanding is how drivers of global change broadly affect food webs. While an industry of studies documents shifts in food webs in response to anthropogenic pressures, a general synthesis is lacking. To address this, we review studies across diverse ecosystems that use stable isotope analysis, energetic food web modelling and gut content analysis to reveal the prevalence of asymmetric rewiring-a phenomenon whereby anthropogenic pressures differentially impact habitats across space, altering some energy pathways within food webs relative to others. We then highlight several examples from the literature to illustrate how this process unfolds. To explore its broader consequences, we use a simple food web model to demonstrate how asymmetric rewiring alters resilience and key ecosystem functions, such as primary and secondary...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1r59t4qq</guid>
      <pubDate>Mon, 4 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Ward, Charlotte A</name>
      </author>
      <author>
        <name>Tunney, Tyler D</name>
      </author>
      <author>
        <name>Donohue, Ian</name>
      </author>
      <author>
        <name>Bieg, Carling</name>
      </author>
      <author>
        <name>Hale, Kayla RS</name>
      </author>
      <author>
        <name>McMeans, Bailey C</name>
      </author>
      <author>
        <name>Moore, John C</name>
        <uri>https://orcid.org/0000-0003-4965-0832</uri>
      </author>
      <author>
        <name>McCann, Kevin S</name>
      </author>
    </item>
    <item>
      <title>Soil functions are shaped by aridity through soil properties and the microbial community structure</title>
      <link>https://escholarship.org/uc/item/74c2067z</link>
      <description>Increasing aridity poses a threat to soil functionality, as it affects the key players -prokaryotes and fungi- responsible for these functions. Studying microbial diversity and functions in soils from different aridity conditions is crucial to understanding potential adaptations and response mechanisms to climate change, which may ultimately affect soil ecosystem multifunctionality. Here, we used a natural humid-to-arid climate gradient to determine: (1) if and how soil functions and microbial communities change across the aridity gradient; and (2) the main drivers of soil function variability along the gradient. We sampled soils (0–10 cm depth) from 12 sites across the Iberian Peninsula and analyzed their prokaryotic and fungal diversity and biomass as well as soil functions (aerobic respiration and extracellular enzyme activities linked to organic carbon, nitrogen and phosphorus degradation), together with soil physicochemical characteristics. Our results showed that increasing...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/74c2067z</guid>
      <pubDate>Sun, 3 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Doménech-Pascual, Anna</name>
      </author>
      <author>
        <name>Rodriguez, Luciana Chavez</name>
      </author>
      <author>
        <name>Han, Xingguo</name>
      </author>
      <author>
        <name>Casas-Ruiz, Joan Pere</name>
      </author>
      <author>
        <name>Ferriol-Ciurana, Joan</name>
      </author>
      <author>
        <name>Donhauser, Jonathan</name>
      </author>
      <author>
        <name>Jordaan, Karen</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Frossard, Aline</name>
      </author>
      <author>
        <name>Priemé, Anders</name>
      </author>
      <author>
        <name>Ramond, Jean-Baptiste</name>
      </author>
      <author>
        <name>Romaní, Anna M</name>
      </author>
    </item>
    <item>
      <title>Evaluating options for balancing the water-electricity nexus in California: Part 1-securingwater availability</title>
      <link>https://escholarship.org/uc/item/5v2640kx</link>
      <description>The technical potential and effectiveness of different water supply options for securing water availability in a large-scale, interconnected water supply system under historical and climate-change augmented inflow and demand conditions were compared. Part 1 of the study focused on determining the scale of the options required to secure water availability and compared the effectiveness of different options. A spatially and temporally resolved model of California'smajor surface reservoirs was developed, and its sensitivity to urban water conservation, desalination, and water reuse was examined. Potential capacities of the different options were determined. Under historical (baseline) hydrology conditions, many individual options were found to be capable of securing water availability alone. Under climate change augment conditions, a portfolio approach was necessary. The water savings from many individual options other than desalination were insufficient in the latter, however, relying...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5v2640kx</guid>
      <pubDate>Wed, 30 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Tarroja, B</name>
      </author>
      <author>
        <name>AghaKouchak, A</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
      <author>
        <name>Sobhani, R</name>
      </author>
      <author>
        <name>Feldman, D</name>
        <uri>https://orcid.org/0000-0003-2288-5017</uri>
      </author>
      <author>
        <name>Jiang, S</name>
        <uri>https://orcid.org/0000-0002-4993-8038</uri>
      </author>
      <author>
        <name>Samuelsen, S</name>
        <uri>https://orcid.org/0000-0002-0420-3951</uri>
      </author>
    </item>
    <item>
      <title>Evaluating options for balancing the water-electricity nexus in California: Part 2-greenhouse gas and renewable energy utilization impacts</title>
      <link>https://escholarship.org/uc/item/20q7d4g3</link>
      <description>A study was conducted to compare the technical potential and effectiveness of differentwater supply options for securing water availability in a large-scale, interconnected water supply system under historical and climatechange augmented inflow and demand conditions. Part 2 of the study focused on determining the greenhouse gas and renewable energy utilization impacts of different pathways to stabilize major surface reservoir levels. Using a detailed electric grid model and taking into account impacts on the operation of the water supply infrastructure, the greenhouse gas emissions and effect on overall grid renewable penetration level was calculated for each water supply option portfolio that successfully secured water availability from Part 1. The effects on the energy signature ofwater supply infrastructurewere found to be just as important as that of the fundamental processes for each option. Under historical (baseline) conditions, many option portfolios were capable of securing...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/20q7d4g3</guid>
      <pubDate>Wed, 30 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Tarroja, B</name>
      </author>
      <author>
        <name>AghaKouchak, A</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
      <author>
        <name>Sobhani, R</name>
      </author>
      <author>
        <name>Feldman, D</name>
        <uri>https://orcid.org/0000-0003-2288-5017</uri>
      </author>
      <author>
        <name>Jiang, S</name>
        <uri>https://orcid.org/0000-0002-4993-8038</uri>
      </author>
      <author>
        <name>Samuelsen, S</name>
        <uri>https://orcid.org/0000-0002-0420-3951</uri>
      </author>
    </item>
    <item>
      <title>Microbiome Adaptation Could Amplify Modeled Projections of Global Soil Carbon Loss With Climate Warming</title>
      <link>https://escholarship.org/uc/item/7sd8p8wc</link>
      <description>Warming alters soil microbial traits through ecological and evolutionary processes, directly influencing the decomposition of organic matter, which significantly affects global soil carbon emissions. Yet, soil carbon models largely ignore these processes and their implications for global responses to warming. Here, we incorporate eco-evolutionary theory into a mechanistic model describing microbial soil carbon decomposition to address the question of whether such processes could have consequential effects on climate carbon feedbacks globally. We assume that a key trait of microbes, their resource allocation to production of exoenzymes (which facilitate decomposition of organic matter)-is optimized to environmental temperatures by natural selection. We find that eco-evolutionary optimization results in microbes allocating more resources to enzyme production under warming. When applied at the global scale, eco-evolutionary optimization enhances the biological realism of soil carbon...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7sd8p8wc</guid>
      <pubDate>Thu, 17 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Abs, Elsa</name>
      </author>
      <author>
        <name>Saleska, Scott R</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Ciais, Philippe</name>
      </author>
      <author>
        <name>Song, Yang</name>
      </author>
      <author>
        <name>Weintraub, Michael N</name>
      </author>
      <author>
        <name>Ferriere, Regis</name>
      </author>
    </item>
    <item>
      <title>Seasonality in the Predictive Skill of Southwest United States Precipitation in the Seasonal Forecast Systems</title>
      <link>https://escholarship.org/uc/item/86w9w84h</link>
      <description>We examine seasonality in the skill of 8 seasonal forecast systems to predict the Southwest United States (SWUS) precipitation between October and April. The models share similarities in the large seasonality they exhibit in their prediction skill over the 1993–2016 period: from October to December, the skill is low if not non-existent, before it gets higher in all the models, with a peak in February-March in the model with an extended hindcast period (European Centre for Medium-Range Weather Forecasts, ECMWF, 1981–2024 period). Using ECMWF, further analyses of daily precipitation illustrate how the model is able to better predict the SWUS precipitation over the February-March forecast target window, versus November-December. Higher precipitation in early February compared to early November is a contributing factor, as is the annual cycle in tropical eastern Pacific sea surface temperature, and the associated El Niño Southern Oscillation teleconnection with the extratropics.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/86w9w84h</guid>
      <pubDate>Wed, 16 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Peings, Yannick</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Dong, Cameron</name>
      </author>
      <author>
        <name>Magnusdottir, Gudrun</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>Decadal Variability of the MJO and Implications for Southwestern United States Wintertime Precipitation Predictability</title>
      <link>https://escholarship.org/uc/item/16q4n9z8</link>
      <description>The Madden-Julian Oscillation (MJO) is the dominant source of tropical convective activity on intraseasonal timescales and a significant influence on extratropical weather through remote teleconnections. Here, we investigate decadal variability of the MJO and its boreal winter teleconnections with the Southwestern United States (SWUS) using an ensemble of historical climate simulations, where tropical atmospheric variability is nudged toward reanalysis. Since the beginning of the 21st century, the MJO has been associated with a wavenumber-5 zonal teleconnection pattern that propagates along the jet stream waveguide. This coupling is absent in the prior two decades, causing significant differences in the Southwestern United States precipitation response. These changes also result in vastly different windows of opportunity for S2S predictability during each period. This decadal variability is potentially associated with the change from a positive to negative Interdecadal Pacific...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/16q4n9z8</guid>
      <pubDate>Wed, 16 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Dong, Cameron</name>
      </author>
      <author>
        <name>Peings, Yannick</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Magnusdottir, Gudrun</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>Climate-driven succession in marine microbiome biodiversity and biogeochemical function</title>
      <link>https://escholarship.org/uc/item/33d330rm</link>
      <description>Seasonal and El Niño-Southern Oscillation (ENSO) warming result in similar ocean changes as predicted with climate change. Climate-driven environmental cycles have strong impacts on microbiome diversity, but impacts on microbiome function are poorly understood. Here we quantify changes in microbial genomic diversity and functioning over 11 years covering seasonal and ENSO cycles at a coastal site in the southern California Current. We observe seasonal oscillations between large-genome lineages during cold, nutrient rich conditions in winter and spring versus small-genome lineages, including Prochlorococcus and Pelagibacter, in summer and fall. Parallel interannual changes separate communities depending on ENSO condition. Biodiversity shifts translate into clear oscillations in microbiome functional potential. Ocean warming induced an ecosystem with less iron but more macronutrient stress genes, depressed organic carbon degradation potential and biomass, and elevated carbon-to-nutrient...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/33d330rm</guid>
      <pubDate>Mon, 30 Jun 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Larkin, Alyse A</name>
      </author>
      <author>
        <name>Brock, Melissa L</name>
      </author>
      <author>
        <name>Fagan, Adam J</name>
      </author>
      <author>
        <name>Moreno, Allison R</name>
      </author>
      <author>
        <name>Gerace, Skylar D</name>
      </author>
      <author>
        <name>Lees, Lauren E</name>
      </author>
      <author>
        <name>Suarez, Stacy A</name>
      </author>
      <author>
        <name>Eloe-Fadrosh, Emiley A</name>
        <uri>https://orcid.org/0000-0002-8162-1276</uri>
      </author>
      <author>
        <name>Martiny, Adam C</name>
        <uri>https://orcid.org/0000-0003-2829-4314</uri>
      </author>
    </item>
    <item>
      <title>Characterization of atmospheric total gaseous mercury at a remote high-elevation site (Col Margherita Observatory, 2543&amp;nbsp;m a.s.l.) in the Italian Alps</title>
      <link>https://escholarship.org/uc/item/9pf4d0wg</link>
      <description>The Col Margherita (MRG) Observatory is a high-altitude background station located in the Eastern Italian Alps. Its elevation and distance from major anthropogenic and natural sources make it ideal for monitoring baseline mercury levels and investigating its geochemical cycles. In this work, total gaseous mercury (TGM), ozone (O3) and meteorological variables were studied to investigate seasonal and diurnal variability of TGM measurements from March 2018 to May 2019. We found that the year-round mean TGM concentration was 1.8 times higher than the annual atmospheric mercury measurements previously reported during the GMOS project at the same measurement site. The seasonal variation of TGM was characterized by high values in spring and summer and lower values in winter. A systematic diel pattern of TGM was obtained, with low concentrations during the daytime and higher concentrations in the late evening. Spatial patterns and temporal changes in TGM, back-trajectories (BTs) and...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9pf4d0wg</guid>
      <pubDate>Wed, 4 Jun 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Vardè, Massimiliano</name>
      </author>
      <author>
        <name>Barbante, Carlo</name>
      </author>
      <author>
        <name>Barbaro, Elena</name>
      </author>
      <author>
        <name>Becherini, Francesca</name>
      </author>
      <author>
        <name>Bonasoni, Paolo</name>
      </author>
      <author>
        <name>Busetto, Maurizio</name>
      </author>
      <author>
        <name>Calzolari, Francescopiero</name>
      </author>
      <author>
        <name>Cozzi, Giulio</name>
      </author>
      <author>
        <name>Cristofanelli, Paolo</name>
      </author>
      <author>
        <name>Dallo, Federico</name>
      </author>
      <author>
        <name>De Blasi, Fabrizio</name>
      </author>
      <author>
        <name>Feltracco, Matteo</name>
      </author>
      <author>
        <name>Gabrieli, Jacopo</name>
      </author>
      <author>
        <name>Gambaro, Andrea</name>
      </author>
      <author>
        <name>Maffezzoli, Niccolò</name>
        <uri>https://orcid.org/0000-0002-8649-9185</uri>
      </author>
      <author>
        <name>Morabito, Elisa</name>
      </author>
      <author>
        <name>Putero, Davide</name>
      </author>
      <author>
        <name>Spolaor, Andrea</name>
      </author>
      <author>
        <name>Cairns, Warren RL</name>
      </author>
    </item>
    <item>
      <title>A gradient-boosted tree framework to model the ice thickness of the world's glaciers (IceBoost v1.1)</title>
      <link>https://escholarship.org/uc/item/0281x7f4</link>
      <description>Knowledge of glacier ice volumes is crucial for constraining future sea level potential, evaluating freshwater resources, and assessing impacts on societies, from regional to global. Motivated by the disparity in existing ice volume estimates, we present IceBoost, a global machine learning framework trained to predict ice thickness at arbitrary coordinates, thereby enabling the generation of spatially distributed thickness maps for individual glaciers. IceBoost is an ensemble of two gradient-boosted trees trained with 3.7 million globally available ice thickness measurements and an array of 39 numerical features. The model error is similar to those of existing models outside polar regions and is up to 30 %-40 % lower at high latitudes. Providing supervision by exposing the model to available glacier thickness measurements reduces the error by a factor of up to 2 to 3. A feature-ranking analysis reveals that geodetic data are the most informative variables, while ice velocity can...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0281x7f4</guid>
      <pubDate>Wed, 4 Jun 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Maffezzoli, Niccolò</name>
      </author>
      <author>
        <name>Rignot, Eric</name>
        <uri>https://orcid.org/0000-0002-3366-0481</uri>
      </author>
      <author>
        <name>Barbante, Carlo</name>
      </author>
      <author>
        <name>Petersen, Troels</name>
      </author>
      <author>
        <name>Vascon, Sebastiano</name>
      </author>
    </item>
    <item>
      <title>Decadal recovery of fungal but not termite deadwood decay in tropical rainforest</title>
      <link>https://escholarship.org/uc/item/2hw4n110</link>
      <description>Deadwood represents ~11% of carbon stocks in tropical rainforest ecosystems and its decay is driven largely by fungi and termites, which contribute to the cycling of carbon and nutrients. Due to land use change, such as forest clearing, secondary growth tropical rainforests are increasingly prevalent around the globe. In secondary growth rainforest, studies found lower decay rates of leaf litter; however, little is known about how deadwood decays in these forests. Here, we tested whether termite and fungal species richness, composition and functions in decaying deadwood were similar in secondary and old-growth tropical rainforests. We assessed termite ability to discover and consume deadwood, as well as fungi community composition and contributions to wood decay. We placed non-native pine blocks, half of which were accessible to termites, in an old-growth rainforest site as a reference and two secondary growth rainforest sites that were restored 4 and 8 years before the start...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2hw4n110</guid>
      <pubDate>Thu, 22 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wijas, Baptiste J</name>
      </author>
      <author>
        <name>Flores‐Moreno, Habacuc</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Cernusak, Lucas A</name>
      </author>
      <author>
        <name>Cheesman, Alexander W</name>
      </author>
      <author>
        <name>Eggleton, Paul</name>
      </author>
      <author>
        <name>Kooyman, Robert M</name>
      </author>
      <author>
        <name>Powell, Jeff R</name>
      </author>
      <author>
        <name>Zanne, Amy E</name>
      </author>
    </item>
    <item>
      <title>Rapid growth and high cloud-forming potential of anthropogenic sulfate aerosol in a thermal power plant plume during COVID lockdown in India</title>
      <link>https://escholarship.org/uc/item/2gg4215z</link>
      <description>The COVID lockdown presented an interesting opportunity to study the anthropogenic emissions from different sectors under relatively cleaner conditions in India. The complex interplays of power production, industry, and transport could be dissected due to the significantly reduced influence of the latter two emission sources. Here, based on measurements of cloud condensation nuclei (CCN) activity and chemical composition of atmospheric aerosols during the lockdown, we report an episodic event resulting from distinct meteorological conditions. This event was marked by rapid growth and high hygroscopicity of new aerosol particles formed in the SO2 plume from a large coal-fired power plant in Southern India. These sulfate-rich particles had high CCN activity and number concentration, indicating high cloud-forming potential. Examining the sensitivity of CCN properties under relatively clean conditions provides important new clues to delineate the contributions of different anthropogenic...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2gg4215z</guid>
      <pubDate>Thu, 22 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Singh, Aishwarya</name>
      </author>
      <author>
        <name>Raj, Subha S</name>
      </author>
      <author>
        <name>Panda, Upasana</name>
      </author>
      <author>
        <name>Kommula, Snehitha M</name>
      </author>
      <author>
        <name>Jose, Christi</name>
      </author>
      <author>
        <name>Liu, Tianjia</name>
        <uri>https://orcid.org/0000-0003-3129-0154</uri>
      </author>
      <author>
        <name>Huang, Shan</name>
      </author>
      <author>
        <name>Swain, Basudev</name>
      </author>
      <author>
        <name>Pöhlker, Mira L</name>
      </author>
      <author>
        <name>Reyes-Villegas, Ernesto</name>
      </author>
      <author>
        <name>Ojha, Narendra</name>
      </author>
      <author>
        <name>Vaishya, Aditya</name>
      </author>
      <author>
        <name>Bigi, Alessandro</name>
      </author>
      <author>
        <name>Ravikrishna, R</name>
      </author>
      <author>
        <name>Zhu, Qiao</name>
      </author>
      <author>
        <name>Shi, Liuhua</name>
      </author>
      <author>
        <name>Allen, James</name>
      </author>
      <author>
        <name>Martin, Scot T</name>
      </author>
      <author>
        <name>McFiggans, Gordon</name>
      </author>
      <author>
        <name>Andreae, Meinrat O</name>
      </author>
      <author>
        <name>Pöschl, Ulrich</name>
      </author>
      <author>
        <name>Coe, Hugh</name>
      </author>
      <author>
        <name>Bianchi, F</name>
      </author>
      <author>
        <name>Su, Hang</name>
      </author>
      <author>
        <name>Kanawade, Vijay P</name>
      </author>
      <author>
        <name>Liu, Pengfei</name>
      </author>
      <author>
        <name>Gunthe, Sachin S</name>
      </author>
    </item>
    <item>
      <title>A Practical Probabilistic Benchmark for AI Weather Models</title>
      <link>https://escholarship.org/uc/item/987636xs</link>
      <description>Abstract Since the weather is chaotic, it is necessary to forecast an ensemble of future states. Recently, multiple AI weather models have emerged claiming breakthroughs in deterministic skill. Unfortunately, it is hard to fairly compare ensembles of AI forecasts because variations in ensembling methodology become confounding and the baseline data volume is immense. We address this by scoring lagged initial condition ensembles—whereby an ensemble can be constructed from a library of deterministic hindcasts. This allows the first parameter‐free intercomparison of leading AI weather models' probabilistic skill against an operational baseline. Lagged ensembles of the two leading AI weather models, GraphCast and Pangu, perform similarly even though the former outperforms the latter in deterministic scoring. These results are elaborated upon by sensitivity tests showing that commonly used multiple time‐step loss functions damage ensemble calibration.
Plain Language Summary 2023 was...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/987636xs</guid>
      <pubDate>Mon, 19 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Brenowitz, Noah D</name>
      </author>
      <author>
        <name>Cohen, Yair</name>
      </author>
      <author>
        <name>Pathak, Jaideep</name>
      </author>
      <author>
        <name>Mahesh, Ankur</name>
      </author>
      <author>
        <name>Bonev, Boris</name>
      </author>
      <author>
        <name>Kurth, Thorsten</name>
      </author>
      <author>
        <name>Durran, Dale R</name>
      </author>
      <author>
        <name>Harrington, Peter</name>
      </author>
      <author>
        <name>Pritchard, Michael S</name>
        <uri>https://orcid.org/0000-0002-0340-6327</uri>
      </author>
    </item>
    <item>
      <title>Trade‐offs among restored ecosystem functions are context‐dependent in Mediterranean‐type regions</title>
      <link>https://escholarship.org/uc/item/66c429fj</link>
      <description>Global biodiversity hotspots, including Mediterranean‐type ecosystems worldwide, are highly threatened by global change that alters biodiversity, ecosystem functions, and services. Some restoration activities enhance ecosystem functions by reintroducing plant species based on known relationships between plant traits and ecosystem processes. Achieving multiple functions across different site conditions, however, requires understanding how abiotic factors like climate and soil, along with plant assemblages, influence ecosystem functions, including their trade‐offs and synergies. We used the ModEST ecosystem simulation model, which integrates carbon, water, and nutrient processes with plant traits, to assess the relationships between restored plant assemblages and ecosystem functions in Mediterranean‐type climates and soils. We investigated whether maximised carbon increment, water use efficiency, and nitrogen use efficiency, along with their trade‐offs and synergies, varied across...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/66c429fj</guid>
      <pubDate>Mon, 12 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Fiedler, Sebastian</name>
      </author>
      <author>
        <name>Perring, Michael P</name>
      </author>
      <author>
        <name>Monteiro, José A</name>
      </author>
      <author>
        <name>Branquinho, Cristina</name>
      </author>
      <author>
        <name>Buzhdygan, Oksana</name>
      </author>
      <author>
        <name>Cavieres, Lohengrin A</name>
      </author>
      <author>
        <name>Cleland, Elsa E</name>
      </author>
      <author>
        <name>Cortina‐Segarra, Jordi</name>
      </author>
      <author>
        <name>Grünzweig, José M</name>
      </author>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Irob, Katja</name>
      </author>
      <author>
        <name>Keenan, Trevor F</name>
        <uri>https://orcid.org/0000-0002-3347-0258</uri>
      </author>
      <author>
        <name>Köbel, Melanie</name>
      </author>
      <author>
        <name>Maestre, Fernando T</name>
      </author>
      <author>
        <name>Pagel, Jörn</name>
      </author>
      <author>
        <name>Rodríguez‐Ramírez, Natalia</name>
      </author>
      <author>
        <name>Ruiz‐Benito, Paloma</name>
      </author>
      <author>
        <name>Schurr, Frank M</name>
      </author>
      <author>
        <name>Sheffer, Efrat</name>
      </author>
      <author>
        <name>Valencia, Enrique</name>
      </author>
      <author>
        <name>Tietjen, Britta</name>
      </author>
    </item>
    <item>
      <title>Recent ice cap snowmelt in Russian High Arctic and anti-correlation with late summer sea ice extent</title>
      <link>https://escholarship.org/uc/item/8vp713tt</link>
      <description>Glacier surface melt dynamics throughout Novaya Zemlya (NovZ) and Severnaya Zemlya (SevZ) serve as a good indicator of ice mass ablation and regional climate change in the Russian High Arctic. Here we report trends of surface melt onset date (MOD) and total melt days (TMD) by combining multiple resolution-enhanced active and passive microwave satellite datasets and analyze the TMD correlations with local temperature and regional sea ice extent. The glacier surface snowpack on SevZ melted significantly earlier (−7.3 days/decade) from 1992 to 2012 and significantly longer (7.7 days/decade) from 1995 to 2011. NovZ experienced large interannual variability in MOD, but its annual mean TMD increased. The snowpack melt on NovZ is more sensitive to temperature fluctuations than SevZ in recent decades. After ruling out the regional temperature influence using partial correlation analysis, the TMD on both archipelagoes is statistically anti-correlated with regional late summer sea ice extent,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8vp713tt</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zhao, Meng</name>
      </author>
      <author>
        <name>Ramage, Joan</name>
      </author>
      <author>
        <name>Semmens, Kathryn</name>
      </author>
      <author>
        <name>Obleitner, Friedrich</name>
      </author>
    </item>
    <item>
      <title>Implications of alder shrub growth for alpine tundra soil properties in Interior Alaska</title>
      <link>https://escholarship.org/uc/item/7c69175h</link>
      <description>The increase in deciduous shrub growth in response to climate change throughout the Arctic tundra has uncertain implications, in part due to a lack of field observations. Here we investigate how increasing alder shrub growth in alpine tundra in Interior Alaska corresponds to active layer thickness and soil physical properties. We documented increased alder growth by combining biomass harvests and dendrochronology with the analysis of remotely sensed Normalized Difference Vegetation Index and fire history. Active layer thickness was measured with a tile probe and carbon and nitrogen pools were assessed via elemental analysis. Shallower organic layers under increasing alder growth indicate that nitrogen-rich, deciduous litter inputs may play a role in accelerating decomposition. Despite the observed reduction in organic carbon stocks, active layer thickness was the same under alder and adjacent graminoid tundra, implying deeper thaw of the underlying mineral soil. This study provides...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7c69175h</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Welch, Allison M</name>
      </author>
      <author>
        <name>Pedron, Shawn A</name>
      </author>
      <author>
        <name>Jespersen, Robert Gus</name>
      </author>
      <author>
        <name>Xu, Xiaomei</name>
      </author>
      <author>
        <name>Martinez, Brittney</name>
      </author>
      <author>
        <name>Khazindar, Yezzen</name>
      </author>
      <author>
        <name>Fiore, Nicole M</name>
      </author>
      <author>
        <name>Goulden, Michael L</name>
      </author>
      <author>
        <name>Czimczik, Claudia I</name>
      </author>
    </item>
    <item>
      <title>Recent fire history enhances semi-arid conifer forest drought resistance</title>
      <link>https://escholarship.org/uc/item/3v91t2tf</link>
      <description>Climate change is amplifying both wildfire burned area and severity, as well as incidents of drought-induced tree mortality (dieback). Direct effects from climate change amplify wildfires and episodes of drought-induced dieback have well-known impacts on forest's ability to regulate climate, provide water, and store carbon. Less understood are how past disturbances produce interaction effects that can change subsequent disturbance occurrence and intensity, with implications for management decisions that can promote forest resistance and resilience. We constructed two parallel forest chrono-sequences by combining a geospatial database of historical fire with satellite and airborne observations of forests in the Sierra Nevada of California to assess the impact of fire history on vegetation recovery, water use (evapotranspiration), and drought-induced forest dieback. We used these data sets to assess two research questions: (1.) Does fire history amplify or reduce drought-dieback...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3v91t2tf</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Norlen, Carl A</name>
        <uri>https://orcid.org/0000-0003-1363-9930</uri>
      </author>
      <author>
        <name>Hemes, Kyle S</name>
      </author>
      <author>
        <name>Wang, Jonathan A</name>
      </author>
      <author>
        <name>Randerson, James T</name>
        <uri>https://orcid.org/0000-0001-6559-7387</uri>
      </author>
      <author>
        <name>Battles, John J</name>
      </author>
      <author>
        <name>Tubbesing, Carmen L</name>
      </author>
      <author>
        <name>Goulden, Michael L</name>
        <uri>https://orcid.org/0000-0002-9379-3948</uri>
      </author>
    </item>
    <item>
      <title>Rising forest exposure and fire severity from climate warming amplify tree cover losses from wildfire in California</title>
      <link>https://escholarship.org/uc/item/3qc9z3cd</link>
      <description>Warmer temperatures and severe drought are driving increases in wildfire activity in the western United States, threatening forest ecosystems. However, identifying the influence of fire severity on tree cover loss (TCL) is challenging using commonly used categorical metrics. In this study, we quantify regional trends in wildfire-driven TCL as the product of annual burned area, average forest exposure (pre-fire tree cover), and average fire severity (relative loss of tree cover). We quantified these trends with Landsat-based 30 m resolution fire and tree cover datasets for California wildfires from 1986-2021. Rates of TCL rose faster than trends in burned area, with the magnitude of tree cover area loss per unit of area burned increasing by 70% from 0.20 ± 0.05 during 1986-1996 to 0.34 ± 0.10 during 2011-2021. Forest exposure (pre-fire tree cover) within fires increased by 41% from a decadal mean of 23.4% ± 5.5% (1986-1996) to 33.1% ± 7.8% (2011-2021). Increasing forest exposure...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3qc9z3cd</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wang, Jonathan A</name>
      </author>
      <author>
        <name>Goulden, Michael L</name>
        <uri>https://orcid.org/0000-0002-9379-3948</uri>
      </author>
      <author>
        <name>Norlen, Carl A</name>
        <uri>https://orcid.org/0000-0003-1363-9930</uri>
      </author>
      <author>
        <name>Bhoot, Ved</name>
      </author>
      <author>
        <name>Coffield, Shane</name>
      </author>
      <author>
        <name>Randerson, James T</name>
        <uri>https://orcid.org/0000-0001-6559-7387</uri>
      </author>
    </item>
    <item>
      <title>Stratospheric sink for chlorofluoromethanes: chlorine atom-catalysed destruction of ozone</title>
      <link>https://escholarship.org/uc/item/13q9n640</link>
      <description>Chlorofluoromethanes are being added to the environment in steadily increasing amounts. These compounds are chemically inert and may remain in the atmosphere for 40–150 years, and concentrations can be expected to reach 10 to 30 times present levels. Photodissociation of the Chlorofluoromethanes in the stratosphere produces significant amounts of chlorine atoms, and leads to the destruction of atmospheric ozone.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/13q9n640</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Molina, Mario J</name>
      </author>
      <author>
        <name>Rowland, F. S.</name>
      </author>
    </item>
    <item>
      <title>Recent Tree Mortality Dampens Semi‐Arid Forest Die‐Off During Subsequent Drought</title>
      <link>https://escholarship.org/uc/item/0x16z4wk</link>
      <description>Abstract  Climate change is expected to increase drought intensity and frequency, which are commonly predicted will threaten the survival of forests. Most forest die‐off projections assume that recent tree mortality will not alter die‐off severity during subsequent droughts. We tested this assumption by comparing die‐off in semi‐arid conifer forest stands in California that were exposed to a single drought in 2012–2015 (“ 2nd Drought Only ”) with forest stands that experienced drought in both 1999–2002 and 2012–2015 (“ Both Droughts ”). We quantified die‐off severity as a reduction in the satellite observed Normalized Difference Moisture Index, and cumulative moisture deficit as negative 4‐year Precipitation minus Evapotranspiration (4‐year Pr‐ET overdraft). Here we show that recent tree morality reduces die‐off severity in semi‐arid conifer forests exposed to subsequent drought. Stands in the 2nd Drought Only sample experienced severe die‐off associated with extreme 4‐year Pr‐ET...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0x16z4wk</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Norlen, Carl A</name>
        <uri>https://orcid.org/0000-0003-1363-9930</uri>
      </author>
      <author>
        <name>Goulden, Michael L</name>
        <uri>https://orcid.org/0000-0002-9379-3948</uri>
      </author>
    </item>
    <item>
      <title>Recent fire history enhances semi-arid conifer forest drought resistance</title>
      <link>https://escholarship.org/uc/item/08j520g1</link>
      <description>Climate change is amplifying both wildfire burned area and severity, as well as incidents of drought-induced tree mortality (dieback). Direct effects from climate change amplify wildfires and episodes of drought-induced dieback have well-known impacts on forest’s ability to regulate climate, provide water, and store carbon. Less understood are how past disturbances produce interaction effects that can change subsequent disturbance occurrence and intensity, with implications for management decisions that can promote forest resistance and resilience. We constructed two parallel forest chrono-sequences by combining a geospatial database of historical fire with satellite and airborne observations of forests in the Sierra Nevada of California to assess the impact of fire history on vegetation recovery, water use (evapotranspiration), and drought-induced forest dieback. We used these data sets to assess two research questions: (1.) Does fire history amplify or reduce drought-dieback...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/08j520g1</guid>
      <pubDate>Mon, 5 May 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Norlen, Carl A</name>
      </author>
      <author>
        <name>Hemes, Kyle S</name>
      </author>
      <author>
        <name>Wang, Jonathan A</name>
      </author>
      <author>
        <name>Randerson, James T</name>
      </author>
      <author>
        <name>Battles, John J</name>
      </author>
      <author>
        <name>Tubbesing, Carmen L</name>
      </author>
      <author>
        <name>Goulden, Michael L</name>
      </author>
    </item>
    <item>
      <title>Frequent rainfall-induced new particle formation within the canopy in the Amazon rainforest</title>
      <link>https://escholarship.org/uc/item/57k190s3</link>
      <description>Atmospheric aerosol particles are essential for forming clouds and precipitation, thereby influencing Earth’s energy budget, water cycle and climate on regional and global scales. However, the origin of aerosol particles over the Amazon rainforest during the wet season is poorly understood. Earlier studies showed new particle formation in the outflow of deep convective clouds and suggested a downward flux of aerosol particles during precipitation events. Here we use comprehensive aerosol, trace gas and meteorological data from the Amazon Tall Tower Observatory to show that rainfall regularly induces bursts of nanoparticles in the nucleation size range. This can be attributed to rain-related scavenging of larger particles and a corresponding reduction of the condensation sink, along with an ozone injection into the forest canopy, which could increase the oxidation of biogenic volatile organic compounds, especially terpenes, and enhance new particle formation. During and after rainfall,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/57k190s3</guid>
      <pubDate>Thu, 24 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Machado, Luiz AT</name>
      </author>
      <author>
        <name>Unfer, Gabriela R</name>
      </author>
      <author>
        <name>Brill, Sebastian</name>
      </author>
      <author>
        <name>Hildmann, Stefanie</name>
      </author>
      <author>
        <name>Pöhlker, Christopher</name>
      </author>
      <author>
        <name>Cheng, Yafang</name>
      </author>
      <author>
        <name>Williams, Jonathan</name>
      </author>
      <author>
        <name>Hartwig, Harder</name>
      </author>
      <author>
        <name>Andreae, Meinrat O</name>
      </author>
      <author>
        <name>Artaxo, Paulo</name>
      </author>
      <author>
        <name>Curtius, Joachim</name>
      </author>
      <author>
        <name>Franco, Marco A</name>
      </author>
      <author>
        <name>Cecchini, Micael A</name>
      </author>
      <author>
        <name>Edtbauer, Achim</name>
      </author>
      <author>
        <name>Hoffmann, Thorsten</name>
      </author>
      <author>
        <name>Holanda, Bruna</name>
      </author>
      <author>
        <name>Khadir, Théodore</name>
      </author>
      <author>
        <name>Krejci, Radovan</name>
      </author>
      <author>
        <name>Kremper, Leslie A</name>
      </author>
      <author>
        <name>Liu, Yunfan</name>
      </author>
      <author>
        <name>Meller, Bruno B</name>
      </author>
      <author>
        <name>Pöhlker, Mira L</name>
      </author>
      <author>
        <name>Quesada, Carlos A</name>
      </author>
      <author>
        <name>Ringsdorf, Akima</name>
      </author>
      <author>
        <name>Riipinen, Ilona</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
      <author>
        <name>Wolff, Stefan</name>
      </author>
      <author>
        <name>Lelieveld, Jos</name>
      </author>
      <author>
        <name>Pöschl, Ulrich</name>
      </author>
    </item>
    <item>
      <title>Lake energy balance response to 21st century warming in the tropical high Andes</title>
      <link>https://escholarship.org/uc/item/5007d5mt</link>
      <description>Lake energy balance response to 21st century warming in the tropical high Andes</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5007d5mt</guid>
      <pubDate>Wed, 9 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Sae-Lim, Jarunetr</name>
      </author>
      <author>
        <name>Konecky, Bronwen L</name>
      </author>
      <author>
        <name>Morrill, Carrie</name>
      </author>
      <author>
        <name>Michelutti, Neal</name>
      </author>
      <author>
        <name>Grooms, Christopher</name>
      </author>
      <author>
        <name>Smol, John P</name>
      </author>
    </item>
    <item>
      <title>Carbon dynamics in long-term starving poplar trees-the importance of older carbohydrates and a shift to lipids during survival.</title>
      <link>https://escholarship.org/uc/item/3f3427f6</link>
      <description>Carbon (C) assimilation can be severely impaired during periods of environmental stress, like drought or defoliation, making trees heavily dependent on the use of C reserve pools for survival; yet, the dynamics of reserve use during periods of reduced C supply are still poorly understood. We used stem girdling in mature poplar trees (Populus tremula L. hybrids), a lipid-storing species, to permanently interrupt the phloem C transport and induced C shortage in the isolated stem section below the girdle and monitored metabolic activity during three campaigns in the growing seasons of 2018, 2019 and 2021. We measured respiratory fluxes (CO2 and O2), non-structural carbon concentration, the respiratory substrate (based on isotopic analysis and CO2/O2 ratio) and the age of the respiratory substrate (based on radiocarbon analysis). Our study shows that poplar trees can survive long periods of reduced C supply from the canopy by switching in metabolism from recent carbohydrates to older...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3f3427f6</guid>
      <pubDate>Fri, 4 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Helm, Juliane</name>
      </author>
      <author>
        <name>Muhr, Jan</name>
      </author>
      <author>
        <name>Hilman, Boaz</name>
      </author>
      <author>
        <name>Kahmen, Ansgar</name>
      </author>
      <author>
        <name>Schulze, Ernst-Detlef</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
      </author>
      <author>
        <name>Herrera-Ramírez, David</name>
      </author>
      <author>
        <name>Hartmann, Henrik</name>
      </author>
    </item>
    <item>
      <title>Bedmap3 updated ice bed, surface and thickness gridded datasets for Antarctica</title>
      <link>https://escholarship.org/uc/item/3k39t2gb</link>
      <description>We present Bedmap3, the latest suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60 °S. Bedmap3 incorporates and adds to all post-1950s datasets previously used for Bedmap2, including 84 new aero-geophysical surveys by 15 data providers, an additional 52 million data points and 1.9 million line-kilometres of measurement. These efforts have filled notable gaps including in major mountain ranges and the deep interior of East Antarctica, along West Antarctic coastlines and on the Antarctic Peninsula. Our new Bedmap3/RINGS grounding line similarly consolidates multiple recent mappings into a single, spatially coherent feature. Combined with updated maps of surface topography, ice shelf thickness, rock outcrops and bathymetry, Bedmap3 reveals in much greater detail the subglacial landscape and distribution of Antarctica’s ice, providing new opportunities to interpret continental-scale landscape...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3k39t2gb</guid>
      <pubDate>Thu, 3 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Pritchard, Hamish D</name>
      </author>
      <author>
        <name>Fretwell, Peter T</name>
      </author>
      <author>
        <name>Fremand, Alice C</name>
      </author>
      <author>
        <name>Bodart, Julien A</name>
      </author>
      <author>
        <name>Kirkham, James D</name>
      </author>
      <author>
        <name>Aitken, Alan</name>
      </author>
      <author>
        <name>Bamber, Jonathan</name>
      </author>
      <author>
        <name>Bell, Robin</name>
      </author>
      <author>
        <name>Bianchi, Cesidio</name>
      </author>
      <author>
        <name>Bingham, Robert G</name>
      </author>
      <author>
        <name>Blankenship, Donald D</name>
      </author>
      <author>
        <name>Casassa, Gino</name>
      </author>
      <author>
        <name>Christianson, Knut</name>
      </author>
      <author>
        <name>Conway, Howard</name>
      </author>
      <author>
        <name>Corr, Hugh FJ</name>
      </author>
      <author>
        <name>Cui, Xiangbin</name>
      </author>
      <author>
        <name>Damaske, Detlef</name>
      </author>
      <author>
        <name>Damm, Volkmar</name>
      </author>
      <author>
        <name>Dorschel, Boris</name>
      </author>
      <author>
        <name>Drews, Reinhard</name>
      </author>
      <author>
        <name>Eagles, Graeme</name>
      </author>
      <author>
        <name>Eisen, Olaf</name>
      </author>
      <author>
        <name>Eisermann, Hannes</name>
      </author>
      <author>
        <name>Ferraccioli, Fausto</name>
      </author>
      <author>
        <name>Field, Elena</name>
      </author>
      <author>
        <name>Forsberg, René</name>
      </author>
      <author>
        <name>Franke, Steven</name>
      </author>
      <author>
        <name>Goel, Vikram</name>
      </author>
      <author>
        <name>Gogineni, Siva Prasad</name>
      </author>
      <author>
        <name>Greenbaum, Jamin</name>
      </author>
      <author>
        <name>Hills, Benjamin</name>
      </author>
      <author>
        <name>Hindmarsh, Richard CA</name>
      </author>
      <author>
        <name>Hoffman, Andrew O</name>
      </author>
      <author>
        <name>Holschuh, Nicholas</name>
      </author>
      <author>
        <name>Holt, John W</name>
      </author>
      <author>
        <name>Humbert, Angelika</name>
      </author>
      <author>
        <name>Jacobel, Robert W</name>
      </author>
      <author>
        <name>Jansen, Daniela</name>
      </author>
      <author>
        <name>Jenkins, Adrian</name>
      </author>
      <author>
        <name>Jokat, Wilfried</name>
      </author>
      <author>
        <name>Jong, Lenneke</name>
      </author>
      <author>
        <name>Jordan, Tom A</name>
      </author>
      <author>
        <name>King, Edward C</name>
      </author>
      <author>
        <name>Kohler, Jack</name>
      </author>
      <author>
        <name>Krabill, William</name>
      </author>
      <author>
        <name>Maton, Joséphine</name>
      </author>
      <author>
        <name>Gillespie, Mette Kusk</name>
      </author>
      <author>
        <name>Langley, Kirsty</name>
      </author>
      <author>
        <name>Lee, Joohan</name>
      </author>
      <author>
        <name>Leitchenkov, German</name>
      </author>
      <author>
        <name>Leuschen, Cartlon</name>
      </author>
      <author>
        <name>Luyendyk, Bruce</name>
        <uri>https://orcid.org/0000-0002-8722-2807</uri>
      </author>
      <author>
        <name>MacGregor, Joseph A</name>
      </author>
      <author>
        <name>MacKie, Emma</name>
      </author>
      <author>
        <name>Moholdt, Geir</name>
      </author>
      <author>
        <name>Matsuoka, Kenichi</name>
      </author>
      <author>
        <name>Morlighem, Mathieu</name>
      </author>
      <author>
        <name>Mouginot, Jérémie</name>
      </author>
      <author>
        <name>Nitsche, Frank O</name>
      </author>
      <author>
        <name>Nost, Ole A</name>
      </author>
      <author>
        <name>Paden, John</name>
      </author>
      <author>
        <name>Pattyn, Frank</name>
      </author>
      <author>
        <name>Popov, Sergey</name>
      </author>
      <author>
        <name>Rignot, Eric</name>
        <uri>https://orcid.org/0000-0002-3366-0481</uri>
      </author>
      <author>
        <name>Rippin, David M</name>
      </author>
      <author>
        <name>Rivera, Andrés</name>
      </author>
      <author>
        <name>Roberts, Jason L</name>
      </author>
      <author>
        <name>Ross, Neil</name>
      </author>
      <author>
        <name>Ruppel, Antonia</name>
      </author>
      <author>
        <name>Schroeder, Dustin M</name>
      </author>
      <author>
        <name>Siegert, Martin J</name>
      </author>
      <author>
        <name>Smith, Andrew M</name>
      </author>
      <author>
        <name>Steinhage, Daniel</name>
      </author>
      <author>
        <name>Studinger, Michael</name>
      </author>
      <author>
        <name>Sun, Bo</name>
      </author>
      <author>
        <name>Tabacco, Ignazio</name>
      </author>
      <author>
        <name>Tinto, Kirsty J</name>
      </author>
      <author>
        <name>Urbini, Stefano</name>
      </author>
      <author>
        <name>Vaughan, David G</name>
      </author>
      <author>
        <name>Wilson, Douglas S</name>
      </author>
      <author>
        <name>Young, Duncan A</name>
      </author>
      <author>
        <name>Zirizzotti, Achille</name>
      </author>
    </item>
    <item>
      <title>Metre-scale vertical zonation of corals and sponges on a deep-marine cliff reflects trophic resource partitioning</title>
      <link>https://escholarship.org/uc/item/0px1568v</link>
      <description>Corals and sponges are considered foundational species and can create biodiversity hotspots in the deep sea, yet little is known of their competitive interactions, particularly with respect to resource partitioning among benthic fauna. Here we report on the feeding ecology of deep-water corals, sponges, ascidians, and anemones from a ~ 450&amp;nbsp;m deep submarine canyon wall off Nova Scotia, Canada. Analysis of bulk stable isotopes of carbon and nitrogen confirms isotopic niche partitioning between species despite their physical proximity. Compound-specific nitrogen isotopes of amino acids (δ15N-AA) separated the taxa along continua of trophic position and benthic-pelagic coupling and resolve the conspicuously enriched bulk nitrogen patterns commonly observed in sponges. Radiocarbon dating (as Δ14C) of tissue samples, particulate organic matter (POM) and dissolved inorganic carbon (DIC) from the Scotian Slope sheds light on food provenance and distinguishes diets dominated by older,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0px1568v</guid>
      <pubDate>Thu, 3 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Greenman, Wilder</name>
      </author>
      <author>
        <name>Murillo, Francisco Javier</name>
      </author>
      <author>
        <name>de Moura Neves, Bárbara</name>
      </author>
      <author>
        <name>Kenchington, Ellen</name>
      </author>
      <author>
        <name>Jasperse, Liam</name>
      </author>
      <author>
        <name>Fox, Aislinn</name>
      </author>
      <author>
        <name>Walker, Brett</name>
      </author>
      <author>
        <name>Edinger, Evan</name>
      </author>
      <author>
        <name>Sherwood, Owen</name>
      </author>
    </item>
    <item>
      <title>Community estimate of global glacier mass changes from 2000 to 2023</title>
      <link>https://escholarship.org/uc/item/2bm4w7f4</link>
      <description>Glaciers are indicators of ongoing anthropogenic climate change1. Their melting leads to increased local geohazards2, and impacts marine3 and terrestrial4,5 ecosystems, regional freshwater resources6, and both global water and energy cycles7,8. Together with the Greenland and Antarctic ice sheets, glaciers are essential drivers of present9,10 and future11, 12–13 sea-level rise. Previous assessments of global glacier mass changes have been hampered by spatial and temporal limitations and the heterogeneity of existing data series14, 15–16. Here we show in an intercomparison exercise that glaciers worldwide lost 273 ± 16 gigatonnes in mass annually from 2000 to 2023, with an increase of 36 ± 10% from the first (2000–2011) to the second (2012–2023) half of the period. Since 2000, glaciers have lost between 2% and 39% of their ice regionally and about 5% globally. Glacier mass loss is about 18% larger than the loss from the Greenland Ice Sheet and more than twice that from the Antarctic...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2bm4w7f4</guid>
      <pubDate>Wed, 2 Apr 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zemp, Michael</name>
      </author>
      <author>
        <name>Jakob, Livia</name>
      </author>
      <author>
        <name>Dussaillant, Inés</name>
      </author>
      <author>
        <name>Nussbaumer, Samuel U</name>
      </author>
      <author>
        <name>Gourmelen, Noel</name>
      </author>
      <author>
        <name>Dubber, Sophie</name>
      </author>
      <author>
        <name>A, Geruo</name>
      </author>
      <author>
        <name>Abdullahi, Sahra</name>
      </author>
      <author>
        <name>Andreassen, Liss Marie</name>
      </author>
      <author>
        <name>Berthier, Etienne</name>
      </author>
      <author>
        <name>Bhattacharya, Atanu</name>
      </author>
      <author>
        <name>Blazquez, Alejandro</name>
      </author>
      <author>
        <name>Boehm Vock, Laura F</name>
      </author>
      <author>
        <name>Bolch, Tobias</name>
      </author>
      <author>
        <name>Box, Jason</name>
      </author>
      <author>
        <name>Braun, Matthias H</name>
      </author>
      <author>
        <name>Brun, Fanny</name>
      </author>
      <author>
        <name>Cicero, Eric</name>
      </author>
      <author>
        <name>Colgan, William</name>
      </author>
      <author>
        <name>Eckert, Nicolas</name>
      </author>
      <author>
        <name>Farinotti, Daniel</name>
      </author>
      <author>
        <name>Florentine, Caitlyn</name>
      </author>
      <author>
        <name>Floricioiu, Dana</name>
      </author>
      <author>
        <name>Gardner, Alex</name>
      </author>
      <author>
        <name>Harig, Christopher</name>
      </author>
      <author>
        <name>Hassan, Javed</name>
      </author>
      <author>
        <name>Hugonnet, Romain</name>
      </author>
      <author>
        <name>Huss, Matthias</name>
      </author>
      <author>
        <name>Jóhannesson, Tómas</name>
      </author>
      <author>
        <name>Liang, Chia-Chun Angela</name>
      </author>
      <author>
        <name>Ke, Chang-Qing</name>
      </author>
      <author>
        <name>Khan, Shfaqat Abbas</name>
      </author>
      <author>
        <name>King, Owen</name>
      </author>
      <author>
        <name>Kneib, Marin</name>
      </author>
      <author>
        <name>Krieger, Lukas</name>
      </author>
      <author>
        <name>Maussion, Fabien</name>
      </author>
      <author>
        <name>Mattea, Enrico</name>
      </author>
      <author>
        <name>McNabb, Robert</name>
      </author>
      <author>
        <name>Menounos, Brian</name>
      </author>
      <author>
        <name>Miles, Evan</name>
      </author>
      <author>
        <name>Moholdt, Geir</name>
      </author>
      <author>
        <name>Nilsson, Johan</name>
      </author>
      <author>
        <name>Pálsson, Finnur</name>
      </author>
      <author>
        <name>Pfeffer, Julia</name>
      </author>
      <author>
        <name>Piermattei, Livia</name>
      </author>
      <author>
        <name>Plummer, Stephen</name>
      </author>
      <author>
        <name>Richter, Andreas</name>
      </author>
      <author>
        <name>Sasgen, Ingo</name>
      </author>
      <author>
        <name>Schuster, Lilian</name>
      </author>
      <author>
        <name>Seehaus, Thorsten</name>
      </author>
      <author>
        <name>Shen, Xiaoyi</name>
      </author>
      <author>
        <name>Sommer, Christian</name>
      </author>
      <author>
        <name>Sutterley, Tyler</name>
      </author>
      <author>
        <name>Treichler, Désirée</name>
      </author>
      <author>
        <name>Velicogna, Isabella</name>
      </author>
      <author>
        <name>Wouters, Bert</name>
      </author>
      <author>
        <name>Zekollari, Harry</name>
      </author>
      <author>
        <name>Zheng, Whyjay</name>
      </author>
    </item>
    <item>
      <title>How Do Model Biases Affect Large-Scale Teleconnections That Control Southwest U.S. Precipitation? Part II: Seasonal Models</title>
      <link>https://escholarship.org/uc/item/6sk408sm</link>
      <description>We explore the skill in predicting southwest United States (SWUS) October–March precipitation and associated large-scale teleconnections in an ensemble of hindcasts from seasonal prediction systems. We identify key model biases that degrade the models’ capability to predict SWUS precipitation. The subtropical jet in the Pacific sector is generally too zonal and elongated. This is reflected in the models’ North Pacific ENSO teleconnections that are generally too weak with exaggerated northwest–southeast tilt, compared to observations. Also, the models are too dependent on tropical, El Niño–like, wave train anomalies for producing high seasonal SWUS precipitation, when in observations there is a larger influence of zonal Rossby wave trains such as the one observed in 2016/17. Overall, this is consistent with biases in the basic-flow-inducing errors in the propagation of zonal wave trains in the North Pacific, which affects SWUS precipitation downstream. Although higher skill may...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6sk408sm</guid>
      <pubDate>Wed, 12 Mar 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Peings, Y</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Dong, C</name>
      </author>
      <author>
        <name>Magnusdottir, G</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>How Do Forecast Model Biases Affect Large-Scale Teleconnections That Control Southwest U.S. Precipitation? Part I: S2S Models</title>
      <link>https://escholarship.org/uc/item/1xv6t3nw</link>
      <description>We analyze biases in subseasonal forecast models and their effect on Southwest United States (SWUS) precipitation prediction (2–6-week time scale). Cluster analyses identify three primary wave trains associated with SWUS precipitation: a meridional El Niño–Southern Oscillation (ENSO)–type wave train, an arching Pacific–North American (PNA)–type wave train, and a circumglobal zonal wave train. Compared to reanalysis, the models overrepresent the arching pattern, underrepresent the zonal pattern, and produce mixed results for the meridional pattern. The arching pattern overrepresentation is linked to model mean flow biases in the midlatitude–subpolar North Pacific, which cause a westward retraction of the region of forbidden linear Rossby wave propagation. The zonal pattern underrepresentation is linked to westerly biases in the subtropical jet, which cause a westward retraction of the waveguide in the midlatitude eastern North Pacific and divert wave trains southward. These results...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1xv6t3nw</guid>
      <pubDate>Wed, 12 Mar 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Dong, Cameron</name>
      </author>
      <author>
        <name>Peings, Yannick</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Magnusdottir, Gudrun</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>Interannual Influence of Antarctic Sea Ice on Southern Hemisphere Stratosphere‐Troposphere Coupling</title>
      <link>https://escholarship.org/uc/item/1wd032p3</link>
      <description>While weakening of the boreal polar vortex may be caused by autumnal Arctic sea ice loss, less is known about the interannual influence of Antarctic sea ice on stratosphere-troposphere coupling in the Southern Hemisphere. Identifying any relationship over the short satellite period is difficult due to sampling variability and anthropogenic modification of the austral polar vortex. To circumvent these issues, we use large ensembles of fixed boundary condition simulations from the Community Atmosphere Model (CAM) and Whole Atmosphere Community Climate Model (WACCM) to assess if and how interannual fluctuations in winter Antarctic sea ice influence spring planetary-scale waves and the coupled stratosphere-troposphere circulation. Low Antarctic sea ice conditions are found to modulate tropospheric stationary waves to project constructively onto the climatological stationary wave, enhancing upward planetary wave propagation into the austral polar stratosphere. In WACCM, the resulting...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1wd032p3</guid>
      <pubDate>Wed, 12 Mar 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Rea, Divya</name>
      </author>
      <author>
        <name>Elsbury, Dillon</name>
      </author>
      <author>
        <name>Butler, Amy H</name>
      </author>
      <author>
        <name>Sun, Lantao</name>
      </author>
      <author>
        <name>Peings, Yannick</name>
        <uri>https://orcid.org/0000-0001-6852-7333</uri>
      </author>
      <author>
        <name>Magnusdottir, Gudrun</name>
        <uri>https://orcid.org/0000-0001-6079-5886</uri>
      </author>
    </item>
    <item>
      <title>Vertical canopy gradients of respiration drive plant carbon budgets and leaf area index</title>
      <link>https://escholarship.org/uc/item/0zq3b9jr</link>
      <description>Despite its importance for determining global carbon fluxes, leaf respiration remains poorly constrained in land surface models (LSMs). We tested the sensitivity of the Energy Exascale Earth System Model Land Model - Functionally Assembled Terrestrial Ecosystem Simulator (ELM-FATES) to variation in the canopy gradients of leaf maintenance respiration (R&lt;sub&gt;dark&lt;/sub&gt;). We ran global and point simulations varying the canopy gradient of R&lt;sub&gt;dark&lt;/sub&gt; to explore the impacts on forest structure, composition, and carbon cycling. In global simulations, steeper canopy gradients of R&lt;sub&gt;dark&lt;/sub&gt; lead to increased understory survival and leaf biomass. Leaf area index (LAI) increased up to 77% in tropical regions compared with the default parameterization, improving alignment with remotely sensed benchmarks. Global vegetation carbon varied from 308 Pg C to 449 Pg C across the ensemble. In tropical forest simulations, steeper gradients of R&lt;sub&gt;dark&lt;/sub&gt; had a large impact on successional...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0zq3b9jr</guid>
      <pubDate>Wed, 12 Mar 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Needham, Jessica F</name>
        <uri>https://orcid.org/0000-0003-3653-3848</uri>
      </author>
      <author>
        <name>Dey, Sharmila</name>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Lamour, Julien</name>
      </author>
      <author>
        <name>Lemieux, Gregory</name>
        <uri>https://orcid.org/0000-0001-5304-8938</uri>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>Holm, Jennifer</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
    </item>
    <item>
      <title>Observed declines in upper ocean phosphate-to-nitrate availability</title>
      <link>https://escholarship.org/uc/item/2zr2b0cr</link>
      <description>Climate warming is increasing ocean stratification, which in turn should decrease the nutrient flux to the upper ocean. This may slow marine primary productivity, causing cascading effects throughout food webs. However, observing changes in upper ocean nutrients is challenging because surface concentrations are often below detection limits. We show that the nutricline depth, where nutrient concentrations reach well-detected levels, is tied to productivity and upper ocean nutrient availability. Next, we quantify nutricline depths from a global database of observed vertical nitrate and phosphate profiles to assess contemporary trends in global nutrient availability (1972-2022). We find strong evidence that the P-nutricline (phosphacline) is mostly deepening, especially throughout the southern hemisphere, but the N-nutricline (nitracline) remains mostly stable. Earth System Model (ESM) simulations support the hypothesis that reduced iron stress and increased nitrogen fixation buffer...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2zr2b0cr</guid>
      <pubDate>Fri, 28 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Gerace, Skylar D</name>
      </author>
      <author>
        <name>Yu, Jun</name>
      </author>
      <author>
        <name>Moore, J Keith</name>
        <uri>https://orcid.org/0000-0003-4965-0832</uri>
      </author>
      <author>
        <name>Martiny, Adam C</name>
        <uri>https://orcid.org/0000-0003-2829-4314</uri>
      </author>
    </item>
    <item>
      <title>Enhanced CH4 emissions from global wildfires likely due to undetected small fires</title>
      <link>https://escholarship.org/uc/item/5tw87727</link>
      <description>Monitoring methane (CH4) emissions from terrestrial ecosystems is essential for assessing the relative contributions of natural and anthropogenic factors leading to climate change and shaping global climate goals. Fires are a significant source of atmospheric CH4, with the increasing frequency of megafires amplifying their impact. Global fire emissions exhibit large spatiotemporal variations, making the magnitude and dynamics difficult to characterize accurately. In this study, we reconstruct global fire CH4 emissions by integrating satellite carbon monoxide (CO)-based atmospheric inversion with well-constrained fire CH4 to CO emission ratio maps. Here we show that global fire CH4 emissions averaged 24.0 (17.7–30.4) Tg yr−1 from 2003 to 2020, approximately 27% higher (equivalent to 5.1 Tg yr−1) than average estimates from four widely used fire emission models. This discrepancy likely stems from undetected small fires and underrepresented emission intensities in coarse-resolution...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5tw87727</guid>
      <pubDate>Thu, 13 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Zhao, Junri</name>
      </author>
      <author>
        <name>Ciais, Philippe</name>
      </author>
      <author>
        <name>Chevallier, Frederic</name>
      </author>
      <author>
        <name>Canadell, Josep G</name>
      </author>
      <author>
        <name>van der Velde, Ivar R</name>
      </author>
      <author>
        <name>Chuvieco, Emilio</name>
      </author>
      <author>
        <name>Chen, Yang</name>
        <uri>https://orcid.org/0000-0002-0993-7081</uri>
      </author>
      <author>
        <name>Zhang, Qiang</name>
      </author>
      <author>
        <name>He, Kebin</name>
      </author>
      <author>
        <name>Zheng, Bo</name>
      </author>
    </item>
    <item>
      <title>The Role of Deadwood in the Carbon Cycle: Implications for Models, Forest Management, and Future Climates</title>
      <link>https://escholarship.org/uc/item/8dx4s9wf</link>
      <description>Deadwood represents a significant carbon pool and unique biodiversity reservoir in forests and savannas but has been largely overlooked until recently. Storage and release of carbon from deadwood is controlled by interacting decomposition drivers including biotic consumers (animals and microbes) and abiotic factors (water, fire, sunlight, and freeze–thaw). Although previous research has focused mainly on forests, we synthesize deadwood studies across diverse ecosystems with woody vegetation. As changing climates and land-use practices alter the landscape, we expect accelerating but variable rates of inputs and outputs from deadwood pools. Currently, Earth system models implicitly represent only microbial consumers as drivers of wood decomposition; we show that many other factors influence deadwood pools. Forest management practices increasingly recognize deadwood as an important contributor to forest dynamics, biodiversity, and carbon budgets. Together, emerging knowledge from...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8dx4s9wf</guid>
      <pubDate>Wed, 12 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wijas, Baptiste J</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Austin, Amy T</name>
      </author>
      <author>
        <name>Cornwell, William K</name>
      </author>
      <author>
        <name>Cornelissen, J Hans C</name>
      </author>
      <author>
        <name>Eggleton, Paul</name>
      </author>
      <author>
        <name>Fraver, Shawn</name>
      </author>
      <author>
        <name>Ooi, Mark KJ</name>
      </author>
      <author>
        <name>Powell, Jeff R</name>
      </author>
      <author>
        <name>Woodall, Christopher W</name>
      </author>
      <author>
        <name>Zanne, Amy E</name>
      </author>
    </item>
    <item>
      <title>Mortality impacts of the most extreme heat events</title>
      <link>https://escholarship.org/uc/item/08b400s3</link>
      <description>Mortality impacts of the most extreme heat events</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/08b400s3</guid>
      <pubDate>Wed, 12 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Matthews, Tom</name>
      </author>
      <author>
        <name>Raymond, Colin</name>
        <uri>https://orcid.org/0000-0003-3093-5774</uri>
      </author>
      <author>
        <name>Foster, Josh</name>
      </author>
      <author>
        <name>Baldwin, Jane W</name>
        <uri>https://orcid.org/0000-0002-4174-2743</uri>
      </author>
      <author>
        <name>Ivanovich, Catherine</name>
      </author>
      <author>
        <name>Kong, Qinqin</name>
      </author>
      <author>
        <name>Kinney, Patrick</name>
      </author>
      <author>
        <name>Horton, Radley M</name>
      </author>
    </item>
    <item>
      <title>Hydroclimatic extremes threaten groundwater quality and stability</title>
      <link>https://escholarship.org/uc/item/1nf0f051</link>
      <description>Heavy precipitation, drought, and other hydroclimatic extremes occur more frequently than in the past climate reference period (1961–1990). Given their strong effect on groundwater recharge dynamics, these phenomena increase the vulnerability of groundwater quantity and quality. Over the course of the past decade, we have documented changes in the composition of dissolved organic matter in groundwater. We show that fractions of ingressing surface-derived organic molecules increased significantly as groundwater levels declined, whereas concentrations of dissolved organic carbon remained constant. Molecular composition changeover was accelerated following 2018’s extreme summer drought. These findings demonstrate that hydroclimatic extremes promote rapid transport between surface ecosystems and groundwaters, thereby enabling xenobiotic substances to evade microbial processing, accrue in greater abundance in groundwater, and potentially compromise the safe nature of these potable...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1nf0f051</guid>
      <pubDate>Mon, 10 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Schroeter, Simon A</name>
      </author>
      <author>
        <name>Orme, Alice May</name>
      </author>
      <author>
        <name>Lehmann, Katharina</name>
      </author>
      <author>
        <name>Lehmann, Robert</name>
      </author>
      <author>
        <name>Chaudhari, Narendrakumar M</name>
      </author>
      <author>
        <name>Küsel, Kirsten</name>
      </author>
      <author>
        <name>Wang, He</name>
      </author>
      <author>
        <name>Hildebrandt, Anke</name>
      </author>
      <author>
        <name>Totsche, Kai Uwe</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
      <author>
        <name>Gleixner, Gerd</name>
      </author>
    </item>
    <item>
      <title>Removal of dissolved organic carbon in the West Pacific hadal zones</title>
      <link>https://escholarship.org/uc/item/02n3c09k</link>
      <description>The deep oceans are environments of complex carbon dynamics that have the potential to significantly impact the global carbon cycle. However, the role of hadal zones, particularly hadal trenches (water depth &amp;gt; 6 km), in the oceanic dissolved organic carbon (DOC) cycle is not thoroughly investigated. Here we report distinct DOC signatures in the Japan Trench bottom water. We find that up to 34% ± 7% of the DOC in the trench bottom is removed during the northeastward transport of dissolved carbon along the trench axis. This DOC removal increases the overall DOC recalcitrance of the deep Pacific DOC pool, and is potentially enhanced by the earthquake-triggered physical and biogeochemical processes in the hadal trenches. Radiocarbon analysis on representative oceanic transects further reveals that the Pacific deep-water DOC undergoes distinct removal compared to those in the Atlantic and Indian Oceans along the thermohaline transport. Our findings highlight hadal trenches as previously...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/02n3c09k</guid>
      <pubDate>Sat, 1 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chu, Mengfan</name>
      </author>
      <author>
        <name>Bao, Rui</name>
      </author>
      <author>
        <name>Strasser, Michael</name>
      </author>
      <author>
        <name>Ikehara, Ken</name>
      </author>
      <author>
        <name>Ding, Yang</name>
      </author>
      <author>
        <name>Liu, Kejian</name>
      </author>
      <author>
        <name>Liu, Mingzhi</name>
      </author>
      <author>
        <name>Xu, Li</name>
      </author>
      <author>
        <name>Wang, Yonghong</name>
      </author>
      <author>
        <name>Bellanova, Piero</name>
      </author>
      <author>
        <name>Rasbury, Troy</name>
      </author>
      <author>
        <name>Kölling, Martin</name>
      </author>
      <author>
        <name>Riedinger, Natascha</name>
      </author>
      <author>
        <name>Luo, Min</name>
      </author>
      <author>
        <name>März, Christian</name>
      </author>
      <author>
        <name>Jitsuno, Kana</name>
      </author>
      <author>
        <name>Cai, Zhirong</name>
      </author>
      <author>
        <name>McHugh, Cecilia</name>
      </author>
      <author>
        <name>Druffel, Ellen</name>
        <uri>https://orcid.org/0000-0002-7139-1075</uri>
      </author>
    </item>
    <item>
      <title>Contrasting Summertime Trends in Vehicle Combustion Efficiency in Los Angeles, CA and Salt Lake City, UT</title>
      <link>https://escholarship.org/uc/item/7w67q9fv</link>
      <description>Policy interventions and technological advances are mitigating emissions of air pollutants from motor vehicles. As a result, vehicle fleets are expected to progressively combust fuel more efficiently, with a declining ratio of carbon monoxide to carbon dioxide (CO/CO&lt;sub&gt;2&lt;/sub&gt;) in their emissions. We assess trends in traffic combustion efficiency in Los Angeles (LA) and Salt Lake City (SLC) by measuring changes in summertime on-road CO/CO&lt;sub&gt;2&lt;/sub&gt; between 2013 and 2021 using mobile observations. Our data show a reduction in CO/CO&lt;sub&gt;2&lt;/sub&gt; in LA, indicating an improvement in combustion efficiency that likely resulted from stringent regulation of CO emissions. In contrast, we observed an increase in CO/CO&lt;sub&gt;2&lt;/sub&gt; values in SLC. While slower progress in SLC compared to LA may be partially due to a later adoption of vehicle emission regulations in Utah compared to California, differing driving conditions and fleet composition may also be playing a role. This is evidenced...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7w67q9fv</guid>
      <pubDate>Fri, 31 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Yañez, Cindy C</name>
      </author>
      <author>
        <name>Bares, Ryan</name>
      </author>
      <author>
        <name>Czimczik, Claudia I</name>
        <uri>https://orcid.org/0000-0002-8251-6603</uri>
      </author>
      <author>
        <name>Lin, John</name>
      </author>
      <author>
        <name>Zhang, Jiachen</name>
      </author>
      <author>
        <name>Bush, Susan</name>
      </author>
      <author>
        <name>Hopkins, Francesca M</name>
        <uri>https://orcid.org/0000-0002-6110-7675</uri>
      </author>
    </item>
    <item>
      <title>Unraveling climate change-induced compound low-solar-low-wind extremes in China</title>
      <link>https://escholarship.org/uc/item/6wv6328h</link>
      <description>China's pursuit of carbon neutrality targets hinges on a profound shift towards low-carbon energy, primarily reliant on intermittent and variable, yet crucial, solar and wind power sources. In particular, low-solar-low-wind (LSLW) compound extremes present a critical yet largely ignored threat to the reliability of renewable electricity generation. While existing studies have largely evaluated the impacts of average climate-induced changes in renewable energy resources, comprehensive analyses of the compound extremes and, particularly, the underpinning dynamic mechanisms remain scarce. Here we show the dynamic evolution of compound LSLW extremes and their underlying mechanisms across China via coupling multi-model simulations with diagnostic analysis. Our results unveil a strong topographic dependence in the frequency of compound LSLW extremes, with a national average frequency of 16.4 (10th-90th percentile interval ranges from 5.3 to 32.6) days/yr, when renewable energy resources...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6wv6328h</guid>
      <pubDate>Fri, 31 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wang, Licheng</name>
      </author>
      <author>
        <name>Liu, Yawen</name>
      </author>
      <author>
        <name>Zhao, Lei</name>
      </author>
      <author>
        <name>Lu, Xi</name>
      </author>
      <author>
        <name>Huang, Liangdian</name>
      </author>
      <author>
        <name>Jin, Yana</name>
      </author>
      <author>
        <name>Davis, Steven J</name>
      </author>
      <author>
        <name>Aghakouchak, Amir</name>
        <uri>https://orcid.org/0000-0003-4689-8357</uri>
      </author>
      <author>
        <name>Huang, Xin</name>
      </author>
      <author>
        <name>Zhu, Tong</name>
      </author>
      <author>
        <name>Qin, Yue</name>
      </author>
    </item>
    <item>
      <title>Temporal and spatial pattern analysis of escaped prescribed fires in California from 1991 to 2020</title>
      <link>https://escholarship.org/uc/item/995448nq</link>
      <description>BackgroundPrescribed fires play a critical role in reducing the intensity and severity of future wildfires by systematically and widely consuming accumulated vegetation fuel. While the current probability of prescribed fire escape in the United States stands very low, their consequential impact, particularly the large wildfires they cause, raises substantial concerns. The most direct way of understanding this trade-off between wildfire risk reduction and prescribed fire escapes is to explore patterns in the historical prescribed fire records. This study investigates the spatiotemporal patterns of escaped prescribed fires in California from 1991 to 2020, offering insights for resource managers in developing effective forest management and fuel treatment strategies.ResultsThe results reveal that the months close to the beginning and end of the wildfire season, namely May, June, September, and November, have the highest frequency of escaped fires. Under similar environmental conditions,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/995448nq</guid>
      <pubDate>Wed, 29 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Li, Shu</name>
      </author>
      <author>
        <name>Baijnath-Rodino, Janine A</name>
      </author>
      <author>
        <name>York, Robert A</name>
      </author>
      <author>
        <name>Quinn-Davidson, Lenya N</name>
      </author>
      <author>
        <name>Banerjee, Tirtha</name>
        <uri>https://orcid.org/0000-0002-5153-9474</uri>
      </author>
    </item>
    <item>
      <title>Nitrogen Deposition Weakens Soil Carbon Control of Nitrogen Dynamics Across the Contiguous United States</title>
      <link>https://escholarship.org/uc/item/75v4t3fx</link>
      <description>Anthropogenic nitrogen (N) deposition is unequally distributed across space and time, with inputs to terrestrial ecosystems impacted by industry regulations and variations in human activity. Soil carbon (C) content normally controls the fraction of mineralized N that is nitrified (ƒ&lt;sub&gt;nitrified&lt;/sub&gt;), affecting N bioavailability for plants and microbes. However, it is unknown whether N deposition has modified the relationships among soil C, net N mineralization, and net nitrification. To test whether N deposition alters the relationship between soil C and net N transformations, we collected soils from coniferous and deciduous forests, grasslands, and residential yards in 14 regions across the contiguous United States that vary in N deposition rates. We quantified rates of net nitrification and N mineralization, soil chemistry (soil C, N, and pH), and microbial biomass and function (as beta-glucosidase (BG) and N-acetylglucosaminidase (NAG) activity) across these regions. Following...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/75v4t3fx</guid>
      <pubDate>Thu, 23 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Nieland, Matthew A</name>
      </author>
      <author>
        <name>Lacy, Piper</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
      <author>
        <name>Bhatnagar, Jennifer M</name>
      </author>
      <author>
        <name>Doroski, Danica A</name>
      </author>
      <author>
        <name>Frey, Serita D</name>
      </author>
      <author>
        <name>Greaney, Kristen</name>
      </author>
      <author>
        <name>Hobbie, Sarah E</name>
      </author>
      <author>
        <name>Kuebbing, Sara E</name>
      </author>
      <author>
        <name>Lewis, David B</name>
      </author>
      <author>
        <name>McDaniel, Marshall D</name>
      </author>
      <author>
        <name>Perakis, Steven S</name>
      </author>
      <author>
        <name>Raciti, Steve M</name>
      </author>
      <author>
        <name>Shaw, Alanna N</name>
      </author>
      <author>
        <name>Sprunger, Christine D</name>
      </author>
      <author>
        <name>Strickland, Michael S</name>
      </author>
      <author>
        <name>Templer, Pamela H</name>
      </author>
      <author>
        <name>Vietorisz, Corinne</name>
      </author>
      <author>
        <name>Ward, Elisabeth B</name>
      </author>
      <author>
        <name>Keiser, Ashley D</name>
      </author>
    </item>
    <item>
      <title>Rethinking microbial carbon use efficiency in soil models</title>
      <link>https://escholarship.org/uc/item/64d8565z</link>
      <description>Soil models include a key parameter known as carbon use efficiency, which impacts estimates of global carbon storage by determining the flow of carbon into soil pools versus the atmosphere. Microbial-explicit versions of these models are due for an update that recasts carbon use efficiency as an output variable emerging from microbial metabolism.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/64d8565z</guid>
      <pubDate>Thu, 23 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
    </item>
    <item>
      <title>Characterizing suburban soil and microbial properties along a soil age chronosequence</title>
      <link>https://escholarship.org/uc/item/2x18c46h</link>
      <description>Abstract Rapid urbanization is drastically altering ecosystem processes in landscapes around the world. In particular, suburban residential neighborhoods comprise novel ecosystems with water and nutrient inputs that differ greatly from the surrounding land area. These impacts generate concern over the sustainability of urban ecosystems, especially whether they will be characterized by net carbon gain or loss over time. To address this knowledge gap, we established a chronosequence of residential yards in Southern California to test how urban soils change after development. We predicted that urbanized soils would experience shifts in physical characteristics and microbial function over time consistent with ecological succession theory, but residential soils would maintain novel moisture and nutrient regimes compared to undeveloped soils, never “recovering” to a pre‐developed state. We compared different vegetation types to quantify impacts of homeowner landscaping choices and characterized...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2x18c46h</guid>
      <pubDate>Thu, 23 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Suratt, Andie</name>
      </author>
      <author>
        <name>Behl, Kavisha</name>
      </author>
      <author>
        <name>Hong, Wai Lam</name>
      </author>
      <author>
        <name>Yoon, Yae Eun</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
    </item>
    <item>
      <title>Bathymetry of the Antarctic continental shelf and ice shelf cavities from circumpolar gravity anomalies and other data</title>
      <link>https://escholarship.org/uc/item/94r2b6j9</link>
      <description>Bathymetry critically influences the intrusion of warm Circumpolar Deep Water onto the continental shelf and under ice shelf cavities in Antarctica, thereby forcing ice melting, grounding line retreat, and sea level rise. We present a novel and comprehensive bathymetry of Antarctica that includes all ice shelf cavities and previously unmeasured continental shelf areas. The new bathymetry is based on a 3D inversion of a circumpolar compilation of gravity anomalies constrained by measurements from the International Bathymetric Chart of the Southern Ocean, BedMachine Antarctica, and discrete seafloor measurements from seismic and ocean robotic probes. Previously unknown troughs with thicker ice shelf cavities are revealed in many parts of Antarctica, especially East Antarctica. The greater depths of troughs on the continental shelf and ice shelf cavities imply that many glaciers are more vulnerable to ocean subsurface warming than previously thought, which may increase the projections...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/94r2b6j9</guid>
      <pubDate>Mon, 20 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Charrassin, Raphaelle</name>
      </author>
      <author>
        <name>Millan, Romain</name>
      </author>
      <author>
        <name>Rignot, Eric</name>
        <uri>https://orcid.org/0000-0002-3366-0481</uri>
      </author>
      <author>
        <name>Scheinert, Mirko</name>
      </author>
    </item>
    <item>
      <title>Coupled model intercomparison project phase 6 (CMIP6) high resolution model intercomparison project (HighResMIP) bias in extreme rainfall drives underestimation of amazonian precipitation</title>
      <link>https://escholarship.org/uc/item/7rw224xf</link>
      <description>Extreme rainfall events drive the amount and spatial distribution of rainfall in the Amazon and are a key driver of forest dynamics across the basin. This study investigates how the 3-hourly predictions in the High Resolution Model Intercomparison Project (HighResMIP, a component of the recent Coupled Model Intercomparison Project, CMIP6) represent extreme rainfall events at annual, seasonal, and sub-daily time scales. TRMM 3B42 (Tropical Rainfall Measuring Mission) 3 h data were used as observations. Our results showed that eleven out of seventeen HighResMIP models showed the observed association between rainfall and number of extreme events at the annual and seasonal scales. Two models captured the spatial pattern of number of extreme events at the seasonal and annual scales better (higher correlation) than the other models. None of the models captured the sub-daily timing of extreme rainfall, though some reproduced daily totals. Our results suggest that higher model resolution...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7rw224xf</guid>
      <pubDate>Thu, 16 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
      <author>
        <name>Wehner, Michael</name>
      </author>
      <author>
        <name>Dias, Maria Assunção F Silva</name>
      </author>
      <author>
        <name>Ullrich, Paul</name>
        <uri>https://orcid.org/0000-0003-4118-4590</uri>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
    </item>
    <item>
      <title>Increased Occurrence of Large‐Scale Windthrows Across the Amazon Basin</title>
      <link>https://escholarship.org/uc/item/09r3s00n</link>
      <description>Abstract Convective storms with strong downdrafts create windthrows: snapped and uprooted trees that locally alter the structure, composition, and carbon balance of forests. Comparing Landsat imagery from subsequent years, we documented temporal and spatial variation in the occurrence of large (≥30&amp;nbsp;ha) windthrows across the Amazon basin from 1985 to 2020. Over 33 individual years, we detected 3179 large windthrows. Windthrow density was greatest in the central and western Amazon regions, with ∼33% of all events occurring in ∼3% of the monitored area. Return intervals for large windthrows in the same location of these “hotspot” regions are centuries to millennia, while over the rest of the Amazon they are &amp;gt;10,000&amp;nbsp;years. Our data demonstrate a nearly 4‐fold increase in windthrow number and affected area between 1985 (78 windthrows and 6,900&amp;nbsp;ha) and 2020 (264 events and 32,170&amp;nbsp;ha), with more events of &amp;gt;500&amp;nbsp;ha size since 1990. Such extremely large events...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/09r3s00n</guid>
      <pubDate>Wed, 8 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Urquiza‐Muñoz, J David</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
      <author>
        <name>Negrón‐Juárez, Robinson I</name>
      </author>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Brenning, Alexander</name>
      </author>
      <author>
        <name>Vasquez‐Parana, C Michael</name>
      </author>
      <author>
        <name>Marra, Daniel Magnabosco</name>
      </author>
    </item>
    <item>
      <title>The International Bathymetric Chart of the Arctic Ocean Version 5.0</title>
      <link>https://escholarship.org/uc/item/3804m8kv</link>
      <description>Knowledge about seafloor depth, or bathymetry, is crucial for various marine activities, including scientific research, offshore industry, safety of navigation, and ocean exploration. Mapping the central Arctic Ocean is challenging due to the presence of perennial sea ice, which limits data collection to icebreakers, submarines, and drifting ice stations. The International Bathymetric Chart of the Arctic Ocean (IBCAO) was initiated in 1997 with the goal of updating the Arctic Ocean bathymetric portrayal. The project team has since released four versions, each improving resolution and accuracy. Here, we present IBCAO Version 5.0, which offers a resolution four times as high as Version 4.0, with 100 × 100 m grid cells compared to 200 × 200 m. Over 25% of the Arctic Ocean is now mapped with individual depth soundings, based on a criterion that considers water depth. Version 5.0 also represents significant advancements in data compilation and computing techniques. Despite these improvements,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3804m8kv</guid>
      <pubDate>Thu, 2 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Jakobsson, Martin</name>
      </author>
      <author>
        <name>Mohammad, Rezwan</name>
      </author>
      <author>
        <name>Karlsson, Marcus</name>
      </author>
      <author>
        <name>Salas-Romero, Silvia</name>
      </author>
      <author>
        <name>Vacek, Florian</name>
      </author>
      <author>
        <name>Heinze, Florian</name>
      </author>
      <author>
        <name>Bringensparr, Caroline</name>
      </author>
      <author>
        <name>Castro, Carlos F</name>
      </author>
      <author>
        <name>Johnson, Paul</name>
      </author>
      <author>
        <name>Kinney, Juliet</name>
      </author>
      <author>
        <name>Cardigos, Sara</name>
      </author>
      <author>
        <name>Bogonko, Michael</name>
      </author>
      <author>
        <name>Accettella, Daniela</name>
      </author>
      <author>
        <name>Amblas, David</name>
      </author>
      <author>
        <name>An, Lu</name>
      </author>
      <author>
        <name>Bohan, Aileen</name>
      </author>
      <author>
        <name>Brandt, Angelika</name>
      </author>
      <author>
        <name>Bünz, Stefan</name>
      </author>
      <author>
        <name>Canals, Miquel</name>
      </author>
      <author>
        <name>Casamor, José Luis</name>
      </author>
      <author>
        <name>Coakley, Bernard</name>
      </author>
      <author>
        <name>Cornish, Natalie</name>
      </author>
      <author>
        <name>Danielson, Seth</name>
      </author>
      <author>
        <name>Demarte, Maurizio</name>
      </author>
      <author>
        <name>Di Franco, Davide</name>
      </author>
      <author>
        <name>Dickson, Mary-Lynn</name>
      </author>
      <author>
        <name>Dorschel, Boris</name>
      </author>
      <author>
        <name>Dowdeswell, Julian A</name>
      </author>
      <author>
        <name>Dreutter, Simon</name>
      </author>
      <author>
        <name>Fremand, Alice C</name>
      </author>
      <author>
        <name>Hall, John K</name>
      </author>
      <author>
        <name>Hally, Bryan</name>
      </author>
      <author>
        <name>Holland, David</name>
      </author>
      <author>
        <name>Hong, Jon Kuk</name>
      </author>
      <author>
        <name>Ivaldi, Roberta</name>
      </author>
      <author>
        <name>Knutz, Paul C</name>
      </author>
      <author>
        <name>Krawczyk, Diana W</name>
      </author>
      <author>
        <name>Kristofferson, Yngve</name>
      </author>
      <author>
        <name>Lastras, Galderic</name>
      </author>
      <author>
        <name>Leck, Caroline</name>
      </author>
      <author>
        <name>Lucchi, Renata G</name>
      </author>
      <author>
        <name>Masetti, Giuseppe</name>
      </author>
      <author>
        <name>Morlighem, Mathieu</name>
      </author>
      <author>
        <name>Muchowski, Julia</name>
      </author>
      <author>
        <name>Nielsen, Tove</name>
      </author>
      <author>
        <name>Noormets, Riko</name>
      </author>
      <author>
        <name>Plaza-Faverola, Andreia</name>
      </author>
      <author>
        <name>Prescott, Megan M</name>
      </author>
      <author>
        <name>Purser, Autun</name>
      </author>
      <author>
        <name>Rasmussen, Tine L</name>
      </author>
      <author>
        <name>Rebesco, Michele</name>
      </author>
      <author>
        <name>Rignot, Eric</name>
        <uri>https://orcid.org/0000-0002-3366-0481</uri>
      </author>
      <author>
        <name>Rysgaard, Søren</name>
      </author>
      <author>
        <name>Silyakova, Anna</name>
      </author>
      <author>
        <name>Snoeijs-Leijonmalm, Pauline</name>
      </author>
      <author>
        <name>Sørensen, Aqqaluk</name>
      </author>
      <author>
        <name>Straneo, Fiammetta</name>
      </author>
      <author>
        <name>Sutherland, David A</name>
      </author>
      <author>
        <name>Tate, Alex J</name>
      </author>
      <author>
        <name>Travaglini, Paola</name>
      </author>
      <author>
        <name>Trenholm, Nicole</name>
      </author>
      <author>
        <name>van Wijk, Esmee</name>
      </author>
      <author>
        <name>Wallace, Luke</name>
      </author>
      <author>
        <name>Willis, Josh K</name>
      </author>
      <author>
        <name>Wood, Michael</name>
      </author>
      <author>
        <name>Zimmermann, Mark</name>
      </author>
      <author>
        <name>Zinglersen, Karl B</name>
      </author>
      <author>
        <name>Mayer, Larry</name>
      </author>
    </item>
    <item>
      <title>From Ridge 2 Reef: An interdisciplinary model for training the next generation of environmental problem solvers</title>
      <link>https://escholarship.org/uc/item/26c2g667</link>
      <description>Regional and global environmental challenges have become increasingly complex and require broader solutions than a single discipline can provide. Although there is a growing need for interdisciplinary research, many graduate education programs still train students within the confines of a particular discipline or specialty. The Ridge 2 Reef research traineeship program at the University of California, Irvine, aimed to provide transferable and interdisciplinary skill training to prepare graduate students from different disciplines to address current and future environmental challenges. The program achieved its goals through a 'culture of improvement' that ensured trainee needs shaped program management and curriculum. Due to trainee feedback and leaders dedicated to program improvement, there was a complete course overhaul during the first two years of the program, resulting in a final curriculum structure that was more effective and aligned with revised program goals. Program...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/26c2g667</guid>
      <pubDate>Thu, 2 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Hill, Raechel J</name>
      </author>
      <author>
        <name>Djokic, Matea A</name>
        <uri>https://orcid.org/0000-0002-0326-3848</uri>
      </author>
      <author>
        <name>Anderson, Andrea</name>
      </author>
      <author>
        <name>Barbour, Kristin</name>
      </author>
      <author>
        <name>Coleman, Amanda M</name>
      </author>
      <author>
        <name>Guerra, Alexis D</name>
      </author>
      <author>
        <name>Hunt, Courtney</name>
      </author>
      <author>
        <name>Jolly, Amber</name>
      </author>
      <author>
        <name>Long, Jennifer J</name>
      </author>
      <author>
        <name>Manley, Kyle T</name>
      </author>
      <author>
        <name>Montoya, Jonathan L</name>
      </author>
      <author>
        <name>Norlen, Carl A</name>
        <uri>https://orcid.org/0000-0003-1363-9930</uri>
      </author>
      <author>
        <name>Nugent-Suratt, Andie</name>
      </author>
      <author>
        <name>Washburn, Kameko</name>
      </author>
      <author>
        <name>Weber, Samuel</name>
      </author>
      <author>
        <name>Welch, Allison</name>
        <uri>https://orcid.org/0000-0002-2314-7625</uri>
      </author>
      <author>
        <name>Wong, Cynthia</name>
      </author>
      <author>
        <name>Allison, Steven D</name>
        <uri>https://orcid.org/0000-0003-4629-7842</uri>
      </author>
    </item>
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