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    <title>Recent berkeley_geography_oapdeposits items</title>
    <link>https://escholarship.org/uc/berkeley_geography_oapdeposits/rss</link>
    <description>Recent eScholarship items from Open Access Policy Deposits</description>
    <pubDate>Fri, 21 Aug 2026 20:03:16 +0000</pubDate>
    <item>
      <title>Corn and the range: rethinking ranching, agriculture and the feedlot</title>
      <link>https://escholarship.org/uc/item/6n70x6dp</link>
      <description>Debates about modern beef production suffer from a major historical blind spot. For over a century, the feedlot relied on a closed nutrient loop to sustain soil fertility in the United States Corn Belt. Driven by industrial capitalist urbanization, a cattle-grain-beef complex shaped land use, tenure systems, management practices and environmental politics on the expanding frontier, sacrificing the tall-grass prairies and fracturing agrarian resistance to corporate concentration and the Union Stock Yards. Concentrated Animal Feeding Operations (CAFOs) emerged after 1950, breaking the nutrient cycle of the original feedlot and turning the relationship between ranching and agriculture into a dysfunctional one.</description>
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      <pubDate>Wed, 22 Apr 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </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>Water availability modulates maximum canopy heights of low-elevation Amazonian second-growth forests</title>
      <link>https://escholarship.org/uc/item/7xj0c3rz</link>
      <description>Tropical second-growth forests of the Amazon sequester large amounts of carbon and are important carbon sinks, contributing substantially to climate change mitigation, biodiversity conservation, and providing crucial ecosystem services. Deforestation due to selective logging and shifting cultivation is expanding second-growth forest areas in tropical forest regions, which if well managed, regenerate rapidly over time. Maximum forest canopy height is an important metric of biomass and carbon accumulation in second-growth forests and is strongly influenced by water availability. The water limitation hypothesis explains the positive influence of water availability on maximum tree heights and has been examined and demonstrated at a small-scale using field data, and at a global scale, with limited accuracy, using remote sensing data in tropical ecosystems. However, this hypothesis concerning maximum canopy height has not been much studied at regional and national scales for tropical...</description>
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      <pubDate>Tue, 17 Feb 2026 00:00:00 +0000</pubDate>
      <author>
        <name>Mohan, Midhun</name>
      </author>
      <author>
        <name>Pastorello, Gilberto Z</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Adrah, Esmaeel</name>
      </author>
      <author>
        <name>Keller, Michael</name>
      </author>
      <author>
        <name>Ewane, Ewane Basil</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Csillik, Ovidiu</name>
      </author>
      <author>
        <name>Ferraz, Antonio</name>
      </author>
      <author>
        <name>Dutta Roy, Abhilash</name>
      </author>
      <author>
        <name>Meng, Lin</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Seasonal Dependence of Atmospheric Responses to Extratropical Forcing</title>
      <link>https://escholarship.org/uc/item/3h3731xv</link>
      <description>Abstract Previous studies have shown that the extratropical-to-tropical teleconnection exhibits seasonal dependence, but the underlying mechanisms remain unclear. In this study, we use an idealized framework to explore the teleconnection and its underlying dynamics. We impose extratropical thermal warming in an aquaplanet model coupled to a mixed layered ocean under two idealized control climates: a perpetual winter-like climate and a perpetual summer-like climate. The extratropical-to-tropical teleconnection is more pronounced in the perpetual summer-like case, primarily due to differences in eddy momentum flux behavior. The unstable environment in the summer-like climate leads to vertically extended warming, which suppresses baroclinicity effectively and results in a subtropical eddy momentum flux convergence anomaly. This in turn drives adjustments in the Hadley cell. Moreover, the summer-like climatological Hadley cell is in a regime that responds effectively to anomalous...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3h3731xv</guid>
      <pubDate>Wed, 22 Oct 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chen, Yung-Jen</name>
      </author>
      <author>
        <name>Hwang, Yen-Ting</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>The Seasonal Cycles of Tropical Sea Surface Temperature from Earth’s Axial Tilt and Orbital Eccentricity</title>
      <link>https://escholarship.org/uc/item/3hx4m49g</link>
      <description>Abstract: 

We explore the relative roles of Earth’s axial tilt (“tilt effect”) and orbital eccentricity (“distance effect”) in generating the seasonal cycle of tropical sea surface temperature (SST), decomposing the two contributions using simulations of an Earth system model varying the eccentricity and longitude of perihelion. Tropical SST seasonality is largely explained by the annual contribution from tilt, but with significant contributions from the semiannual contribution from tilt and annual contribution from distance, especially in regions where the tilt annual contribution is relatively small. Precessional changes to tropical SST seasonality are readily explained by the distance annual component whose amplitude increases linearly with eccentricity and whose phase changes linearly with the longitude of perihelion, while the tilt contributions remain essentially unchanged. As such, the annual cycle contribution from distance can become significant at high eccentricity...</description>
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      <pubDate>Tue, 26 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Kong, Leah YL</name>
      </author>
    </item>
    <item>
      <title>Real-Time Partitioning of Diurnal Stem CO2 Efflux into Local Stem Respiration and Xylem Transport Processes</title>
      <link>https://escholarship.org/uc/item/06p7s99v</link>
      <description>The apparent respiratory quotient (ARQ) of tree stems, defined as the ratio of net stem CO2 efflux (ES_CO2) to net stem O2 influx (ES_O2), offers insights into the balance between local respiratory CO2 production and CO2 transported via the xylem. Traditional static chamber methods for measuring ARQ can introduce artifacts and obscure natural diurnal variations. Here, we employed an open flow-through stem chamber with ambient air coupled with cavity ring-down spectrometry, which uses the molecular properties of CO2 and O2 molecules to continuously measure ES_CO2, ES_O2, and ARQ, at the base of a California cherry tree (Prunus ilicifolia) during the 2024 growing season. Measurements across three stem chambers over 3–11-day periods revealed strong correlations between ES_CO2 and ES_O2 and mean ARQ values ranging from 1.3 to 2.9, far exceeding previous reports. Two distinct diurnal ARQ patterns were observed: daytime suppression with nighttime recovery, and a morning peak followed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/06p7s99v</guid>
      <pubDate>Tue, 26 Aug 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Oliveira, Regison</name>
      </author>
      <author>
        <name>Ajami, Parsa</name>
      </author>
      <author>
        <name>Knox, Ryan</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Koven, Charlie</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Gimenez, Bruno</name>
      </author>
      <author>
        <name>Spanner, Gustavo</name>
      </author>
      <author>
        <name>Warren, Jeffrey</name>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Tcherkez, Guillaume</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
    </item>
    <item>
      <title>Hyperspectral leaf reflectance of grasses varies with evolutionary lineage more than with site</title>
      <link>https://escholarship.org/uc/item/9wj5j03r</link>
      <description>Abstract  To predict ecological responses at broad environmental scales, grass species are commonly grouped into two broad functional types based on photosynthetic pathway. However, closely related species may have distinctive anatomical and physiological attributes that influence ecological responses, beyond those related to photosynthetic pathway alone. Hyperspectral leaf reflectance can provide an integrated measure of covarying leaf traits that may result from phylogenetic trait conservatism and/or environmental conditions. Understanding whether spectra‐trait relationships are lineage specific or reflect environmental variation across sites is necessary for using hyperspectral reflectance to predict plant responses to environmental changes across spatial scales. We measured hyperspectral leaf reflectance (400–2400 nm) and 12 structural, biochemical, and physiological leaf traits from five grass‐dominated sites spanning the Great Plains of North America. We assessed if variation...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9wj5j03r</guid>
      <pubDate>Tue, 22 Jul 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Slapikas, Ryan</name>
      </author>
      <author>
        <name>Ho, Che‐Ling</name>
      </author>
      <author>
        <name>Bayliss, Shannon LJ</name>
        <uri>https://orcid.org/0000-0002-3997-8343</uri>
      </author>
      <author>
        <name>Donnelly, Ryan C</name>
      </author>
      <author>
        <name>Abdullahi, Adam</name>
      </author>
      <author>
        <name>Helliker, Brent R</name>
      </author>
      <author>
        <name>Nippert, Jesse B</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Still, Christopher J</name>
      </author>
      <author>
        <name>Wedel, Emily R</name>
      </author>
      <author>
        <name>Griffith, Daniel M</name>
      </author>
    </item>
    <item>
      <title>Arctic sea-ice loss drives a strong regional atmospheric response over the North Pacific and North Atlantic on decadal scales</title>
      <link>https://escholarship.org/uc/item/6xq0g2dp</link>
      <description>Previous studies have suggested that Arctic sea-ice loss can have a profound influence on atmospheric circulation far away from the Arctic. However, there is little scientific consensus on the features of these remote responses, with the opposite impacts reported. Here we present a multi-model analysis of the decadal climate response to Arctic sea-ice loss using state-of-the-art energy conserving methodologies to isolate the impacts of sea-ice decline. We observe weakening of the Aleutian Low and development of a geopotential ridge in the North Pacific, associated with drier winter conditions over the southwest United States. Over the Atlantic, a negative NAO-like response drives wetter winter conditions across the western Mediterranean. These decadal-scale impacts substantially differ from reported centennial-scale responses to Arctic sea-ice loss simulated using non-energy conserving methodologies. Factors such as the timescale of the response and methodologies used to isolate...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6xq0g2dp</guid>
      <pubDate>Mon, 2 Jun 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Cvijanovic, Ivana</name>
      </author>
      <author>
        <name>Simon, Amelie</name>
      </author>
      <author>
        <name>Levine, Xavier</name>
      </author>
      <author>
        <name>White, Rachel</name>
      </author>
      <author>
        <name>Ortega, Pablo</name>
      </author>
      <author>
        <name>Donat, Markus</name>
      </author>
      <author>
        <name>Lucas, Donald D</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Seidenglanz, Anne</name>
      </author>
      <author>
        <name>Bojovic, Dragana</name>
      </author>
      <author>
        <name>Amaral, Arthur Ramos</name>
      </author>
      <author>
        <name>Lapin, Vladimir</name>
      </author>
      <author>
        <name>Doblas-Reyes, Francisco</name>
      </author>
      <author>
        <name>Petrova, Desislava</name>
      </author>
    </item>
    <item>
      <title>What Causes the Hemispheric Difference in the Asymmetry of the Temperature Annual Cycle?</title>
      <link>https://escholarship.org/uc/item/6hd177k2</link>
      <description>Previous studies have noted the asymmetry in the annual cycle of zonal mean surface air temperature, defined as the difference in the lengths of warming and cooling periods. Pronounced north-south hemispheric differences in this asymmetry, by up to 40&amp;nbsp;days, were attributed to the eccentricity of Earth's orbit. However, we propose that the dominant factor comes from the difference in the land-sea fraction between hemispheres, because the asymmetry is strongly influenced by the annually varying heat capacity and land-sea interactions. The oceanic temperature annual cycle generally features a longer cooling period than warming due to the seasonal variation in ocean mixed layer depth, and exhibits the opposite situation when there is seasonal sea ice. Land-sea interactions impact the zonal mean temperature annual cycle by resulting in an earlier winter trough of the downstream oceanic temperature and delaying the summer peak in west coasts.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6hd177k2</guid>
      <pubDate>Mon, 2 Jun 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Yang, Fucheng</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Wu, Zhaohua</name>
      </author>
    </item>
    <item>
      <title>Transformation of Unregulated Cannabis Cultivation Under Proposition 64</title>
      <link>https://escholarship.org/uc/item/1b2587z7</link>
      <description>Transformation of Unregulated Cannabis Cultivation Under Proposition 64</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1b2587z7</guid>
      <pubDate>Wed, 12 Mar 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Polson, Michael</name>
      </author>
      <author>
        <name>Laudati, Ann</name>
      </author>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>No evidence of canopy-scale leaf thermoregulation to cool leaves below air temperature across a range of forest ecosystems</title>
      <link>https://escholarship.org/uc/item/558973sk</link>
      <description>Understanding and predicting the relationship between leaf temperature (&lt;i&gt;T&lt;sub&gt;leaf&lt;/sub&gt;&lt;/i&gt;) and air temperature (&lt;i&gt;T&lt;sub&gt;air&lt;/sub&gt;&lt;/i&gt;) is essential for projecting responses to a warming climate, as studies suggest that many forests are near thermal thresholds for carbon uptake. Based on leaf measurements, the limited leaf homeothermy hypothesis argues that daytime &lt;i&gt;T&lt;sub&gt;leaf&lt;/sub&gt;&lt;/i&gt; is maintained near photosynthetic temperature optima and below damaging temperature thresholds. Specifically, leaves should cool below &lt;i&gt;T&lt;sub&gt;air&lt;/sub&gt;&lt;/i&gt; at higher temperatures (i.e., &amp;gt; ∼25-30°C) leading to slopes &amp;lt;1 in &lt;i&gt;T&lt;sub&gt;leaf&lt;/sub&gt;&lt;/i&gt;/&lt;i&gt;T&lt;sub&gt;air&lt;/sub&gt;&lt;/i&gt; relationships and substantial carbon uptake when leaves are cooler than air. This hypothesis implies that climate warming will be mitigated by a compensatory leaf cooling response. A key uncertainty is understanding whether such thermoregulatory behavior occurs in natural forest canopies. We present an unprecedented...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/558973sk</guid>
      <pubDate>Fri, 14 Feb 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Still, Christopher J</name>
      </author>
      <author>
        <name>Page, Gerald</name>
      </author>
      <author>
        <name>Rastogi, Bharat</name>
      </author>
      <author>
        <name>Griffith, Daniel M</name>
      </author>
      <author>
        <name>Aubrecht, Donald M</name>
      </author>
      <author>
        <name>Kim, Youngil</name>
      </author>
      <author>
        <name>Burns, Sean P</name>
      </author>
      <author>
        <name>Hanson, Chad V</name>
      </author>
      <author>
        <name>Kwon, Hyojung</name>
      </author>
      <author>
        <name>Hawkins, Linnia</name>
      </author>
      <author>
        <name>Meinzer, Frederick C</name>
      </author>
      <author>
        <name>Sevanto, Sanna</name>
      </author>
      <author>
        <name>Roberts, Dar</name>
        <uri>https://orcid.org/0000-0002-3555-4842</uri>
      </author>
      <author>
        <name>Goulden, Mike</name>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Detto, Matteo</name>
      </author>
      <author>
        <name>Helliker, Brent</name>
      </author>
      <author>
        <name>Richardson, Andrew D</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>A Later Onset of the Rainy Season in California</title>
      <link>https://escholarship.org/uc/item/9w67v8z9</link>
      <description>Californian hydroclimate is strongly seasonal and prone to severe water shortages. Recent changes in climate trends have induced shifts in seasonality, thus exacerbating droughts, wildfires, and adverse water shortage effects on the environment and economy. Previous studies have examined the timing of the seasonal cycle shifts mainly as temperature driven earlier onset of the spring season. In this paper, we address quantitative changes in the onset, amounts, and termination of the precipitation season over the past 6 decades, as well as the large-scale atmospheric circulation underpinning the seasonal cycle changes. We discover that the onset of the rainy season has been progressively delayed since the 1960s, and as a result the precipitation season has become shorter and sharper in California. The progressively later onset of the rainy season is shown to be related to the summer circulation pattern extending into autumn across the North Pacific, in particular, a delay in the...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9w67v8z9</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Lukovic, Jelena</name>
      </author>
      <author>
        <name>Chiang, John</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Blagojevic, Dragan</name>
      </author>
      <author>
        <name>Sekulic, Aleksandar</name>
      </author>
    </item>
    <item>
      <title>Role of precession on the transition seasons of the Asian monsoon</title>
      <link>https://escholarship.org/uc/item/997138qt</link>
      <description>While there have been many paleoclimate studies on the precessional control of climate, typically only the orbital phase where perihelion occurs close to the solstices has received attention. Here, we explore how precession affects the seasonal evolution of the Asian summer monsoon in the transitional seasons of boreal spring and autumn. With perihelion occurring in boreal spring, the Hadley circulation weakens over the northern Indian Ocean, linked to precession-enhanced sensible heating over the Tibetan Plateau. There is an early northward migration of the midlatitude westerly jet stream, and the advancement of the pre-monsoon along the Asian–Australian land bridge. The pre-monsoon response to precession may have had a major role in the early part of the last deglaciation, when perihelion last occurred during boreal spring. A weak continental summer monsoon and autumn aphelion during the early part of the last deglaciation led to a weak Pacific high over the east of coastal...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/997138qt</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Wu, Chi-Hua</name>
      </author>
      <author>
        <name>Lee, Shih-Yu</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Tsai, Pei-Chia</name>
      </author>
    </item>
    <item>
      <title>Orbit-induced changes in the seasonality of the Pacific cold-tongue region explained</title>
      <link>https://escholarship.org/uc/item/8fn784rx</link>
      <description>Simulations reveal that the annual temperature cycle in the Pacific cold-tongue region is influenced by the shape of Earth’s orbit, as well as by the planet’s axial tilt. Together, these influences drive remarkable changes in the cold tongue’s seasonality across a cycle of about 22,000 years.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8fn784rx</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Zhang, Honghai</name>
      </author>
    </item>
    <item>
      <title>A role for orbital eccentricity in Earth’s seasonal climate</title>
      <link>https://escholarship.org/uc/item/8dm0w7xr</link>
      <description>The seasonality of Earth’s climate is driven by two factors: the tilt of the Earth’s rotation axis relative to the plane of its orbit (hereafter the tilt effect), and the variation in the Earth–Sun distance due to the Earth’s elliptical orbit around the Sun (hereafter the distance effect). The seasonal insolation change between aphelion and perihelion is only ~ 7% of the annual mean and it is thus assumed that the distance effect is not relevant for the seasons. A recent modeling study by the authors and collaborators demonstrated however that the distance effect is not small for the Pacific cold tongue: it drives an annual cycle there that is dynamically distinct and ~ 1/3 of the amplitude from the known annual cycle arising from the tilt effect. The simulations also suggest that the influence of distance effect is significant and pervasive across several other regional climates, in both the tropics and extratropics. Preliminary work suggests that the distance effect works its...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8dm0w7xr</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Broccoli, Anthony J</name>
      </author>
    </item>
    <item>
      <title>Book review—Beyond Global Warming: How Numerical Models Revealed the Secrets of Climate Change</title>
      <link>https://escholarship.org/uc/item/7zj5c00x</link>
      <description>Book review—Beyond Global Warming: How Numerical Models Revealed the Secrets of Climate Change</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7zj5c00x</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>The Role of Southeast Asian Island Topography on Indo‐Pacific Climate and Silicate Weathering</title>
      <link>https://escholarship.org/uc/item/5sc2k0z7</link>
      <description>The geography of the Southeast Asian Islands (SEAI) has changed over the last 15 million years, as a result of tectonic processes contributing to both increased land area and high topography. The presence of the additional land area has been postulated to enhance convective rainfall, facilitating both increased silicate weathering and the development of the modern-day Walker circulation. Using an Earth System Model in conjunction with a climate-silicate weathering model, we argue instead for a significant role of SEAI topography for both effects. SEAI topography increases orographic rainfall over land, through intercepting moist Asian-Australian monsoon winds and enhancing land-sea breezes. Large-scale atmospheric uplift over the SEAI region increases by ∼14% as a consequence of increased rainfall over the SEAI and enhancement through dynamical ocean-atmosphere feedback. The atmospheric zonal overturning circulation over the Indo-Pacific increases modestly arising from dynamical...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5sc2k0z7</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Maffre, Pierre</name>
      </author>
      <author>
        <name>Swanson‐Hysell, Nicholas L</name>
      </author>
      <author>
        <name>Macdonald, Francis A</name>
        <uri>https://orcid.org/0000-0001-8416-4894</uri>
      </author>
    </item>
    <item>
      <title>Orbital eccentricity and Earth’s seasonal cycle</title>
      <link>https://escholarship.org/uc/item/4z79f096</link>
      <description>Orbital eccentricity and Earth’s seasonal cycle</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4z79f096</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Broccoli, Anthony J</name>
      </author>
    </item>
    <item>
      <title>The effect of Pliocene regional climate changes on silicate weathering: a potential amplifier of Pliocene-Pleistocene cooling</title>
      <link>https://escholarship.org/uc/item/4g89m414</link>
      <description>Abstract. The warmer early Pliocene climate featured changes to global sea surface temperature (SST) patterns, namely a reduction to the equator-pole gradient and to the east-west SST gradient in the tropical Pacific, the so-called “permanent El Niño”. Here we investigate the consequences of the SST changes to silicate weathering and thus to atmospheric CO2 on geological timescales. Different SST patterns than today imply regional modifications of the hydrological cycle that directly affects continental silicate weathering in particular over tropical “hotspots” of weathering such as the Maritime continent, thus leading to a “weatherability pattern effect”. We explore the impact of Pliocene SST changes on weathering using climate model and silicate weathering model simulations, and deduce CO2 and temperature at C cycle equilibrium between solid Earth degassing and silicate weathering. In general, we find large regional increases and decreases to weathering fluxes that largely cancel...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4g89m414</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Maffre, Pierre</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Swanson-Hysell, Nicholas L</name>
        <uri>https://orcid.org/0000-0003-3215-4648</uri>
      </author>
    </item>
    <item>
      <title>Two annual cycles of the Pacific cold tongue under orbital precession</title>
      <link>https://escholarship.org/uc/item/4f96w2q2</link>
      <description>The Pacific cold tongue annual cycle in sea surface temperature is presumed to be driven by Earth's axial tilt&lt;sup&gt;1-5&lt;/sup&gt; (tilt effect), and thus its phasing should be fixed relative to the calendar. However, its phase and amplitude change dramatically and consistently under various configurations of orbital precession in several Earth System models. Here, we show that the cold tongue possesses another annual cycle driven by the variation in Earth-Sun distance (distance effect) from orbital eccentricity. As the two cycles possess slightly different periodicities&lt;sup&gt;6&lt;/sup&gt;, their interference results in a complex evolution of the net seasonality over a precession cycle. The amplitude from the distance effect increases linearly with eccentricity and is comparable to the amplitude from the tilt effect for the largest eccentricity values over the last million years (e value approximately 0.05)&lt;sup&gt;7&lt;/sup&gt;. Mechanistically, the distance effect on the cold tongue arises through...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4f96w2q2</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Atwood, Alyssa R</name>
      </author>
      <author>
        <name>Vimont, Daniel J</name>
      </author>
      <author>
        <name>Nicknish, Paul A</name>
      </author>
      <author>
        <name>Roberts, William HG</name>
      </author>
      <author>
        <name>Tabor, Clay R</name>
      </author>
      <author>
        <name>Broccoli, Anthony J</name>
      </author>
    </item>
    <item>
      <title>Abrupt change in tropical Pacific climate mean state during the Little Ice Age</title>
      <link>https://escholarship.org/uc/item/3vv5g25m</link>
      <description>The mean state of the tropical Pacific ocean-atmosphere climate, in particular its east-west asymmetry, has profound consequences for regional climates and for the El Niño/Southern Oscillation variability. Here we present a new high-resolution paleohydrological record using the stable-hydrogen-isotopic composition of terrestrial-lipid biomarkers (δDwax) from a 1,400-year-old lake sedimentary sequence from northern Philippines. Results show a dramatic and abrupt increase in δDwax values around 1630 AD with sustained high values until around 1900 AD. We interpret this change as a shift to significantly drier conditions in the western tropical Pacific during the second half of the Little Ice Age as a result of a change in tropical Pacific mean state tied to zonal sea surface temperature (SST) gradients. Our findings highlight the prominent role of abrupt shifts in zonal SST gradients on multidecadal to multicentennial timescales in shaping the tropical Pacific hydrology of the last...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3vv5g25m</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Prohaska, Ana</name>
      </author>
      <author>
        <name>Seddon, Alistair WR</name>
      </author>
      <author>
        <name>Meese, Bernd</name>
      </author>
      <author>
        <name>Willis, Katherine J</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Sachse, Dirk</name>
      </author>
    </item>
    <item>
      <title>Author Correction: Split westerlies over Europe in the early Little Ice Age</title>
      <link>https://escholarship.org/uc/item/3sz1594d</link>
      <description>The original version of this Article contained an error in Fig. 3g, inwhich the age on theXaxis for the AtlanticMultidecadal Variability index recordwas incorrect. This has been corrected in both the PDF and HTML versions of the Article.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3sz1594d</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Hu, Hsun-Ming</name>
      </author>
      <author>
        <name>Shen, Chuan-Chou</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Trouet, Valerie</name>
      </author>
      <author>
        <name>Michel, Véronique</name>
      </author>
      <author>
        <name>Tsai, Hsien-Chen</name>
      </author>
      <author>
        <name>Valensi, Patricia</name>
      </author>
      <author>
        <name>Spötl, Christoph</name>
      </author>
      <author>
        <name>Starnini, Elisabetta</name>
      </author>
      <author>
        <name>Zunino, Marta</name>
      </author>
      <author>
        <name>Chien, Wei-Yi</name>
      </author>
      <author>
        <name>Sung, Wen-Hui</name>
      </author>
      <author>
        <name>Chien, Yu-Tang</name>
      </author>
      <author>
        <name>Chang, Ping</name>
      </author>
      <author>
        <name>Korty, Robert</name>
      </author>
    </item>
    <item>
      <title>Increased tropical South Pacific western boundary current transport over the past century</title>
      <link>https://escholarship.org/uc/item/336069n7</link>
      <description>The wind-driven meridional overturning circulation between the tropical and subtropical oceans is important for regulating decadal-scale temperature fluctuations in the Pacific Ocean and globally. An acceleration of the overturning circulation can act to reduce global surface temperature as ocean stores more heat. The equatorward low-latitude western boundary current represents a key component of the meridional circulation cell in the Pacific and a major source of water mass for the Equatorial Undercurrent, yet long-term observations of its transport are scarce. Here we demonstrate that the 15N/14N ratio recorded by Porites spp. corals in the western tropical South Pacific is sensitive to the exchanges of water masses driven by the western boundary transport. Using a 94-year coral record from the Solomon Sea, we report that the 15N/14N ratio declined as the global surface temperature rose. The record suggests that the South Pacific western boundary current has strengthened in...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/336069n7</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Chen, Wen-Hui</name>
      </author>
      <author>
        <name>Ren, Haojia</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Wang, You-Lin</name>
      </author>
      <author>
        <name>Cai-Li, Ren-Yi</name>
      </author>
      <author>
        <name>Chen, Yi-Chi</name>
      </author>
      <author>
        <name>Shen, Chuan-Chou</name>
      </author>
      <author>
        <name>Taylor, Frederick W</name>
      </author>
      <author>
        <name>DeCarlo, Thomas M</name>
      </author>
      <author>
        <name>Wu, Chau-Ron</name>
      </author>
      <author>
        <name>Mii, Horng-Sheng</name>
      </author>
      <author>
        <name>Wang, Xingchen Tony</name>
      </author>
    </item>
    <item>
      <title>Atmospheric River Representation in the Energy Exascale Earth System Model (E3SM) Version 1.0</title>
      <link>https://escholarship.org/uc/item/2zx7k06x</link>
      <description>Abstract. The Energy Exascale Earth System Model (E3SM) Project is an ongoing, state-of-the-science Earth system modeling, simulation, and prediction project developed by the U.S. Department of Energy (DOE). With an emphasis on supporting DOE's energy mission, understanding and quantifying how well the model simulates water cycle processes is of particular importance. Here, we evaluate E3SM version v1.0 for its ability to represent atmospheric rivers (ARs), which play significant roles in water vapor transport and precipitation. The characteristics and precipitation associated with global ARs in E3SM at standard resolution (1° × 1°) are compared to the Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA2). Global pattern of AR frequencies in E3SM show high degrees of correlation (&amp;gt;= 0.97) with MERRA2 and low mean absolute errors (&amp;lt; 1 %) annually, seasonally, and across different ensemble members. However, some large-scale condition biases exist...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2zx7k06x</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Kim, Sol</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
      <author>
        <name>Guan, Bin</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Regional tropical rainfall shifts under global warming: an energetic perspective</title>
      <link>https://escholarship.org/uc/item/2n38j1bc</link>
      <description>Abstract: 

               Future climate simulations feature pronounced spatial shifts in the structure of tropical rainfall. We apply a novel atmospheric energy flux analysis to diagnose late 21st century tropical rainfall shifts in a large ensemble of simulations of 21st century climate. The method reconstructs 2D spatial changes in rainfall based on horizontal shifts in the lines of zero meridional and zonal divergent energy flux, called the energy flux equator (EFE) and energy flux prime meridian (EFPM), respectively. Two main sources of future atmospheric energy flux changes, and hence rainfall shifts, are identified by the analysis: the high-latitude North Atlantic due to a weakened Atlantic Meridional Overturning Circulation that shifts tropical rainfall southwards over the greater Tropical Atlantic sector and eastern Pacific; and the eastern tropical Pacific due to a permanent El-Niño-like response that produces zonal shifts over the Maritime Continent and South America....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2n38j1bc</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Nicknish, Paul A</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Hu, Aixue</name>
      </author>
      <author>
        <name>Boos, William R</name>
        <uri>https://orcid.org/0000-0001-9076-3551</uri>
      </author>
    </item>
    <item>
      <title>Author Correction: Split westerlies over Europe in the early Little Ice Age</title>
      <link>https://escholarship.org/uc/item/1wp9s9d1</link>
      <description>The original version of this Article contained an error in Fig. 3, in which the uncertainty of the Atlantic Multidecadal Variability index was included as an orange trend line labelled with the letter ‘g’. This index however was found to be not linked to the findings of this study and has been removed. This has been corrected in both the PDF and HTML versions of the Article. The original version of this Article contained an error in the caption of Figure 3, which incorrectly read ‘g Orange: Atlantic Multidecadal Variability index&lt;sup&gt;55&lt;/sup&gt;. Black: total solar irradiance12.’ The correct version replaces this sentence with ‘g Total solar irradiance&lt;sup&gt;12&lt;/sup&gt;.’. This has been corrected in both the PDF and HTML versions of the Article. The original version of this Article contained an error in the Results section, which incorrectly read ‘Fromthe 1400 s C.E. onwards, sea ice extent decreased significantly (Fig. 3b, c) due to an intrusion of warm Atlantic Water into the North...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1wp9s9d1</guid>
      <pubDate>Thu, 9 Jan 2025 00:00:00 +0000</pubDate>
      <author>
        <name>Hu, Hsun-Ming</name>
      </author>
      <author>
        <name>Shen, Chuan-Chou</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Trouet, Valerie</name>
      </author>
      <author>
        <name>Michel, Véronique</name>
      </author>
      <author>
        <name>Tsai, Hsien-Chen</name>
      </author>
      <author>
        <name>Valensi, Patricia</name>
      </author>
      <author>
        <name>Spötl, Christoph</name>
      </author>
      <author>
        <name>Starnini, Elisabetta</name>
      </author>
      <author>
        <name>Zunino, Marta</name>
      </author>
      <author>
        <name>Chien, Wei-Yi</name>
      </author>
      <author>
        <name>Sung, Wen-Hui</name>
      </author>
      <author>
        <name>Chien, Yu-Tang</name>
      </author>
      <author>
        <name>Chang, Ping</name>
      </author>
      <author>
        <name>Korty, Robert</name>
      </author>
    </item>
    <item>
      <title>Unexplained high and persistent methyl bromide emissions in China</title>
      <link>https://escholarship.org/uc/item/0hq0w16p</link>
      <description>Methyl bromide (CH3Br) is an important ozone-depleting substance whose use is regulated under the Montreal Protocol. Quantifying emissions on the national scale is required to assess compliance with the Montreal Protocol and thereby ensure the timely recovery of the ozone layer. However, the spatial-temporal patterns of China’s national CH3Br emissions remain unclear. Here we estimate the national emissions of CH3Br in China during 2011−2020 using atmospheric observations at 10 sites across China combined with an inversion technique (top-down) and compare those with an updated inventory of identified emission sources (bottom-up). Measured CH3Br mole fractions are enhanced well above the background mole fractions, especially at sites in eastern China. Top-down emission estimates exceed bottom-up estimates by 5.5 ± 1.4 gigagrams per year, with the largest fraction (60%) of observationally derived CH3Br emissions arising from underestimated or&amp;nbsp;unidentified emissions sources....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0hq0w16p</guid>
      <pubDate>Sat, 23 Nov 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Hu, Xiaoyi</name>
      </author>
      <author>
        <name>Yao, Bo</name>
      </author>
      <author>
        <name>Mühle, Jens</name>
      </author>
      <author>
        <name>Rhew, Robert C</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
      <author>
        <name>Fraser, Paul J</name>
      </author>
      <author>
        <name>O’Doherty, Simon</name>
      </author>
      <author>
        <name>Prinn, Ronald G</name>
      </author>
      <author>
        <name>Fang, Xuekun</name>
      </author>
    </item>
    <item>
      <title>Beyond the hype: Digital transformations in global land, housing, and property</title>
      <link>https://escholarship.org/uc/item/1sc1v1tk</link>
      <description>This theme issue investigates how 21st-century digital innovations are changing the nature and value of land, housing, and property. Contributors bring together an array of cases to understand how digitization is remaking land and housing on a global scale and, in turn, how existing property relations structure digital transformations in particular geographies. In this introduction to the theme issue, we outline how hype can be used as an analytical entry point to characterize the collection’s contribution, demonstrating how hype elides unequal relations of land and labor while stoking speculation in immovable property, even as it creates new markets for less tangible assets—whether rental data or virtual plots—that usher in new global connections and familiar market dynamics.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1sc1v1tk</guid>
      <pubDate>Wed, 9 Oct 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Faxon, Hilary Oliva</name>
      </author>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
      <author>
        <name>Wainwright, Thomas</name>
      </author>
    </item>
    <item>
      <title>Grass Evolutionary Lineages Can Be Identified Using Hyperspectral Leaf Reflectance</title>
      <link>https://escholarship.org/uc/item/2503g86v</link>
      <description>Abstract  Hyperspectral remote sensing has the potential to map numerous attributes of the Earth’s surface, including spatial patterns of biological diversity. Grasslands are one of the largest biomes on Earth. Accurate mapping of grassland biodiversity relies on spectral discrimination of endmembers of species or plant functional types. We focused on spectral separation of grass lineages that dominate global grassy biomes: Andropogoneae (C 4 ), Chloridoideae (C 4 ), and Pooideae (C 3 ). We examined leaf reflectance spectra (350–2,500&amp;nbsp;nm) from 43 grass species representing these grass lineages from four representative grassland sites in the Great Plains region of North America. We assessed the utility of leaf reflectance data for classification of grass species into three major lineages and by collection site. Classifications had very high accuracy (94%) that were robust to site differences in species and environment. We also show an information loss using multispectral sensors,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2503g86v</guid>
      <pubDate>Mon, 7 Oct 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Slapikas, Ryan</name>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Donnelly, Ryan C</name>
      </author>
      <author>
        <name>Ho, Che‐Ling</name>
      </author>
      <author>
        <name>Nippert, Jesse B</name>
      </author>
      <author>
        <name>Helliker, Brent R</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Still, Christopher J</name>
      </author>
      <author>
        <name>Griffith, Daniel M</name>
      </author>
    </item>
    <item>
      <title>Hysteresis area at the canopy level during and after a drought event in the Central Amazon</title>
      <link>https://escholarship.org/uc/item/8pp319zj</link>
      <description>Understanding forest water limitation during droughts within a warming climate is essential for accurate predictions of forest-climate interactions. In hyperdiverse ecosystems like the Amazon forest, the mechanisms shaping hysteresis patterns in transpiration relative to environmental factors are not well understood. From this perspective, we investigated these dynamics by conducting in situ leaf-level measurements throughout and after the 2015 El Niño-Southern Oscillation (ENSO) drought. Our findings indicate a substantial increase in the hysteresis area (Harea ) among transpiration (E), vapor pressure deficit (VPD), and stomatal conductance (gs ) at canopy level during the ENSO peak, attributed to both temporal lag and differences in magnitude between gs and VPD peaks. Specifically, the canopy species Pouteria anomala exhibited an increased Harea , due to earlier maximum gs rates leading to a greater temporal lag with VPD compared to the post-drought period. Additionally, leaf...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8pp319zj</guid>
      <pubDate>Tue, 24 Sep 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Souza, Daisy C</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>de Jesus Sampaio-Filho, Israel</name>
      </author>
      <author>
        <name>Araújo, Alessandro C</name>
      </author>
      <author>
        <name>Lima, Adriano JN</name>
      </author>
      <author>
        <name>Fontes, Clarissa G</name>
      </author>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Meng, Lin</name>
      </author>
      <author>
        <name>Pastorello, Gilberto</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>What Makes a Natural Harbor?Naturalizing Port Development along the Gulf of Kutch, Western India</title>
      <link>https://escholarship.org/uc/item/5bm6p73h</link>
      <description>Abstract: 

               The Mundra Port on the Gulf of Kutch in western India is one of India's largest port projects today. This article takes the port-circulated narrative of the coast being a natural harbor as its starting point, to show how fresh water was central to official maritime projects until the early postcolonial period. Conserving mangroves and freshwater creeks was not antithetical to maritime ports but part of the same administrative project. Political and infrastructural shifts from the river to the tide naturalized the erasure of coastal fresh water and transformed the coast into a singularly tidal space, creating the conditions for the development of a large-scale, high-technology shipping port.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5bm6p73h</guid>
      <pubDate>Thu, 12 Sep 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Anusha, Chandana</name>
      </author>
    </item>
    <item>
      <title>Future climate doubles the risk of hydraulic failure in a wet tropical forest</title>
      <link>https://escholarship.org/uc/item/4rn086b0</link>
      <description>Future climate presents conflicting implications for forest biomass. We evaluate how plant hydraulic traits, elevated CO&lt;sub&gt;2&lt;/sub&gt; levels, warming, and changes in precipitation affect forest primary productivity, evapotranspiration, and the risk of hydraulic failure. We used a dynamic vegetation model with plant hydrodynamics (FATES-HYDRO) to simulate the stand-level responses to future climate changes in a wet tropical forest in Barro Colorado Island, Panama. We calibrated the model by selecting plant trait assemblages that performed well against observations. These assemblages were run with temperature and precipitation changes for two greenhouse gas emission scenarios (2086-2100: SSP2-45, SSP5-85) and two CO&lt;sub&gt;2&lt;/sub&gt; levels (contemporary, anticipated). The risk of hydraulic failure is projected to increase from a contemporary rate of 5.7% to 10.1-11.3% under future climate scenarios, and, crucially, elevated CO&lt;sub&gt;2&lt;/sub&gt; provided only slight amelioration. By contrast,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4rn086b0</guid>
      <pubDate>Wed, 11 Sep 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Robbins, Zachary</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
      <author>
        <name>Chitra‐Tarak, Rutuja</name>
      </author>
      <author>
        <name>Christoffersen, Bradley</name>
      </author>
      <author>
        <name>Dickman, L Turin</name>
      </author>
      <author>
        <name>Fisher, Rosie</name>
      </author>
      <author>
        <name>Jonko, Alex</name>
      </author>
      <author>
        <name>Knox, Ryan</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Koven, Charles</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Kueppers, Lara</name>
        <uri>https://orcid.org/0000-0002-8134-3579</uri>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Xu, Chonggang</name>
        <uri>https://orcid.org/0000-0002-0937-5744</uri>
      </author>
    </item>
    <item>
      <title>Proptech and the private rental sector: New forms of extraction at the intersection of rental properties and platform rentierisation</title>
      <link>https://escholarship.org/uc/item/65h334f2</link>
      <description>Private renting increasingly comprises a complex ecosystem of actors who assemble housing within the market, and collect rental income and data from tenants, and data on the material assets themselves. Our analysis – at the intersection of rentier and platform capitalism – focuses on landed (material real estate) and technological (digital infrastructure and data) property in Australia’s private rental system. Drawing out relationships between the various actors – landlords, rental property managers and real estate agencies, software developers and providers, property developers and investors – and both their properties and their uses of Proptech (property technology), we show how housing and technology are being leveraged for profit in new ways. In Australia, landed property retains its precedence for established (individual and institutional) landlords, whose interest in Proptech relates to enhancing or value-adding to rental housing assets. For Proptech and institutional real...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/65h334f2</guid>
      <pubDate>Thu, 15 Aug 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Rogers, Dallas</name>
      </author>
      <author>
        <name>Maalsen, Sophia</name>
      </author>
      <author>
        <name>Wolifson, Peta</name>
      </author>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
    </item>
    <item>
      <title>A History of North American Rangelands</title>
      <link>https://escholarship.org/uc/item/89p67161</link>
      <description>North America's diverse grassland, savanna, steppe and desert ecosystems evolved in the absence of domesticated livestock. The arrival of cattle, sheep, goats, pigs and horses after 1492 transformed many ecosystems while enabling European soldiers, missionaries and settlers to conquer the continent. The decimation of indige-nous populations by warfare, disease and economic dependency further transformed rangelands by removing Native management practices, especially the use of fire. The history of rangelands since then has been one of recursive efforts to commodify and territorialize rangeland resources-including wildlife, grass, soil fertility and the land itself-for market production and exchange. Many former rangelands have been lost altogether, by conversion to forest cover (due to fire suppression) or to agricultural uses (especially in the Great Plains), and invasive exotic plant species have radically altered large areas of rangelands in California, the Great Basin, and...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/89p67161</guid>
      <pubDate>Wed, 14 Aug 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>From Experimenting with Property to Experimenting on Place: A Rejoinder to Migozzi and Safransky</title>
      <link>https://escholarship.org/uc/item/5cb803qj</link>
      <description>This rejoinder engages with the commentaries on my article on ‘Digital experiments with landed property’ from Julien Migozzi and Sara Safransky. In my response, I share my reflections on the valuable provocations and interrelated themes offered in these generous commentaries. First, I argue that an especially distinctive aspect of digital experiments with landed property is the volumetric property relations they are generating. Second, I attend to subjectivities cultivated within and against digitised property relations, and how they relate to structures of power. Third, I extend my thinking on the glitchiness and fallibility associated with processes of experimentation.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5cb803qj</guid>
      <pubDate>Thu, 6 Jun 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
    </item>
    <item>
      <title>Digital Experiments with Landed Property: Robots, Race, and Rent</title>
      <link>https://escholarship.org/uc/item/3nr3378p</link>
      <description>A wide range of digital innovations has changed property relations globally over the past fifteen years. What are we to make of these digital experiments with landed property? I argue we should not mistake their technological novelty for a break with the geographic and historical specificities of property relations. The yoking of property to modernity and civilization makes technological progress a fundamental part of how relationships to land are constituted and reconstituted, and in whose interests, throughout global capitalism. In this article, I situate 21st century housing market technologies within sedimented relations of landed property in the United States, showing the history of property innovation in the United States is also one of racialized wealth accumulation and dispossession. I interpret current anxieties about ‘robot landlords’ as anxieties about how the shifting landscape of property ownership appears to threaten the economic benefits associated with racial dominance.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3nr3378p</guid>
      <pubDate>Thu, 6 Jun 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
    </item>
    <item>
      <title>Housing Movements and Care: Rethinking the Political Imaginaries of Housing</title>
      <link>https://escholarship.org/uc/item/6zn7q66n</link>
      <description>Care is a practice and form of labour making human survival and flourishing possible. This Symposium explores the place and work of care within housing movements, asking how care operates as a politics, an ethics, and a set of practices through which tenants survive—and ultimately seek to transform—the structural violence of capitalist housing systems. Situated in US cities with abiding associations with Blackness and indigeneity, papers in the Symposium examine housing movements that take care as the starting point. As we discuss in this introduction to the Symposium, in such movements, care operates as connective tissue across households and modes of difference; challenges relations of racial capitalism and settler colonialism that underlie dominant understandings of who deserves and can demand care; and drives calls for public care and experiments with non-propertised forms of ownership. Housing systems are care infrastructures, making housing movements a vital place for care work.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6zn7q66n</guid>
      <pubDate>Thu, 9 May 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
      <author>
        <name>Power, Emma R</name>
      </author>
      <author>
        <name>Card, Kenton</name>
      </author>
    </item>
    <item>
      <title>Enriched East Asian oxygen isotope of precipitation indicates reduced summer seasonality in regional climate and westerlies</title>
      <link>https://escholarship.org/uc/item/53w9146w</link>
      <description>Speleothem oxygen isotope records over East Asia reveal apparently large and rapid paleoclimate changes over the last several hundred thousand years. However, what the isotopic variation actually represent in terms of the regional climate and circulation is debated. We present an answer that emerges from an analysis of the interannual variation in amount-weighted annual δ&lt;sup&gt;18&lt;/sup&gt;O of precipitation over East Asia as simulated by an isotope-enabled model constrained by large-scale atmospheric reanalysis fields. &lt;sup&gt;18&lt;/sup&gt;O-enriched years have reduced summer seasonality both in terms of precipitation isotopes and in the large-scale circulation. Changes occur between June and October, where the δ&lt;sup&gt;18&lt;/sup&gt;O of precipitation (δ&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;p&lt;/sub&gt;) transitions from the isotopically heavier winter to the lighter summer regime. For &lt;sup&gt;18&lt;/sup&gt;O-enriched years, this transition is less pronounced. Variations in precipitation amount alone are insufficient to explain the...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/53w9146w</guid>
      <pubDate>Mon, 8 Apr 2024 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Herman, Michael J</name>
      </author>
      <author>
        <name>Yoshimura, Kei</name>
      </author>
      <author>
        <name>Fung, Inez Y</name>
        <uri>https://orcid.org/0000-0003-4106-9875</uri>
      </author>
    </item>
    <item>
      <title>The effect of the Pliocene temperature pattern on silicate weathering and Pliocene–Pleistocene cooling</title>
      <link>https://escholarship.org/uc/item/2bk5j3zn</link>
      <description>The warmer early Pliocene climate featured changes to global sea surface temperature (SST) patterns, namely a reduction in the Equator-pole gradient and the east-west SST gradient in the tropical Pacific, the so-called "permanent El Niño". Here we investigate the consequences of the SST changes to silicate weathering and thus to atmospheric CO2 on geological timescales. Different SST patterns than today imply regional modifications of the hydrological cycle that directly affect continental silicate weathering in particular over tropical "hotspots"of weathering, such as the Maritime Continent, thus leading to a "weatherability pattern effect". We explore the impact of Pliocene-like SST changes on weathering using climate model and silicate weathering model simulations, and we deduce CO2 and temperature at carbon cycle equilibrium between solid Earth degassing and silicate weathering. In general, we find large regional increases and decreases in weathering fluxes, and the net effect...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2bk5j3zn</guid>
      <pubDate>Fri, 8 Dec 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Maffre, Pierre</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Swanson-Hysell, Nicholas L</name>
        <uri>https://orcid.org/0000-0003-3215-4648</uri>
      </author>
    </item>
    <item>
      <title>A Near Four-Decade Time Series Shows the Hawaiian Islands Have Been Browning Since the 1980s</title>
      <link>https://escholarship.org/uc/item/9xh693c8</link>
      <description>The Hawaiian Islands have been identified as a global biodiversity hotspot. We examine the Normalized Difference Vegetation Index (NDVI) using Climate Data Records products (0.05 × 0.05°) to identify significant differences in NDVI between neutral El Niño-Southern Oscillation years (1984, 2019) and significant long-term changes over the entire time series (1982–2019) for the Hawaiian Islands and six land cover classes. Overall, there has been a significant decline in NDVI (i.e., browning) across the Hawaiian Islands from 1982 to 2019 with the islands of Lāna’i and Hawai’i experiencing the greatest decreases in NDVI (≥44%). All land cover classes significantly decreased in NDVI for most months, especially during the wet season month of March. Native vegetation cover across all islands also experienced significant declines in NDVI, with the leeward, southwestern side of the island of Hawai’i experiencing the greatest declines. The long-term trends in the annual total precipitation...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9xh693c8</guid>
      <pubDate>Thu, 7 Dec 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Madson, Austin</name>
      </author>
      <author>
        <name>Dimson, Monica</name>
      </author>
      <author>
        <name>Fortini, Lucas Berio</name>
      </author>
      <author>
        <name>Kawelo, Kapua</name>
      </author>
      <author>
        <name>Ticktin, Tamara</name>
      </author>
      <author>
        <name>Keir, Matt</name>
      </author>
      <author>
        <name>Dong, Chunyu</name>
      </author>
      <author>
        <name>Ma, Zhimin</name>
      </author>
      <author>
        <name>Beilman, David W</name>
      </author>
      <author>
        <name>Kay, Kelly</name>
      </author>
      <author>
        <name>Ocón, Jonathan Pando</name>
      </author>
      <author>
        <name>Gallerani, Erica</name>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Gillespie, Thomas W</name>
      </author>
    </item>
    <item>
      <title>Understanding farmer knowledge of soil and soil management: a case study of 13 organic farms in an agricultural landscape of northern California</title>
      <link>https://escholarship.org/uc/item/679294sf</link>
      <description>While it is recognized that farming alternatively is inherently knowledge intensive, in the United States, farmer knowledge has been widely overlooked and under-documented within the scientific literature. Farmer knowledge of soil in particular is understudied in the US, especially given that healthy soils have been identified as the basis for resilient agriculture. Applying an exploratory, case study approach, we interviewed 13 organic farmers based in Yolo County, California to understand how organic farmers in this region acquire knowledge about their soils, to document what organic farmers in this region know about their soils, and to share key management practices organic farmers use to build soil health in the region. We found the organic farmers in this study acquire knowledge about their farming systems primarily through direct observation, personal experience, experimentation, and inherited wisdom. To evaluate soil health, farmers in this study cited using a range of...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/679294sf</guid>
      <pubDate>Wed, 8 Nov 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Klein, Ansel Olive</name>
      </author>
      <author>
        <name>Carlisle, Liz</name>
      </author>
      <author>
        <name>Lloyd, Margaret G</name>
      </author>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
      <author>
        <name>Bowles, Timothy M</name>
      </author>
    </item>
    <item>
      <title>Case Studies of Forest Windthrows and Mesoscale Convective Systems in Amazonia</title>
      <link>https://escholarship.org/uc/item/1c5902q3</link>
      <description>Abstract This study identifies 38 cases of windthrows in the Amazonia to explore the relationship between windthrows and the characteristics (storm passing time, cloud top temperature, and maximum precipitation) of mesoscale convective systems (MCSs) that produced them. Most of windthrow cases in this study occurred in August and September. The storm passing time is positively correlated with the size of windthrows. MCSs with colder cloud top temperature (with a mean at 206&amp;nbsp;K)—indicating deeper convection—resulted in large windthrows, while those with warm cloud top (with a mean above 230&amp;nbsp;K) resulted in relatively small windthrows except for windthrows in the western Amazonia. No significant relationship is found between maximum precipitation intensity and the area of windthrows.
Plain Language Summary Fan‐shaped dead forest patches were found over the entire Amazonia. These patches affect the role the Amazon forests played in the world's carbon cycle. Scientists found...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1c5902q3</guid>
      <pubDate>Fri, 6 Oct 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Negrón‐Juárez, Robinson I</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Review of Black Ranching Frontiers: African Cattle Herders of the Atlantic World, 1500-1900 by Andrew Sluyter</title>
      <link>https://escholarship.org/uc/item/8mg4s3z6</link>
      <description>Review of Black Ranching Frontiers: African Cattle Herders of the Atlantic World, 1500-1900 by Andrew Sluyter</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8mg4s3z6</guid>
      <pubDate>Wed, 27 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>A machine learning approach targeting parameter estimation for plant functional type coexistence modeling using ELM-FATES (v2.0)</title>
      <link>https://escholarship.org/uc/item/7734f0ps</link>
      <description>Abstract. Tropical forest dynamics play a crucial role in the global carbon, water, and energy cycles. However, realistically simulating the dynamics of competition and coexistence between different plant functional types (PFTs) in tropical forests remains a significant challenge. This study aims to improve the modeling of PFT coexistence in the Functionally Assembled Terrestrial Ecosystem Simulator (FATES), a vegetation demography model implemented in the Energy Exascale Earth System Model (E3SM) land model (ELM), ELM-FATES. Specifically, we explore (1)&amp;nbsp;whether plant trait relationships established from field measurements can constrain ELM-FATES simulations and (2)&amp;nbsp;whether machine learning (ML)-based surrogate models can emulate the complex ELM-FATES model and optimize parameter selections to improve PFT coexistence modeling. We conducted three ensembles of ELM-FATES experiments at a tropical forest site near Manaus, Brazil. By comparing the ensemble experiments without...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7734f0ps</guid>
      <pubDate>Wed, 27 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Li, Lingcheng</name>
      </author>
      <author>
        <name>Fang, Yilin</name>
      </author>
      <author>
        <name>Zheng, Zhonghua</name>
      </author>
      <author>
        <name>Shi, Mingjie</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>McDowell, Nate G</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
    </item>
    <item>
      <title>The Woolly West: Colorado's Hidden History of Sheepscapes</title>
      <link>https://escholarship.org/uc/item/2k27f0wf</link>
      <description>The Woolly West: Colorado's Hidden History of Sheepscapes</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2k27f0wf</guid>
      <pubDate>Wed, 27 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>Guadalupe Mountains National Park: An Environmental History of the Southwest Borderlands. By Jeffrey P. Shepherd. Amherst: University of Massachusetts Press, 2019. xii +227 pp. Illustrations, maps, notes, and index. Paper $29.95.</title>
      <link>https://escholarship.org/uc/item/2jt8k1sw</link>
      <description>Guadalupe Mountains National Park: An Environmental History of the Southwest Borderlands. By Jeffrey P. Shepherd. Amherst: University of Massachusetts Press, 2019. xii +227 pp. Illustrations, maps, notes, and index. Paper $29.95.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2jt8k1sw</guid>
      <pubDate>Wed, 27 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>Review: The Blue and the Green: A Cultural Ecological History of an Arizona Ranching Community by Jack Stauder</title>
      <link>https://escholarship.org/uc/item/2c58108t</link>
      <description>Review: The Blue and the Green: A Cultural Ecological History of an Arizona Ranching Community by Jack Stauder</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2c58108t</guid>
      <pubDate>Wed, 27 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Sayre, Nathan F</name>
        <uri>https://orcid.org/0000-0002-9243-2219</uri>
      </author>
    </item>
    <item>
      <title>Deglacial temperature history of West Antarctica</title>
      <link>https://escholarship.org/uc/item/8472v5f9</link>
      <description>The most recent glacial to interglacial transition constitutes a remarkable natural experiment for learning how Earth's climate responds to various forcings, including a rise in atmospheric CO&lt;sub&gt;2&lt;/sub&gt; This transition has left a direct thermal remnant in the polar ice sheets, where the exceptional purity and continual accumulation of ice permit analyses not possible in other settings. For Antarctica, the deglacial warming has previously been constrained only by the water isotopic composition in ice cores, without an absolute thermometric assessment of the isotopes' sensitivity to temperature. To overcome this limitation, we measured temperatures in a deep borehole and analyzed them together with ice-core data to reconstruct the surface temperature history of West Antarctica. The deglacial warming was [Formula: see text]C, approximately two to three times the global average, in agreement with theoretical expectations for Antarctic amplification of planetary temperature changes....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8472v5f9</guid>
      <pubDate>Mon, 18 Sep 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Cuffey, Kurt M</name>
      </author>
      <author>
        <name>Clow, Gary D</name>
      </author>
      <author>
        <name>Steig, Eric J</name>
      </author>
      <author>
        <name>Buizert, Christo</name>
      </author>
      <author>
        <name>Fudge, TJ</name>
      </author>
      <author>
        <name>Koutnik, Michelle</name>
      </author>
      <author>
        <name>Waddington, Edwin D</name>
      </author>
      <author>
        <name>Alley, Richard B</name>
      </author>
      <author>
        <name>Severinghaus, Jeffrey P</name>
        <uri>https://orcid.org/0000-0001-8883-3119</uri>
      </author>
    </item>
    <item>
      <title>Sensitivity of Optical Satellites to Estimate Windthrow Tree-Mortality in a Central Amazon Forest</title>
      <link>https://escholarship.org/uc/item/80v2g9gc</link>
      <description>Windthrow (i.e., trees broken and uprooted by wind) is a major natural disturbance in Amazon forests. Images from medium-resolution optical satellites combined with extensive field data have allowed researchers to assess patterns of windthrow tree-mortality and to monitor forest recovery over decades of succession in different regions. Although satellites with high spatial-resolution have become available in the last decade, they have not yet been employed for the quantification of windthrow tree-mortality. Here, we address how increasing the spatial resolution of satellites affects plot-to-landscape estimates of windthrow tree-mortality. We combined forest inventory data with Landsat 8 (30 m pixel), Sentinel 2 (10 m), and WorldView 2 (2 m) imagery over an old-growth forest in the Central Amazon that was disturbed by a single windthrow event in November 2015. Remote sensing estimates of windthrow tree-mortality were produced from Spectral Mixture Analysis and evaluated with forest...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/80v2g9gc</guid>
      <pubDate>Wed, 16 Aug 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Emmert, Luciano</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson Isaac</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Quintin</name>
      </author>
      <author>
        <name>dos Santos, Joaquim</name>
      </author>
      <author>
        <name>Lima, Adriano José Nogueira</name>
      </author>
      <author>
        <name>Trumbore, Susan</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
      <author>
        <name>Marra, Daniel Magnabosco</name>
      </author>
    </item>
    <item>
      <title>Controls on the size distributions of shallow landslides</title>
      <link>https://escholarship.org/uc/item/0kt093hc</link>
      <description>Rainfall-triggered shallow landslides are destructive hazards and play an important role in landscape processes. A theory explaining the size distributions of such features remains elusive. Prior work connects size distributions to topography, but field-mapped inventories reveal pronounced similarities in the form, mode, and spread of distributions from diverse landscapes. We analyze nearly identical distributions occurring in the Oregon Coast Range and the English Lake District, two regions of strikingly different topography, lithology, and vegetation. Similarity in minimum sizes at these sites is partly explained by theory that accounts for the interplay of mechanical soil strength controls resisting failure. Maximum sizes, however, are not explained by current theory. We develop a generalized framework to account for the entire size distribution by unifying a mechanistic slope stability model with a flexible spatial-statistical description for the variability of hillslope strength....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0kt093hc</guid>
      <pubDate>Sat, 17 Jun 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Bellugi, Dino G</name>
      </author>
      <author>
        <name>Milledge, David G</name>
      </author>
      <author>
        <name>Cuffey, Kurt M</name>
      </author>
      <author>
        <name>Dietrich, William E</name>
      </author>
      <author>
        <name>Larsen, Laurel G</name>
      </author>
    </item>
    <item>
      <title>Windthrow characteristics and their regional association with rainfall, soil, and surface elevation in the Amazon</title>
      <link>https://escholarship.org/uc/item/1kf448qf</link>
      <description>Windthrows (trees uprooted and broken by winds) are common across the Amazon. They range in size from single trees to large gaps that lead to changes in forest dynamics, composition, structure, and carbon balance. Yet, the current understanding of the spatial variability of windthrows is limited. By integrating remote sensing data and geospatial analysis, we present the first study to examine the occurrence, area, and direction of windthrows and the control that environmental variables exert on them across the whole Amazon. Windthrows are more frequent and larger in the northwestern Amazon (Peru and Colombia), with the central Amazon (Brazil) being another hot spot of windthrows. The predominant direction of windthrows is westward. Rainfall, surface elevation, and soil characteristics explain the variability (20%–50%) of windthrows but their effects vary regionally. A better understanding of the spatial dynamics of windthrows will improve understanding of the functioning of Amazon...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1kf448qf</guid>
      <pubDate>Tue, 23 May 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
      <author>
        <name>Magnabosco-Marra, Daniel</name>
      </author>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Urquiza-Muñoz, Jose David</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Seasonal temperatures in West Antarctica during the Holocene</title>
      <link>https://escholarship.org/uc/item/36r1p98h</link>
      <description>The recovery of long-term climate proxy records with seasonal resolution is rare because of natural smoothing processes, discontinuities and limitations in measurement resolution. Yet insolation forcing, a primary driver of multimillennial-scale climate change, acts through seasonal variations with direct impacts on seasonal climate1. Whether the sensitivity of seasonal climate to insolation matches theoretical predictions has not been assessed over long timescales. Here, we analyse a continuous record of water-isotope ratios from the West Antarctic Ice Sheet Divide ice core to reveal summer and winter temperature changes through the last 11,000 years. Summer temperatures in West Antarctica increased through the early-to-mid-Holocene, reached a peak 4,100 years ago and then decreased to the present. Climate model simulations show that these variations primarily reflect changes in maximum summer insolation, confirming the general connection between seasonal insolation and warming...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/36r1p98h</guid>
      <pubDate>Thu, 11 May 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Jones, Tyler R</name>
      </author>
      <author>
        <name>Cuffey, Kurt M</name>
      </author>
      <author>
        <name>Roberts, William HG</name>
      </author>
      <author>
        <name>Markle, Bradley R</name>
      </author>
      <author>
        <name>Steig, Eric J</name>
      </author>
      <author>
        <name>Stevens, C Max</name>
      </author>
      <author>
        <name>Valdes, Paul J</name>
      </author>
      <author>
        <name>Fudge, TJ</name>
      </author>
      <author>
        <name>Sigl, Michael</name>
      </author>
      <author>
        <name>Hughes, Abigail G</name>
      </author>
      <author>
        <name>Morris, Valerie</name>
      </author>
      <author>
        <name>Vaughn, Bruce H</name>
      </author>
      <author>
        <name>Garland, Joshua</name>
      </author>
      <author>
        <name>Vinther, Bo M</name>
      </author>
      <author>
        <name>Rozmiarek, Kevin S</name>
      </author>
      <author>
        <name>Brashear, Chloe A</name>
      </author>
      <author>
        <name>White, James WC</name>
      </author>
    </item>
    <item>
      <title>Amazon windthrow disturbances are likely to increase with storm frequency under global warming</title>
      <link>https://escholarship.org/uc/item/14h8j44t</link>
      <description>Forest mortality caused by convective storms (windthrow) is a major disturbance in the Amazon. However, the linkage between windthrows at the surface and convective storms in the atmosphere remains unclear. In addition, the current Earth system models (ESMs) lack mechanistic links between convective wind events and tree mortality. Here we find an empirical relationship that maps convective available potential energy, which is well simulated by ESMs, to the spatial pattern of large windthrow events. This relationship builds connections between strong convective storms and forest dynamics in the Amazon. Based on the relationship, our model projects a 51 ± 20% increase in the area favorable to extreme storms, and a 43 ± 17% increase in windthrow density within the Amazon by the end of this century under the high-emission scenario (SSP 585). These results indicate significant changes in tropical forest composition and carbon&amp;nbsp;cycle dynamics under climate change.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/14h8j44t</guid>
      <pubDate>Tue, 2 May 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Romps, David M</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Development of a lightweight, portable, waterproof, and low power stem respiration system for trees</title>
      <link>https://escholarship.org/uc/item/6680h2x7</link>
      <description>Stem respiration is a quantitatively important, but poorly understood component of ecosystem carbon cycling in terrestrial ecosystems. However, a dynamic stem gas exchange system for quantifying real-time stem carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) efflux (E&lt;sub&gt;s&lt;/sub&gt;) is not commercially available resulting in limited observations based on the static method where air is recirculated through a stem enclosure. The static method has limited temporal resolution, suffers from condensation issues, requires a leak-free enclosure, which is often difficult to verify in the field, and requires physically removing the chamber or flushing it with ambient air before starting each measurement.•With the goal of improving our quantitative understanding of biophysical, physiological, biochemical, and environmental factors that influence diurnal E&lt;sub&gt;s&lt;/sub&gt; patterns, here we present a custom system for quantifying real-time stem E&lt;sub&gt;s&lt;/sub&gt; in remote tropical forests.•The system is low cost, lightweight,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6680h2x7</guid>
      <pubDate>Tue, 14 Feb 2023 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Augusto, Edson</name>
      </author>
      <author>
        <name>Levine, Sienna D</name>
      </author>
      <author>
        <name>Sunder, Aatish</name>
      </author>
      <author>
        <name>Som, Suman</name>
        <uri>https://orcid.org/0000-0002-0162-7302</uri>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
    </item>
    <item>
      <title>Speculative urbanism</title>
      <link>https://escholarship.org/uc/item/7gx4s5x4</link>
      <description>Speculative urbanism</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7gx4s5x4</guid>
      <pubDate>Tue, 15 Nov 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
    </item>
    <item>
      <title>Raquel Rolnik 2019: Urban Warfare: Housing under the Empire of Finance. London: Verso Books</title>
      <link>https://escholarship.org/uc/item/08f1s5rx</link>
      <description>Raquel Rolnik 2019: Urban Warfare: Housing under the Empire of Finance. London: Verso Books</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/08f1s5rx</guid>
      <pubDate>Tue, 15 Nov 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
    </item>
    <item>
      <title>Atmospheric river representation in the Energy Exascale Earth System Model (E3SM) version 1.0</title>
      <link>https://escholarship.org/uc/item/8wf505sk</link>
      <description>The Energy Exascale Earth System Model (E3SM) project is an ongoing, state-of-the-science Earth system modeling, simulation, and prediction project developed by the US Department of Energy (DOE). With an emphasis on supporting the DOE's energy mission, understanding and quantifying how well the model simulates water cycle processes is of particular importance. Here, we evaluate E3SM version 1.0 (v1.0) for its ability to represent atmospheric rivers (ARs), which play significant roles in water vapor transport and precipitation. The characteristics and precipitation associated with global ARs in E3SM at standard resolution (1×1) are compared to the Modern-Era Retrospective analysis for Research and Applications, version 2 (MERRA2). Global patterns of AR frequencies in E3SM show high degrees of correlation (≥0.97) with MERRA2 and low mean absolute errors (MAEs; &amp;lt;1%) annually, seasonally, and across different ensemble members. However, some large-scale condition biases exist, leading...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/8wf505sk</guid>
      <pubDate>Wed, 31 Aug 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Kim, Sol</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
      <author>
        <name>Guan, Bin</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Split westerlies over Europe in the early Little Ice Age</title>
      <link>https://escholarship.org/uc/item/0gv945k1</link>
      <description>The Little Ice Age (LIA; ca. 1450–1850 C.E.) is the best documented cold period of the past millennium, characterized by high-frequency volcanism, low solar activity, and high variability of Arctic sea-ice cover. Past studies of LIA Atlantic circulation changes have referenced the North Atlantic Oscillation (NAO), but recent studies have noted that LIA climate patterns appear to possess complexity not captured by an NAO analogue. Here, we present a new precipitation-sensitive stalagmite record from northern Italy that covers the past 800 years. We show that in the early LIA (1470–1610 C.E.), increased atmospheric ridging over northern Europe split the climatological westerlies away from central and northern Europe, possibly caused by concurrent Artic sea-ice reduction. With ongoing ice melting in the northern high latitudes and decreasing solar irradiance in the coming years, the early LIA may potentially serve as an analogue for European hydroclimatic conditions in the coming decades.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0gv945k1</guid>
      <pubDate>Wed, 31 Aug 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Hu, Hsun-Ming</name>
      </author>
      <author>
        <name>Shen, Chuan-Chou</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Trouet, Valerie</name>
      </author>
      <author>
        <name>Michel, Véronique</name>
      </author>
      <author>
        <name>Tsai, Hsien-Chen</name>
      </author>
      <author>
        <name>Valensi, Patricia</name>
      </author>
      <author>
        <name>Spötl, Christoph</name>
      </author>
      <author>
        <name>Starnini, Elisabetta</name>
      </author>
      <author>
        <name>Zunino, Marta</name>
      </author>
      <author>
        <name>Chien, Wei-Yi</name>
      </author>
      <author>
        <name>Sung, Wen-Hui</name>
      </author>
      <author>
        <name>Chien, Yu-Tang</name>
      </author>
      <author>
        <name>Chang, Ping</name>
      </author>
      <author>
        <name>Korty, Robert</name>
      </author>
    </item>
    <item>
      <title>East Asian Rainbands and Associated Circulation over the Tibetan Plateau Region</title>
      <link>https://escholarship.org/uc/item/6wq3z649</link>
      <description>Rainbands that migrate northward from spring to summer are persistent features of the East Asian summer monsoon. This study employs a machine learning algorithm to identify individual East Asian rainbands from May to August in the 6-hourly ERA-Interim reanalysis product and captures rainband events during these months for the period 1979–2018. The median duration of rainband events at any location in East Asia is 12 h, and the centroids of these rainbands move northward continuously from approximately 288N in late May to approximately 338N in July, instead of making jumps between quasi-stationary periods. Whereas the length and overall area of the rainbands grow monotonically from May to June, the intensity of the rainfall within the rainband dips slightly in early June before it peaks in late June. We find that extratropical northerly winds on all pressure levels over East China are the most important anomalous flow accompanying the rainband events. The anomalous northerlies...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6wq3z649</guid>
      <pubDate>Wed, 20 Jul 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Liu, Jiabin</name>
      </author>
      <author>
        <name>Fung, Inez Y</name>
        <uri>https://orcid.org/0000-0003-4106-9875</uri>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Dry Season Transpiration and Soil Water Dynamics in the Central Amazon</title>
      <link>https://escholarship.org/uc/item/6x89953z</link>
      <description>With current observations and future projections of more intense and frequent droughts in the tropics, understanding the impact that extensive dry periods may have on tree and ecosystem-level transpiration and concurrent carbon uptake has become increasingly important. Here, we investigate paired soil and tree water extraction dynamics in an old-growth upland forest in central Amazonia during the 2018 dry season. Tree water use was assessed via radial patterns of sap flow in eight dominant canopy trees, each a different species with a range in diameter, height, and wood density. Paired multi-sensor soil moisture probes used to quantify volumetric water content dynamics and soil water extraction within the upper 100 cm were installed adjacent to six of those trees. To link depth-specific water extraction patterns to root distribution, fine root biomass was assessed through the soil profile to 235 cm. To scale tree water use to the plot level (stand transpiration), basal area was...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6x89953z</guid>
      <pubDate>Tue, 19 Jul 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Spanner, Gustavo C</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Wright, Cynthia L</name>
      </author>
      <author>
        <name>Menezes, Valdiek Silva</name>
      </author>
      <author>
        <name>Newman, Brent D</name>
      </author>
      <author>
        <name>Collins, Adam D</name>
      </author>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Lima, Adriano José Nogueira</name>
      </author>
      <author>
        <name>Rodrigues, Jardel Ramos</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Warren, Jeffrey M</name>
      </author>
    </item>
    <item>
      <title>Soil moisture thresholds explain a shift from light-limited to water-limited sap velocity in the Central Amazon during the 2015–16 El Niño drought</title>
      <link>https://escholarship.org/uc/item/5wg102pq</link>
      <description>Transpiration is often considered to be light- but not water-limited in humid tropical rainforests due to abundant soil water, even during the dry seasons. The record-breaking 2015–16 El Niño drought provided a unique opportunity to examine whether transpiration is constrained by water under severe lack of rainfall. We measured sap velocity, soil water content, and meteorological variables in an old-growth upland forest in the Central Amazon throughout the 2015–16 drought. We found a rapid decline in sap velocity (−38 ± 21%, mean ± SD.) and in its temporal variability (−88%) during the drought compared to the wet season. Such changes were accompanied by a marked decline in soil moisture and an increase in temperature and vapor pressure deficit. Sap velocity was largely limited by net radiation during the wet and normal dry seasons; however, it shifted to be primarily limited by soil moisture during the drought. The threshold in which sap velocity became dominated by soil moisture...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5wg102pq</guid>
      <pubDate>Tue, 19 Jul 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Meng, Lin</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
      <author>
        <name>Koven, Charles</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Pastorello, Gilberto</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>Gimenez, Bruno</name>
      </author>
      <author>
        <name>Jardine, Kolby</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Tang, Yao</name>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Negron-Juarez, Robinson</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Araujo, Alessandro</name>
      </author>
      <author>
        <name>Tomasella, Javier</name>
      </author>
      <author>
        <name>Fontes, Clarissa</name>
      </author>
      <author>
        <name>Mohan, Midhun</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
    </item>
    <item>
      <title>Deglacial temperature history of West Antarctica.</title>
      <link>https://escholarship.org/uc/item/3qd9k5q8</link>
      <description>The most recent glacial to interglacial transition constitutes a remarkable natural experiment for learning how Earth's climate responds to various forcings, including a rise in atmospheric CO&lt;sub&gt;2&lt;/sub&gt; This transition has left a direct thermal remnant in the polar ice sheets, where the exceptional purity and continual accumulation of ice permit analyses not possible in other settings. For Antarctica, the deglacial warming has previously been constrained only by the water isotopic composition in ice cores, without an absolute thermometric assessment of the isotopes' sensitivity to temperature. To overcome this limitation, we measured temperatures in a deep borehole and analyzed them together with ice-core data to reconstruct the surface temperature history of West Antarctica. The deglacial warming was [Formula: see text]C, approximately two to three times the global average, in agreement with theoretical expectations for Antarctic amplification of planetary temperature changes....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3qd9k5q8</guid>
      <pubDate>Wed, 8 Jun 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Cuffey, Kurt M</name>
        <uri>https://orcid.org/0000-0001-9314-2996</uri>
      </author>
      <author>
        <name>Clow, Gary D</name>
      </author>
      <author>
        <name>Steig, Eric J</name>
      </author>
      <author>
        <name>Buizert, Christo</name>
      </author>
      <author>
        <name>Fudge, TJ</name>
        <uri>https://orcid.org/0000-0002-6818-7479</uri>
      </author>
      <author>
        <name>Koutnik, Michelle</name>
      </author>
      <author>
        <name>Waddington, Edwin D</name>
      </author>
      <author>
        <name>Alley, Richard B</name>
      </author>
      <author>
        <name>Severinghaus, Jeffrey P</name>
        <uri>https://orcid.org/0000-0001-8883-3119</uri>
      </author>
    </item>
    <item>
      <title>Reclaiming the chocolate city: Soundscapes of gentrification and resistance in Washington, DC</title>
      <link>https://escholarship.org/uc/item/6qn1662j</link>
      <description>In Washington, DC, Black residents have experienced unprecedented levels of cultural and physical displacement since 2000. Because of gentrification, the first “chocolate city,” long been defined by its blackness, has experienced shifts in the economy and commitments by the local government, that privilege policies that facilitate the displacement of Black families. Everyday struggles against gentrification have been of wide-ranging theoretical concern and pose an ongoing challenge for scholars in geography to understand the ways people resist gentrification and displacement. In this article, I show through an analysis of the anti-gentrification movement, #DontMuteDC, how Black people challenge the processes of gentrification by reclaiming space and resisting capitalist dispossession through cultural production. I demonstrate the relationship between Black sound aesthetics, gentrification, and a spatial politics of reclamation. I analyze the movement’s emphasis on go-go music...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6qn1662j</guid>
      <pubDate>Wed, 27 Apr 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Summers, Brandi Thompson</name>
        <uri>https://orcid.org/0000-0003-3072-3595</uri>
      </author>
    </item>
    <item>
      <title>Black insurgent aesthetics and the public imaginary</title>
      <link>https://escholarship.org/uc/item/1hm7d5n7</link>
      <description>This article analyzes the spontaneous production of graffiti art and murals covering the entrances of businesses in the central business district of Oakland, CA, in the wake of the global protest movements, in 2020, against state violence and systemic racism. I argue that the art made legible what gets hidden through the violent processes of gentrification, neoliberal urbanism, and displacement/dispossession. The paper rethinks what borders, policing, and reclamation mean in a time of economic instability and a global health crisis, through the placement of these vernacular expressions in Downtown Oakland. What is revealed through the art is the convergence of two co-constitutive publics–a segregated, decaying city mostly inhabited by poor and working-class Black and Latinx residents and laborers, and a modern, prosperous, neoliberal city that caters to a privileged class of white residents and tourists–especially as the city grappled with the management and regulation of public...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1hm7d5n7</guid>
      <pubDate>Wed, 27 Apr 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Summers, Brandi T</name>
        <uri>https://orcid.org/0000-0003-3072-3595</uri>
      </author>
    </item>
    <item>
      <title>Multi-cyclone analysis and machine learning model implications of cyclone effects on forests</title>
      <link>https://escholarship.org/uc/item/1km0k7dx</link>
      <description>Past studies of cyclones (hurricanes, typhoons, tropical cyclones) disturbance showed that meteorological, topographical, and biological factors affect the patterns of forest disturbance intensity but left open the extent to which these findings were representative across different global cyclone regions. Using remote sensing data and machine learning models, we examined how these factors change over spatial scales and assessed their consistency across four major cyclones: Katrina (August 2005), Rita (September 2005), Yasi (February 2011), and María (September 2017). Our results revealed that the factors which best explained forest disturbance intensity pattern varied across these regions. Wind speed and precipitation were the dominant factors contributing to the variation in impacts of Katrina; terrain features, especially elevation, explained most of the variation in disturbance intensity of Rita; pre-disturbance vegetation condition was significant predictors of effects of...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1km0k7dx</guid>
      <pubDate>Tue, 19 Apr 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Corporate landlords and market power: What does the single-family rental boom mean for our housing future?</title>
      <link>https://escholarship.org/uc/item/07d6445s</link>
      <description>The single-family rental (SFR) industry became a new site of institutional investment in the aftermath of the 2008 foreclosure crisis and the wider macroeconomic and policy shifts that ensued. Together with these political economic conditions, rapid advances in digital technologies, data, and analytics have been a crucial factor in the corporate transformation of SFR and the housing landscape more broadly. The four largest public and private SFR operators together control over 200,000 homes, and the SFR asset class has boomed in the pandemic, drawing interest from a wide range of investors and spawning new business models and partnerships. 

In this report we examine SEC filings and quarterly investor calls for Invitation Homes, American Homes 4 Rent, Tricon American Homes, and Front Yard Residential to trace how institutional narratives and market strategies have evolved in the SFR asset class. As the pool of foreclosed properties has largely dried up, SFR companies are developing...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/07d6445s</guid>
      <pubDate>Thu, 14 Apr 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
      <author>
        <name>Vergerio, Manon</name>
      </author>
    </item>
    <item>
      <title>Stem respiration and growth in a central Amazon rainforest</title>
      <link>https://escholarship.org/uc/item/0mv5c3f0</link>
      <description>Key messageAnnual stem CO2 efflux increases with stem wood production rates and are inhibited by daily moisture stress.AbstractTropical forests cycle a large amount of CO2 between the land and atmosphere, with a substantial portion of the return flux due tree respiratory processes. However, in situ estimates of woody tissue respiratory fluxes and carbon use efficiencies (CUEW) and their dependencies on physiological processes including stem wood production (Pw) and transpiration in tropical forests remain scarce. Here, we synthesize monthly Pw and daytime stem CO2 efflux (ES) measurements over 1 year from 80 trees with variable biomass accumulation rates in the central Amazon. On average, carbon flux to woody tissues, expressed in the same stem area normalized units as ES, averaged 0.90 ± 1.2&amp;nbsp;µmol&amp;nbsp;m−2&amp;nbsp;s−1 for Pw, and 0.55 ± 0.33&amp;nbsp;µmol&amp;nbsp;m−2&amp;nbsp;s−1 for daytime ES. A positive linear correlation was found between stem growth rates and stem CO2 efflux, with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/0mv5c3f0</guid>
      <pubDate>Wed, 16 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Cobello, Leticia O</name>
      </author>
      <author>
        <name>Teixeira, Liliane M</name>
      </author>
      <author>
        <name>East, Malyia-Mason S</name>
      </author>
      <author>
        <name>Levine, Sienna</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Robles, Emily</name>
        <uri>https://orcid.org/0000-0003-3720-6566</uri>
      </author>
      <author>
        <name>Spanner, Gustavo</name>
      </author>
      <author>
        <name>Koven, Charlie</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Xu, Chongang</name>
      </author>
      <author>
        <name>Warren, Jeffrey M</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Pastorello, Gilberto</name>
        <uri>https://orcid.org/0000-0002-9387-3702</uri>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Convergent evolution of tree hydraulic traits in Amazonian habitats: implications for community assemblage and vulnerability to drought</title>
      <link>https://escholarship.org/uc/item/3sd762s4</link>
      <description>Amazonian droughts are increasing in frequency and severity. However, little is known about how this may influence species-specific vulnerability to drought across different ecosystem types. We measured 16 functional traits for 16 congeneric species from six families and eight genera restricted to floodplain, swamp, white-sand or plateau forests of Central Amazonia. We investigated whether habitat distributions can be explained by species hydraulic strategies, and if habitat specialists differ in their vulnerability to embolism that would make water transport difficult during drought periods. We found strong functional differences among species. Nonflooded species had higher wood specific gravity and lower stomatal density, whereas flooded species had wider vessels, and higher leaf and xylem hydraulic conductivity. The P&lt;sub&gt;50&lt;/sub&gt; values (water potential at 50% loss of hydraulic conductivity) of nonflooded species were significantly more negative than flooded species. However,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3sd762s4</guid>
      <pubDate>Fri, 11 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Fontes, Clarissa G</name>
      </author>
      <author>
        <name>Fine, Paul VA</name>
      </author>
      <author>
        <name>Wittmann, Florian</name>
      </author>
      <author>
        <name>Bittencourt, Paulo RL</name>
      </author>
      <author>
        <name>Piedade, Maria Teresa Fernandez</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Dawson, Todd E</name>
        <uri>https://orcid.org/0000-0002-6871-3440</uri>
      </author>
    </item>
    <item>
      <title>Global tropical dry forest extent and cover: A comparative study of bioclimatic definitions using two climatic data sets</title>
      <link>https://escholarship.org/uc/item/41x641sc</link>
      <description>There is a debate concerning the definition and extent of tropical dry forest biome and vegetation type at a global spatial scale. We identify the potential extent of the tropical dry forest biome based on bioclimatic definitions and climatic data sets to improve global estimates of distribution, cover, and change. We compared four bioclimatic definitions of the tropical dry forest biome-Murphy and Lugo, Food and Agriculture Organization (FAO), DryFlor, aridity index-using two climatic data sets: WorldClim and Climatologies at High-resolution for the Earth's Land Surface Areas (CHELSA). We then compared each of the eight unique combinations of bioclimatic definitions and climatic data sets using 540 field plots identified as tropical dry forest from a literature search and evaluated the accuracy of World Wildlife Fund tropical and subtropical dry broadleaf forest ecoregions. We used the definition and climate data that most closely matched field data to calculate forest cover...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/41x641sc</guid>
      <pubDate>Mon, 7 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Ocón, Jonathan Pando</name>
      </author>
      <author>
        <name>Ibanez, Thomas</name>
      </author>
      <author>
        <name>Franklin, Janet</name>
        <uri>https://orcid.org/0000-0003-0314-4598</uri>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Keppel, Gunnar</name>
      </author>
      <author>
        <name>Rivas-Torres, Gonzalo</name>
      </author>
      <author>
        <name>Shin, Michael Edward</name>
      </author>
      <author>
        <name>Gillespie, Thomas Welch</name>
      </author>
    </item>
    <item>
      <title>Ethene, propene, butene and isoprene emissions from a ponderosa pine forest measured by relaxed eddy accumulation</title>
      <link>https://escholarship.org/uc/item/7qx3j5gb</link>
      <description>Alkenes are reactive hydrocarbons that influence local and regional atmospheric chemistry by playing important roles in the photochemical production of tropospheric ozone and in the formation of secondary organic aerosols. The simplest alkene, ethene (ethylene), is a major plant hormone and ripening agent for agricultural commodities. The group of light alkenes (C2-C4) originates from both biogenic and anthropogenic sources, but their biogenic sources are poorly characterized, with limited field-based flux observations. Here we report net ecosystem fluxes of light alkenes and isoprene from a semiarid ponderosa pine forest in the Rocky Mountains of Colorado, USA using the relaxed eddy accumulation (REA) technique during the summer of 2014. Ethene, propene, butene and isoprene emissions have strong diurnal cycles, with median daytime fluxes of 123, 95, 39 and 17 μg mg-2 hg-1, respectively. The fluxes were correlated with each other, followed general ecosystem trends of CO2 and water...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7qx3j5gb</guid>
      <pubDate>Tue, 1 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Rhew, Robert C</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
      <author>
        <name>Deventer, Malte Julian</name>
      </author>
      <author>
        <name>Turnipseed, Andrew A</name>
      </author>
      <author>
        <name>Warneke, Carsten</name>
      </author>
      <author>
        <name>Ortega, John</name>
      </author>
      <author>
        <name>Shen, Steve</name>
      </author>
      <author>
        <name>Martinez, Luis</name>
      </author>
      <author>
        <name>Koss, Abigail</name>
      </author>
      <author>
        <name>Lerner, Brian M</name>
      </author>
      <author>
        <name>Gilman, Jessica B</name>
      </author>
      <author>
        <name>Smith, James N</name>
        <uri>https://orcid.org/0000-0003-4677-8224</uri>
      </author>
      <author>
        <name>Guenther, Alex B</name>
        <uri>https://orcid.org/0000-0001-6283-8288</uri>
      </author>
      <author>
        <name>de Gouw, Joost A</name>
      </author>
    </item>
    <item>
      <title>Ecosystem‐Scale Measurements of Methyl Halide Fluxes From a Brackish Tidal Marsh Invaded With Perennial Pepperweed (Lepidium latifolium)</title>
      <link>https://escholarship.org/uc/item/6819v9nh</link>
      <description>Natural methyl chloride (CH3Cl) and methyl bromide (CH3Br) emissions from coastal marsh ecosystems may constitute a significant proportion of stratospheric chlorine and bromine, which catalyze ozone depletion. Current inventories involve substantial uncertainties associated with upscaling plot-scale footprints (i.e., ≤1&amp;nbsp;m2). Here we present net ecosystem flux measurements of methyl halides from a brackish tidal marsh on the west coast of the United States between April 2016 and June 2017 using the relaxed eddy accumulation method. The measurement footprint encompasses a large part of the studied tidal marsh, including roughly 20 vascular plant species, open water, and soil surfaces. On the annual scale, ecosystem methyl halide emissions showed the strongest relationships to temperature and the growth cycle of halophyte vegetation, whereas on diurnal time scales, fluxes correlated the most with evapotranspiration. The maximum seasonal emissions occurred during the flowering...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6819v9nh</guid>
      <pubDate>Tue, 1 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Deventer, MJ</name>
      </author>
      <author>
        <name>Jiao, Y</name>
      </author>
      <author>
        <name>Knox, SH</name>
      </author>
      <author>
        <name>Anderson, F</name>
      </author>
      <author>
        <name>Ferner, MC</name>
      </author>
      <author>
        <name>Lewis, JA</name>
      </author>
      <author>
        <name>Rhew, RC</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
    </item>
    <item>
      <title>Large methyl halide emissions from south Texas salt marshes</title>
      <link>https://escholarship.org/uc/item/3xj8m73q</link>
      <description>Coastal salt marshes are natural sources of methyl chloride (CH3Cl) and methyl bromide (CH3Br) to the atmosphere, but measured emission rates vary widely by geography. Here we report large methyl halide fluxes from subtropical salt marshes of south Texas. Sites with the halophytic plant, &lt;i&gt;Batis maritima&lt;/i&gt;, emitted methyl halides at rates that are orders of magnitude greater than sites containing other vascular plants or macroalgae. &lt;i&gt;B. maritima&lt;/i&gt; emissions were generally highest at midday; however, diurnal variability was more pronounced for CH3Br than CH3Cl, and surprisingly high nighttime CH3Cl fluxes were observed in July. Seasonal and intra-site variability were large, even taking into account biomass differences. Overall, these subtropical salt marsh sites show much higher emission rates than temperate salt marshes at similar times of the year, supporting the contention that low-latitude salt marshes are significant sources of CH3Cl and CH3Br.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3xj8m73q</guid>
      <pubDate>Tue, 1 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Rhew, RC</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
      <author>
        <name>Whelan, ME</name>
      </author>
      <author>
        <name>Min, D-H</name>
      </author>
    </item>
    <item>
      <title>Chloroform (CHCl3) Emissions From Coastal Antarctic Tundra</title>
      <link>https://escholarship.org/uc/item/1s17x0dd</link>
      <description>In this study, the first in situ static-chamber measurements were conducted at coastal Antarctica tundra for CHCl3 fluxes, which showed that CHCl3 was naturally emitted from the Antarctic tundra at 35&amp;nbsp;±&amp;nbsp;27&amp;nbsp;nmol m−2&amp;nbsp;d−1, comparable to other reported important natural sources. Significantly, enhanced CHCl3 emission rates (66&amp;nbsp;±&amp;nbsp;20&amp;nbsp;nmol m−2&amp;nbsp;d−1) were observed from ornithogenic soil on the island populated with penguins, which was rich in organic matter and halides coming from penguin excrements. It is estimated that Antarctic tundra emits up to 0.1&amp;nbsp;Gg CHCl3 per year, which is an important source for regional atmospheric CHCl3. Laboratory-based incubations suggested that organic carbon and chlorine inputs by penguins may stimulate O2 dependent microbial-mediated CHCl3 emission from the Antarctic tundra, and all tundra soils showed the maximum CHCl3 emission at 4°C. The strength of this CHCl3 source is also expected to change in response...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1s17x0dd</guid>
      <pubDate>Tue, 1 Feb 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Zhang, Wanying</name>
      </author>
      <author>
        <name>Jiao, Yi</name>
      </author>
      <author>
        <name>Zhu, Renbin</name>
      </author>
      <author>
        <name>Rhew, Robert C</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
      <author>
        <name>Sun, Bowen</name>
      </author>
      <author>
        <name>Dai, Haitao</name>
      </author>
    </item>
    <item>
      <title>Application of copper(II)-based chemicals induces CH3Br and CH3Cl emissions from soil and seawater</title>
      <link>https://escholarship.org/uc/item/22r2x9j1</link>
      <description>Methyl bromide (CH&lt;sub&gt;3&lt;/sub&gt;Br) and methyl chloride (CH&lt;sub&gt;3&lt;/sub&gt;Cl) are major carriers of atmospheric bromine and chlorine, respectively, which can catalyze stratospheric ozone depletion. However, in our current understanding, there are missing sources associated with these two species. Here we investigate the effect of copper(II) on CH&lt;sub&gt;3&lt;/sub&gt;Br and CH&lt;sub&gt;3&lt;/sub&gt;Cl production from soil, seawater and model organic compounds: catechol (benzene-1,2-diol) and guaiacol (2-methoxyphenol). We show that copper sulfate (CuSO&lt;sub&gt;4&lt;/sub&gt;) enhances CH&lt;sub&gt;3&lt;/sub&gt;Br and CH&lt;sub&gt;3&lt;/sub&gt;Cl production from soil and seawater, and it may be further amplified in conjunction with hydrogen peroxide (H&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt;) or solar radiation. This represents an abiotic production pathway of CH&lt;sub&gt;3&lt;/sub&gt;Br and CH&lt;sub&gt;3&lt;/sub&gt;Cl perturbed by anthropogenic application of copper(II)-based chemicals. Hence, we suggest that the widespread application of copper(II) pesticides in agriculture...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/22r2x9j1</guid>
      <pubDate>Mon, 31 Jan 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Jiao, Yi</name>
      </author>
      <author>
        <name>Zhang, Wanying</name>
      </author>
      <author>
        <name>Kim, Jae Yun Robin</name>
      </author>
      <author>
        <name>Deventer, Malte Julian</name>
      </author>
      <author>
        <name>Vollering, Julien</name>
      </author>
      <author>
        <name>Rhew, Robert C</name>
        <uri>https://orcid.org/0000-0001-6358-2050</uri>
      </author>
    </item>
    <item>
      <title>Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary</title>
      <link>https://escholarship.org/uc/item/9cb0b6c3</link>
      <description>Across the Miocene–Pliocene boundary (MPB; 5.3 million years ago, Ma), late Miocene cooling gave way to the early-to-middle Pliocene Warm Period. This transition, across which atmospheric CO2 concentrations increased to levels similar to present, holds potential for deciphering regional climate responses in Asia—currently home to more than half of the world’s population— to global climate change. Here we find that CO2-induced MPB warming both increased summer monsoon moisture transport over East Asia, and enhanced aridification over large parts of Central Asia by increasing evaporation, based on integration of our ~1–2-thousand-year (kyr) resolution summer monsoon records from the Chinese Loess Plateau aeolian red clay with existing terrestrial records, land-sea correlations, and climate model simulations. Our results offer palaeoclimate-based support for ‘wet-gets-wetter and dry-gets-drier’ projections of future regional hydroclimate responses to sustained anthropogenic forcing....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9cb0b6c3</guid>
      <pubDate>Mon, 17 Jan 2022 00:00:00 +0000</pubDate>
      <author>
        <name>Ao, Hong</name>
      </author>
      <author>
        <name>Rohling, Eelco J</name>
      </author>
      <author>
        <name>Zhang, Ran</name>
      </author>
      <author>
        <name>Roberts, Andrew P</name>
      </author>
      <author>
        <name>Holbourn, Ann E</name>
      </author>
      <author>
        <name>Ladant, Jean-Baptiste</name>
      </author>
      <author>
        <name>Dupont-Nivet, Guillaume</name>
      </author>
      <author>
        <name>Kuhnt, Wolfgang</name>
      </author>
      <author>
        <name>Zhang, Peng</name>
      </author>
      <author>
        <name>Wu, Feng</name>
      </author>
      <author>
        <name>Dekkers, Mark J</name>
      </author>
      <author>
        <name>Liu, Qingsong</name>
      </author>
      <author>
        <name>Liu, Zhonghui</name>
      </author>
      <author>
        <name>Xu, Yong</name>
      </author>
      <author>
        <name>Poulsen, Christopher J</name>
      </author>
      <author>
        <name>Licht, Alexis</name>
      </author>
      <author>
        <name>Sun, Qiang</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Liu, Xiaodong</name>
      </author>
      <author>
        <name>Wu, Guoxiong</name>
      </author>
      <author>
        <name>Ma, Chao</name>
      </author>
      <author>
        <name>Zhou, Weijian</name>
      </author>
      <author>
        <name>Jin, Zhangdong</name>
      </author>
      <author>
        <name>Li, Xinxia</name>
      </author>
      <author>
        <name>Li, Xinzhou</name>
      </author>
      <author>
        <name>Peng, Xianzhe</name>
      </author>
      <author>
        <name>Qiang, Xiaoke</name>
      </author>
      <author>
        <name>An, Zhisheng</name>
      </author>
    </item>
    <item>
      <title>Canopy Position Influences the Degree of Light Suppression of Leaf Respiration in Abundant Tree Genera in the Amazon Forest</title>
      <link>https://escholarship.org/uc/item/3t52s01j</link>
      <description>Leaf respiration in the dark (Rdark) and light (Rday) is poorly characterized in diverse tropical ecosystems, and little to no information exists on the degree of light suppression in common tree species within the Amazon basin, and their dependences upon plant functional traits and position within the canopy. We quantified Rdark and apparent Rday using the Kok method and measured key leaf traits in 26 tree individuals of different species distributed in three different canopy positions: canopy, lower canopy, and understory. To explore the relationships between the leaf traits we used the standardized major axis (SMA). We found that canopy trees had significantly higher rates of Rdark and Rday than trees in the understory. The difference between Rdark and Rday (the light suppression of respiration) was greatest in the understory (68 ± 9%, 95% CI) and lower canopy (49 ± 9%, 95% CI) when compared to the canopy (37 ± 10%, 95% CI). We also found that Rday was significantly and strongly...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/3t52s01j</guid>
      <pubDate>Thu, 9 Dec 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Souza, Daisy C</name>
      </author>
      <author>
        <name>Jardine, Kolby J</name>
        <uri>https://orcid.org/0000-0001-8491-9310</uri>
      </author>
      <author>
        <name>Rodrigues, João VFC</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>McDowell, Nate</name>
      </author>
      <author>
        <name>Walker, Anthony P</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Sampaio-Filho, Israel J</name>
      </author>
      <author>
        <name>Chambers, Jeffrey</name>
      </author>
    </item>
    <item>
      <title>Disentangling the Effects of Vapor Pressure Deficit and Soil Water Availability on Canopy Conductance in a Seasonal Tropical Forest During the 2015 El Niño Drought</title>
      <link>https://escholarship.org/uc/item/9tk4s9t6</link>
      <description>Abstract  Water deficit in the atmosphere and soil are two key interactive factors that constrain transpiration and vegetation productivity. It is not clear which of these two factors is more important for the water and carbon flux response to drought stress in ecosystems. In this study, field data and numerical modeling were used to isolate their impact on evapotranspiration (ET) and gross primary productivity (GPP) at a tropical forest site in Barro Colorado Island (BCI), Panama, focusing on their response to the drought induced by the El Niño event of 2015–2016. Numerical simulations were performed using a plant hydrodynamic scheme (HYDRO) and a heuristic approach that ignores stomatal sensitivity to leaf water potential in the Energy Exascale Earth System Model (E3SM) Land Model (ELM). The sensitivity of canopy conductance ( G s ) to vapor pressure deficit (VPD) obtained from eddy‐covariance fluxes and measured sap flux shows that, at both ecosystem and plant scale, soil water...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9tk4s9t6</guid>
      <pubDate>Thu, 19 Aug 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Fang, Yilin</name>
      </author>
      <author>
        <name>Leung, L Ruby</name>
      </author>
      <author>
        <name>Wolfe, Brett T</name>
      </author>
      <author>
        <name>Detto, Matteo</name>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>McDowell, Nate G</name>
      </author>
      <author>
        <name>Grossiord, Charlotte</name>
      </author>
      <author>
        <name>Xu, Chonggang</name>
        <uri>https://orcid.org/0000-0002-0937-5744</uri>
      </author>
      <author>
        <name>Christoffersen, Bradley O</name>
      </author>
      <author>
        <name>Gentine, Pierre</name>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Recovery of Forest Structure Following Large-Scale Windthrows in the Northwestern Amazon</title>
      <link>https://escholarship.org/uc/item/232461hb</link>
      <description>The dynamics of forest recovery after windthrows (i.e., broken or uprooted trees by wind) are poorly understood in tropical forests. The Northwestern Amazon (NWA) is characterized by a higher occurrence of windthrows, greater rainfall, and higher annual tree mortality rates (~2%) than the Central Amazon (CA). We combined forest inventory data from three sites in the Iquitos region of Peru, with recovery periods spanning 2, 12, and 22 years following windthrow events. Study sites and sampling areas were selected by assessing the windthrow severity using remote sensing. At each site, we recorded all trees with a diameter at breast height (DBH) ≥ 10 cm along transects, capturing the range of windthrow severity from old-growth to highly disturbed (mortality &amp;gt; 60%) forest. Across all damage classes, tree density and basal area recovered to &amp;gt;90% of the old-growth values after 20 years. Aboveground biomass (AGB) in old-growth forest was 380 (±156) Mg ha−1. In extremely disturbed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/232461hb</guid>
      <pubDate>Wed, 18 Aug 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Muñoz, J David Urquiza</name>
      </author>
      <author>
        <name>Marra, Daniel Magnabosco</name>
      </author>
      <author>
        <name>Negrón-Juarez, Robinson I</name>
      </author>
      <author>
        <name>Tello-Espinoza, Rodil</name>
      </author>
      <author>
        <name>Alegría-Muñoz, Waldemar</name>
      </author>
      <author>
        <name>Pacheco-Gómez, Tedi</name>
      </author>
      <author>
        <name>Rifai, Sami W</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Jenkins, Hillary S</name>
      </author>
      <author>
        <name>Brenning, Alexander</name>
      </author>
      <author>
        <name>Trumbore, Susan E</name>
        <uri>https://orcid.org/0000-0003-3885-6202</uri>
      </author>
    </item>
    <item>
      <title>Untangling the Relationship Between AMOC Variability and North Atlantic Upper‐Ocean Temperature and Salinity</title>
      <link>https://escholarship.org/uc/item/9bk973wd</link>
      <description>The relationship between Atlantic meridional overturning circulation (AMOC) variability and high-latitude North Atlantic buoyancy changes is complicated by the latter both driving, and responding to, AMOC changes. A maximum covariance analysis applied to a 1,201-year preindustrial control simulation reveals two leading modes that separate these two distinct roles of North Atlantic temperature and salinity as related to AMOC variability. A linear combination of the two modes accounts for most of the variation of a widely used AMOC index. The same analysis applied to another control simulation known to possess two distinct regimes of AMOC variability—oscillatory and red-noise—suggests that the North Atlantic buoyancy-forced AMOC variability is present in both regimes but is weaker in the latter, and moreover there is pronounced multidecadal/centennial AMOC behavior in the latter regime that is unrelated to North Atlantic buoyancy forcing.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9bk973wd</guid>
      <pubDate>Wed, 4 Aug 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, JCH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Cheng, W</name>
      </author>
      <author>
        <name>Kim, WM</name>
      </author>
      <author>
        <name>Kim, S</name>
      </author>
    </item>
    <item>
      <title>Atmospheric river lifecycle characteristics shaped by synoptic conditions at genesis</title>
      <link>https://escholarship.org/uc/item/5mp5v5sn</link>
      <description>The range of synoptic patterns that North Pacific landfalling atmospheric rivers form under are objectively identified using genesis day 500 hPa geopotential height anomalies in a self-organizing map (SOM). The SOM arranges the synoptic patterns to differentiate between two groups of climate modes—the first group with ENSO (El Niño Southern Oscillation), PDO (Pacific Decadal Oscillation), PNA (Pacific North American) and NP (North Pacific index) and the second group with AO (Arctic Oscillation), EPO (East Pacific Oscillation), and WPO (West Pacific Oscillation). These two groups have their positive and negative modes organized in opposite corners of the SOM. The ARs produced in each of the synoptic patterns have distinct lifecycle characteristics (such as genesis and landfall location, duration, velocity, meridional/zonal movement) and precipitation impacts (magnitude and spatial distribution). The conditions that favour AR trajectories closer to the tropics tend to produce higher...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5mp5v5sn</guid>
      <pubDate>Wed, 21 Jul 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Kim, Sol</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Landsat near-infrared (NIR) band and ELM-FATES sensitivity to forest disturbances and regrowth in the Central Amazon</title>
      <link>https://escholarship.org/uc/item/26c686k4</link>
      <description>Abstract. Forest disturbance and regrowth are key processes in forest dynamics, but detailed information on these processes is difficult to obtain in remote forests such as the Amazon. We used chronosequences of Landsat satellite imagery&amp;nbsp;(Landsat 5&amp;nbsp;Thematic Mapper and Landsat&amp;nbsp;7 Enhanced Thematic Mapper Plus) to determine the sensitivity of surface reflectance from all spectral bands to windthrow, clear-cut, and clear-cut and burned (cut + burn) and their successional pathways of forest regrowth in the Central Amazon. We also assessed whether the forest demography model Functionally Assembled Terrestrial Ecosystem Simulator (FATES) implemented in the Energy Exascale Earth System Model (E3SM) Land Model (ELM), ELM-FATES, accurately represents the changes for windthrow and clear-cut. The results show that all spectral bands from the Landsat satellites were sensitive to the disturbances but after 3 to 6&amp;nbsp;years only the near-infrared (NIR) band had significant changes...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/26c686k4</guid>
      <pubDate>Mon, 12 Jul 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Faybishenko, Boris</name>
        <uri>https://orcid.org/0000-0003-0085-8499</uri>
      </author>
      <author>
        <name>Magnabosco-Marra, Daniel</name>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Shuman, Jacquelyn K</name>
      </author>
      <author>
        <name>de Araujo, Alessandro C</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>From gatekeepers to gateway constructors: Credit rating agencies and the financialisation of housing associations</title>
      <link>https://escholarship.org/uc/item/696293h0</link>
      <description>This paper uses the twin metaphors of ‘gatekeeper’ and ‘gateway constructor’ as devices to explore the role of Credit Rating Agencies (CRAs) as intermediaries between global corporate finance and specific institutions – housing associations in England. The analysis utilises a financialisation framing, whereby the practices, logics and measurements of finance capital, increasingly permeate government, institutional and household behaviour and discourse. This paper examines how housing associations have increasingly resorted to corporate bond finance, partly in response to reductions in government funding, and in the process engaged with CRAs. Surprisingly little research has been undertaken on the role and function of CRAs, and their impact on the organisations they rate. The case of housing associations (HAs) is of particular interest, given their historical social mission to build and manage properties to meet housing need, rather than operate as commercial private landlords...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/696293h0</guid>
      <pubDate>Thu, 17 Jun 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Smyth, Stewart</name>
      </author>
      <author>
        <name>Cole, Ian</name>
      </author>
      <author>
        <name>Fields, Desiree</name>
      </author>
    </item>
    <item>
      <title>Relative Roles of Energy and Momentum Fluxes in the Tropical Response to Extratropical Thermal Forcing</title>
      <link>https://escholarship.org/uc/item/14p6877f</link>
      <description>This study investigates the transient responses of atmospheric energy and momentum fluxes to a time-invariant extratropical thermal heating in an atmospheric model coupled to an aquaplanet mixed layer ocean with the goal of understanding the mechanisms and time scales governing the extratropical-to-tropical connection. Two distinct stages are observed in the teleconnection: 1) A decrease in the meridional temperature gradient in midlatitudes leads to a rapid weakening of the eddy momentum flux and a slight reduction of the Hadley cell strength in the forced hemisphere. 2) The subtropical trades in the forced hemisphere decrease and reduce evaporation. The resulting change to sea surface temperature leads to the development of a cross-equatorial Hadley cell, and the intertropical convergence zone shifts to the warmer hemisphere. The Hadley cell weakening in the first stage is related to decreased eddy momentum flux divergence, and the response time scale is independent of the mixed...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/14p6877f</guid>
      <pubDate>Thu, 10 Jun 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Hwang, Yen-Ting</name>
      </author>
      <author>
        <name>Tseng, Hung-Yi</name>
      </author>
      <author>
        <name>Li, Kuan-Chen</name>
      </author>
      <author>
        <name>Kang, Sarah M</name>
      </author>
      <author>
        <name>Chen, Yung-Jen</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Walking the financialized city: confronting capitalist urbanization through mobile popular education</title>
      <link>https://escholarship.org/uc/item/67k1z076</link>
      <description>How do communities understand the highly abstract process of housing financialization? In this paper we argue that walking tours offer the capacity to develop new forms of mobile, public education to learn about the capitalist urbanization process, especially as the financialization of housing accelerates. Based on walking the city of Manchester we show that this type of learning may improve public literacy concerning the opaque and extended ways in which housing in central areas has increasingly been shaped by new types of real estate finance. Although many people in Manchester have understood the outline of these dramatic transformations, and could connect the new skyscrapers to their struggles for everyday survival, there remained a gap in detailed literacy of the actors, finances and dynamics that had changed the city so quickly. We contextualize the rapidly changing global landscape of housing since the global financial crisis of 2008 before showing how these transformations...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/67k1z076</guid>
      <pubDate>Thu, 13 May 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Silver, Jonathan</name>
      </author>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
      <author>
        <name>Goulding, Rich</name>
      </author>
      <author>
        <name>Rose, Isaac</name>
      </author>
      <author>
        <name>Donnachie, Siobhan</name>
      </author>
    </item>
    <item>
      <title>Racialized geographies of housing financialization</title>
      <link>https://escholarship.org/uc/item/5gd214jn</link>
      <description>Financial violence is racial violence: geographies of housing financialization spatialize hierarchies of death-dealing racial difference. However, research concerned with housing financialization rarely addresses the inextricable relationship between racism and capitalism. Racial division and subordination have always been necessary to producing value in real estate; financialization materially reproduces racial capitalism by reconfiguring the death-dealing abstraction of racism from systems of individual bias and racialized bodies into automated systems. Rather than reducing racially subordinated communities to experiences of oppression and domination, producing life-giving geographies of housing requires bringing collective resistance for emancipatory social change into the analytic frame.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/5gd214jn</guid>
      <pubDate>Wed, 12 May 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Fields, Desiree</name>
        <uri>https://orcid.org/0000-0001-6959-8803</uri>
      </author>
      <author>
        <name>Raymond, Elora Lee</name>
      </author>
    </item>
    <item>
      <title>Lineage‐based functional types: characterising functional diversity to enhance the representation of ecological behaviour in Land Surface Models</title>
      <link>https://escholarship.org/uc/item/1c12q7dp</link>
      <description>Process-based vegetation models attempt to represent the wide range of trait variation in biomes by grouping ecologically similar species into plant functional types (PFTs). This approach has been successful in representing many aspects of plant physiology and biophysics but struggles to capture biogeographic history and ecological dynamics that determine biome boundaries and plant distributions. Grass-dominated ecosystems are broadly distributed across all vegetated continents and harbour large functional diversity, yet most Land Surface Models (LSMs) summarise grasses into two generic PFTs based primarily on differences between temperate C&lt;sub&gt;3&lt;/sub&gt; grasses and (sub)tropical C&lt;sub&gt;4&lt;/sub&gt; grasses. Incorporation of species-level trait variation is an active area of research to enhance the ecological realism of PFTs, which form the basis for vegetation processes and dynamics in LSMs. Using reported measurements, we developed grass functional trait values (physiological, structural,...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1c12q7dp</guid>
      <pubDate>Mon, 10 May 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Griffith, Daniel M</name>
      </author>
      <author>
        <name>Osborne, Colin P</name>
      </author>
      <author>
        <name>Edwards, Erika J</name>
      </author>
      <author>
        <name>Bachle, Seton</name>
      </author>
      <author>
        <name>Beerling, David J</name>
      </author>
      <author>
        <name>Bond, William J</name>
      </author>
      <author>
        <name>Gallaher, Timothy J</name>
      </author>
      <author>
        <name>Helliker, Brent R</name>
      </author>
      <author>
        <name>Lehmann, Caroline ER</name>
      </author>
      <author>
        <name>Leatherman, Lila</name>
      </author>
      <author>
        <name>Nippert, Jesse B</name>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Qiu, Fan</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Smith, Melinda D</name>
      </author>
      <author>
        <name>Strömberg, Caroline AE</name>
      </author>
      <author>
        <name>Taylor, Lyla</name>
      </author>
      <author>
        <name>Ungerer, Mark</name>
      </author>
      <author>
        <name>Still, Christopher J</name>
      </author>
    </item>
    <item>
      <title>Remote sensing and statistical analysis of the effects of hurricane María on the forests of Puerto Rico</title>
      <link>https://escholarship.org/uc/item/03s1d44t</link>
      <description>Widely recognized as one of the worst natural disaster in Puerto Rico's history, hurricane María made landfall on September 20, 2017 in southeast Puerto Rico as a high-end category 4 hurricane on the Saffir-Simpson scale causing widespread destruction, fatalities and forest disturbance. This study focused on hurricane María's effect on Puerto Rico's forests as well as the effect of landform and forest characteristics on observed disturbance patterns. We used Google Earth Engine (GEE) to assess the severity of forest disturbance using a disturbance metric based on Landsat 8 satellite data composites with pre and post-hurricane María. Forest structure, tree phenology characteristics, and landforms were obtained from satellite data products, including digital elevation model and global forest canopy height. Our analyses showed that forest structure, and characteristics such as forest age and forest type affected patterns of forest disturbance. Among forest types, highest disturbance...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/03s1d44t</guid>
      <pubDate>Wed, 5 May 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Feng, Yanlei</name>
      </author>
      <author>
        <name>Negrón-Juárez, Robinson I</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Calibration, measurement, and characterization of soil moisture dynamics in a central Amazonian tropical forest</title>
      <link>https://escholarship.org/uc/item/9rw6h325</link>
      <description>Soil moisture plays a key role in hydrological, biogeochemical, and energy budgets of terrestrial ecosystems. Accurate soil moisture measurements in remote ecosystems such as the Amazon are difficult and limited because of logistical constraints. Time domain reflectometry (TDR) sensors are widely used to monitor soil moisture and require calibration to convert the TDR's dielectric permittivity measurement (Ka) to volumetric water content (θv). In this study, our objectives were to develop a field-based calibration of TDR sensors in an old-growth upland forest in the central Amazon, to evaluate the performance of the calibration, and then to apply the calibration to determine the dynamics of soil moisture content within a 14.2-m-deep vertical soil profile. Depth-specific TDR calibration using local soils in a controlled laboratory setting yielded a novel Ka–θv third-degree polynomial calibration. The sensors were later installed to their specific calibration depth in a 14.2-m pit....</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9rw6h325</guid>
      <pubDate>Thu, 18 Mar 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Negrón‐Juárez, Robinson</name>
      </author>
      <author>
        <name>Ferreira, Savio JF</name>
      </author>
      <author>
        <name>Mota, Marcelo Crestani</name>
      </author>
      <author>
        <name>Faybishenko, Boris</name>
        <uri>https://orcid.org/0000-0003-0085-8499</uri>
      </author>
      <author>
        <name>Monteiro, Maria Terezinha F</name>
      </author>
      <author>
        <name>Candido, Luiz A</name>
      </author>
      <author>
        <name>Ribeiro, Rubia Pereira</name>
      </author>
      <author>
        <name>Oliveira, Regison Costa</name>
      </author>
      <author>
        <name>Araujo, Alessandro C</name>
      </author>
      <author>
        <name>Warren, Jeffrey M</name>
      </author>
      <author>
        <name>Newman, Brent D</name>
      </author>
      <author>
        <name>Gimenez, Bruno O</name>
      </author>
      <author>
        <name>Varadharajan, Charuleka</name>
        <uri>https://orcid.org/0000-0002-4142-3224</uri>
      </author>
      <author>
        <name>Agarwal, Deborah</name>
      </author>
      <author>
        <name>Borma, Laura</name>
      </author>
      <author>
        <name>Tomasella, Javier</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>A Later Onset of the Rainy Season in California</title>
      <link>https://escholarship.org/uc/item/6055t6qc</link>
      <description>Californian hydroclimate is strongly seasonal and prone to severe water shortages. Recent changes in climate trends have induced shifts in seasonality, thus exacerbating droughts, wildfires, and adverse water shortage effects on the environment and economy. Previous studies have examined the timing of the seasonal cycle shifts mainly as temperature driven earlier onset of the spring season. In this paper, we address quantitative changes in the onset, amounts, and termination of the precipitation season over the past 6&amp;nbsp;decades, as well as the large-scale atmospheric circulation underpinning the seasonal cycle changes. We discover that the onset of the rainy season has been progressively delayed since the 1960s, and as a result the precipitation season has become shorter and sharper in California. The progressively later onset of the rainy season is shown to be related to the summer circulation pattern extending into autumn across the North Pacific, in particular, a delay in...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6055t6qc</guid>
      <pubDate>Wed, 17 Feb 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Luković, Jelena</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Blagojević, Dragan</name>
      </author>
      <author>
        <name>Sekulić, Aleksandar</name>
      </author>
    </item>
    <item>
      <title>When Do Ecosystem Services Depend on Rare Species?</title>
      <link>https://escholarship.org/uc/item/7xm1g947</link>
      <description>Conservation aims to preserve species and ecosystem services. If rare species contribute little to ecosystem services, yet are those most in need of preservation, tradeoffs may exist for these contrasting objectives. However, little attention has focused on identifying how, when, and where rare species contribute to ecosystem services and at what scales. Here, we review distinct ways that ecosystem services can positively depend on the presence, abundance, disproportionate contribution or, counterintuitively, the scarcity of rare species. By contrast, ecosystem services are less likely to depend on rare species that do not have a unique role in any service or become abundant enough to contribute substantially. We propose a research agenda to identify when rare species may contribute significantly to services.</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/7xm1g947</guid>
      <pubDate>Thu, 4 Feb 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Dee, Laura E</name>
      </author>
      <author>
        <name>Cowles, Jane</name>
      </author>
      <author>
        <name>Isbell, Forest</name>
      </author>
      <author>
        <name>Pau, Stephanie</name>
        <uri>https://orcid.org/0000-0001-8135-9266</uri>
      </author>
      <author>
        <name>Gaines, Steven D</name>
        <uri>https://orcid.org/0000-0002-7604-3483</uri>
      </author>
      <author>
        <name>Reich, Peter B</name>
      </author>
    </item>
    <item>
      <title>ClimateNet: an expert-labeled open dataset and deep learning architecture for enabling high-precision analyses of extreme weather</title>
      <link>https://escholarship.org/uc/item/2321d436</link>
      <description>Abstract. Identifying, detecting, and localizing extreme weather events is a crucial first step in understanding how they may vary under different climate change scenarios. Pattern recognition tasks such as classification, object detection, and segmentation (i.e., pixel-level classification) have remained challenging problems in the weather and climate sciences. While there exist many empirical heuristics for detecting extreme events, the disparities between the output of these different methods even for a single event are large and often difficult to reconcile. Given the success of deep learning (DL) in tackling similar problems in computer vision, we advocate a DL-based approach. DL, however, works best in the context of supervised learning – when labeled datasets are readily available. Reliable labeled training data for extreme weather and climate events is scarce. We create “ClimateNet” – an open, community-sourced human-expert-labeled curated dataset that captures tropical...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/2321d436</guid>
      <pubDate>Tue, 2 Feb 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Prabhat</name>
      </author>
      <author>
        <name>Kashinath, Karthik</name>
      </author>
      <author>
        <name>Mudigonda, Mayur</name>
      </author>
      <author>
        <name>Kim, Sol</name>
      </author>
      <author>
        <name>Kapp-Schwoerer, Lukas</name>
      </author>
      <author>
        <name>Graubner, Andre</name>
      </author>
      <author>
        <name>Karaismailoglu, Ege</name>
      </author>
      <author>
        <name>von Kleist, Leo</name>
      </author>
      <author>
        <name>Kurth, Thorsten</name>
      </author>
      <author>
        <name>Greiner, Annette</name>
        <uri>https://orcid.org/0000-0001-6465-7456</uri>
      </author>
      <author>
        <name>Mahesh, Ankur</name>
      </author>
      <author>
        <name>Yang, Kevin</name>
      </author>
      <author>
        <name>Lewis, Colby</name>
      </author>
      <author>
        <name>Chen, Jiayi</name>
      </author>
      <author>
        <name>Lou, Andrew</name>
      </author>
      <author>
        <name>Chandran, Sathyavat</name>
      </author>
      <author>
        <name>Toms, Ben</name>
      </author>
      <author>
        <name>Chapman, Will</name>
      </author>
      <author>
        <name>Dagon, Katherine</name>
      </author>
      <author>
        <name>Shields, Christine A</name>
      </author>
      <author>
        <name>O'Brien, Travis</name>
        <uri>https://orcid.org/0000-0002-6643-1175</uri>
      </author>
      <author>
        <name>Wehner, Michael</name>
        <uri>https://orcid.org/0000-0001-8423-7870</uri>
      </author>
      <author>
        <name>Collins, William</name>
        <uri>https://orcid.org/0000-0002-4463-9848</uri>
      </author>
    </item>
    <item>
      <title>Detection of atmospheric rivers with inline uncertainty quantification: TECA-BARD v1.0.1</title>
      <link>https://escholarship.org/uc/item/9tn726tq</link>
      <description>Abstract. It has become increasingly common for researchers to utilize methods that identify weather features in climate models. There is an increasing recognition that the uncertainty associated with choice of detection method may affect our scientific understanding. For example, results from the Atmospheric River Tracking Method Intercomparison Project (ARTMIP) indicate that there are a broad range of plausible atmospheric river (AR) detectors and that scientific results can depend on the algorithm used. There are similar examples from the literature on extratropical cyclones and tropical cyclones. It is therefore imperative to develop detection techniques that explicitly quantify the uncertainty associated with the detection of events. We seek to answer the following question: given a “plausible” AR detector, how does uncertainty in the detector quantitatively impact scientific results? We develop a large dataset of global AR counts, manually identified by a set of eight researchers...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9tn726tq</guid>
      <pubDate>Thu, 28 Jan 2021 00:00:00 +0000</pubDate>
      <author>
        <name>O'Brien, Travis A</name>
        <uri>https://orcid.org/0000-0002-6643-1175</uri>
      </author>
      <author>
        <name>Risser, Mark D</name>
        <uri>https://orcid.org/0000-0003-1956-1783</uri>
      </author>
      <author>
        <name>Loring, Burlen</name>
        <uri>https://orcid.org/0000-0002-4678-8142</uri>
      </author>
      <author>
        <name>Elbashandy, Abdelrahman A</name>
      </author>
      <author>
        <name>Krishnan, Harinarayan</name>
        <uri>https://orcid.org/0000-0001-8018-0547</uri>
      </author>
      <author>
        <name>Johnson, Jeffrey</name>
      </author>
      <author>
        <name>Patricola, Christina M</name>
      </author>
      <author>
        <name>O'Brien, John P</name>
      </author>
      <author>
        <name>Mahesh, Ankur</name>
      </author>
      <author>
        <name>Prabhat</name>
      </author>
      <author>
        <name>Ramirez, Sarahí Arriaga</name>
      </author>
      <author>
        <name>Rhoades, Alan M</name>
        <uri>https://orcid.org/0000-0003-3723-2422</uri>
      </author>
      <author>
        <name>Charn, Alexander</name>
      </author>
      <author>
        <name>Díaz, Héctor Inda</name>
      </author>
      <author>
        <name>Collins, William D</name>
        <uri>https://orcid.org/0000-0002-4463-9848</uri>
      </author>
    </item>
    <item>
      <title>The Central Amazon Biomass Sink Under Current and Future Atmospheric CO2: Predictions From Big‐Leaf and Demographic Vegetation Models</title>
      <link>https://escholarship.org/uc/item/4jd893k6</link>
      <description>Abstract  There is large uncertainty whether Amazon forests will remain a carbon sink as atmospheric CO 2 increases. Hence, we simulated an old‐growth tropical forest using six versions of four terrestrial models differing in scale of vegetation structure and representation of biogeochemical (BGC) cycling, all driven with CO 2 forcing from the preindustrial period to 2100. The models were benchmarked against tree inventory and eddy covariance data from a Brazilian site for present‐day predictions. All models predicted positive vegetation growth that outpaced mortality, leading to continual increases in present‐day biomass accumulation. Notably, the two vegetation demographic models (VDMs) (ED2 and ELM‐FATES) always predicted positive stem diameter growth in all size classes. The field data, however, indicated that a quarter of canopy trees didn't grow over the 15‐year period, and while high interannual variation existed, biomass change was near neutral. With a doubling of CO 2...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4jd893k6</guid>
      <pubDate>Tue, 12 Jan 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Holm, Jennifer A</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Zhu, Qing</name>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Lima, Adriano J Nogueira</name>
      </author>
      <author>
        <name>Riley, William J</name>
      </author>
      <author>
        <name>Longo, Marcos</name>
        <uri>https://orcid.org/0000-0001-5062-6245</uri>
      </author>
      <author>
        <name>Negrón‐Juárez, Robinson I</name>
      </author>
      <author>
        <name>de Araujo, Alessandro C</name>
      </author>
      <author>
        <name>Kueppers, Lara M</name>
        <uri>https://orcid.org/0000-0002-8134-3579</uri>
      </author>
      <author>
        <name>Moorcroft, Paul R</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
    </item>
    <item>
      <title>Integrating high resolution drone imagery and forest inventory to distinguish canopy and understory trees and quantify their contributions to forest structure and dynamics</title>
      <link>https://escholarship.org/uc/item/4gr236t1</link>
      <description>Tree growth and survival differ strongly between canopy trees (those directly exposed to overhead light), and understory trees. However, the structural complexity of many tropical forests makes it difficult to determine canopy positions. The integration of remote sensing and ground-based data enables this determination and measurements of how canopy and understory trees differ in structure and dynamics. Here we analyzed 2 cm resolution RGB imagery collected by a Remotely Piloted Aircraft System (RPAS), also known as drone, together with two decades of bi-annual tree censuses for 2 ha of old growth forest in the Central Amazon. We delineated all crowns visible in the imagery and linked each crown to a tagged stem through field work. Canopy trees constituted 40% of the 1244 inventoried trees with diameter at breast height (DBH) &amp;gt; 10 cm, and accounted for ~70% of aboveground carbon stocks and wood productivity. The probability of being in the canopy increased logistically with...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/4gr236t1</guid>
      <pubDate>Sun, 3 Jan 2021 00:00:00 +0000</pubDate>
      <author>
        <name>Araujo, Raquel Fernandes</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Celes, Carlos Henrique Souza</name>
      </author>
      <author>
        <name>Muller-Landau, Helene C</name>
      </author>
      <author>
        <name>dos Santos, Ana Paula Ferreira</name>
      </author>
      <author>
        <name>Emmert, Fabiano</name>
      </author>
      <author>
        <name>Ribeiro, Gabriel HPM</name>
      </author>
      <author>
        <name>Gimenez, Bruno Oliva</name>
      </author>
      <author>
        <name>Lima, Adriano JN</name>
      </author>
      <author>
        <name>Campos, Moacir AA</name>
      </author>
      <author>
        <name>Higuchi, Niro</name>
      </author>
    </item>
    <item>
      <title>Sulfate Aerosol Control of Tropical Atlantic Climate over the Twentieth Century</title>
      <link>https://escholarship.org/uc/item/1rv9q3k2</link>
      <description>The tropical Atlantic interhemispheric gradient in sea surface temperature significantly influences the rainfall climate of the tropical Atlantic sector, including droughts over West Africa and Northeast Brazil. This gradient exhibits a secular trend from the beginning of the twentieth century until the 1980s, with stronger warming in the south relative to the north. This trend behavior is on top of a multidecadal variation associated with the Atlantic multidecadal oscillation. A similar long-term forced trend is found in a multimodel ensemble of forced twentieth-century climate simulations. Through examining the distribution of the trend slopes in the multimodel twentieth-century and preindustrial models, the authors conclude that the observed trend in the gradient is unlikely to arise purely from natural variations; this study suggests that at least half the observed trend is a forced response to twentieth-century climate forcings. Further analysis using twentiethcentury single-forcing...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1rv9q3k2</guid>
      <pubDate>Thu, 8 Oct 2020 00:00:00 +0000</pubDate>
      <author>
        <name>Chang, C-Y</name>
      </author>
      <author>
        <name>Chiang, JCH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Wehner, MF</name>
        <uri>https://orcid.org/0000-0001-5991-0082</uri>
      </author>
      <author>
        <name>Friedman, AR</name>
      </author>
      <author>
        <name>Ruedy, R</name>
      </author>
    </item>
    <item>
      <title>Forced and unforced decadal behavior of the interhemispheric SST contrast during the instrumental period (1881–2012): contextualizing the abrupt shift around 1970 Forced and unforced decadal behavior of the interhemispheric SST contrast during the instrumental period (1881–2012): contextualizing the abrupt shift around 1970</title>
      <link>https://escholarship.org/uc/item/9k33d7dg</link>
      <description>The sea surface temperature (SST) contrast between the Northern Hemisphere (NH) and Southern Hemisphere (SH) influences the location of the intertropical convergence zone (ITCZ) and the intensity of the monsoon systems. This study examines the contributions of external forcing and unforced internal variability to the interhemispheric SST contrast in HadSST3 and ERSSTv5 observations, and 10 models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) from 1881 to 2012. Using multimodel mean fingerprints, a significant influence of anthropogenic, but not natural, forcing is detected in the interhemispheric SST contrast, with the observed response larger than that of the model mean in ERSSTv5. The forced response consists of asymmetric NH–SH SST cooling from the mid-twentieth century to around 1980, followed by opposite NH–SH SST warming. The remaining best-estimate residual or unforced component is marked by NH–SH SST maxima in the 1930s and mid-1960s, and a rapid NH–SH...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/9k33d7dg</guid>
      <pubDate>Tue, 29 Sep 2020 00:00:00 +0000</pubDate>
      <author>
        <name>Friedman, Andrew R</name>
      </author>
      <author>
        <name>Hegerl, Gabriele C</name>
      </author>
      <author>
        <name>Schurer, Andrew P</name>
      </author>
      <author>
        <name>Lee, Shih-Yu</name>
      </author>
      <author>
        <name>Kong, Wenwen</name>
      </author>
      <author>
        <name>Cheng, Wei</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
    <item>
      <title>Origins of East Asian Summer Monsoon Seasonality</title>
      <link>https://escholarship.org/uc/item/6cp545gh</link>
      <description>The East Asian summer monsoon is unique among summer monsoon systems in its complex seasonality, exhibiting distinct intraseasonal stages. Previous studies have alluded to the downstream influence of the westerlies flowing around the Tibetan Plateau as key to its existence. We explore this hypothesis using an atmospheric general circulation model that simulates the intraseasonal stages with fidelity. Without a Tibetan Plateau, East Asia exhibits only one primary convective stage typical of other monsoons. As the plateau is introduced, the distinct rainfall stages—spring, pre-mei-yu, mei-yu, and midsummer—emerge, and rainfall becomes more intense overall. This emergence coincides with a pronounced modulation of the westerlies around the plateau and extratropical northerlies penetrating northeastern China. The northerlies meridionally constrain the moist southerly flow originating from the tropics, leading to a band of lower-tropospheric convergence and humidity front that produces...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6cp545gh</guid>
      <pubDate>Tue, 29 Sep 2020 00:00:00 +0000</pubDate>
      <author>
        <name>Chiang, JCH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
      <author>
        <name>Kong, W</name>
      </author>
      <author>
        <name>Wu, CH</name>
      </author>
      <author>
        <name>Battisti, DS</name>
      </author>
    </item>
    <item>
      <title>Benchmarking and parameter sensitivity of physiological and vegetation dynamics using the Functionally Assembled Terrestrial Ecosystem Simulator (FATES) at Barro Colorado Island, Panama</title>
      <link>https://escholarship.org/uc/item/6458741n</link>
      <description>Abstract. Plant functional traits determine vegetation responses to environmental variation, but variation in trait values is large, even within a single site. Likewise, uncertainty in how these traits map to Earth system feedbacks is large. We use a vegetation demographic model (VDM), the Functionally Assembled Terrestrial Ecosystem Simulator (FATES), to explore parameter sensitivity of model predictions, and comparison to observations, at a tropical forest site: Barro Colorado Island in Panama. We define a single 12-dimensional distribution of plant trait variation, derived primarily from observations in Panama, and define plant functional types (PFTs) as random draws from this distribution. We compare several model ensembles, where individual ensemble members vary only in the plant traits that define PFTs, and separate ensembles differ from each other based on either model structural assumptions or non-trait, ecosystem-level parameters, which include (a)&amp;nbsp;the number of...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/6458741n</guid>
      <pubDate>Tue, 8 Sep 2020 00:00:00 +0000</pubDate>
      <author>
        <name>Koven, Charles D</name>
        <uri>https://orcid.org/0000-0002-3367-0065</uri>
      </author>
      <author>
        <name>Knox, Ryan G</name>
        <uri>https://orcid.org/0000-0003-1140-3350</uri>
      </author>
      <author>
        <name>Fisher, Rosie A</name>
      </author>
      <author>
        <name>Chambers, Jeffrey Q</name>
      </author>
      <author>
        <name>Christoffersen, Bradley O</name>
      </author>
      <author>
        <name>Davies, Stuart J</name>
      </author>
      <author>
        <name>Detto, Matteo</name>
      </author>
      <author>
        <name>Dietze, Michael C</name>
      </author>
      <author>
        <name>Faybishenko, Boris</name>
        <uri>https://orcid.org/0000-0003-0085-8499</uri>
      </author>
      <author>
        <name>Holm, Jennifer</name>
        <uri>https://orcid.org/0000-0001-5921-3068</uri>
      </author>
      <author>
        <name>Huang, Maoyi</name>
      </author>
      <author>
        <name>Kovenock, Marlies</name>
      </author>
      <author>
        <name>Kueppers, Lara M</name>
        <uri>https://orcid.org/0000-0002-8134-3579</uri>
      </author>
      <author>
        <name>Lemieux, Gregory</name>
        <uri>https://orcid.org/0000-0001-5304-8938</uri>
      </author>
      <author>
        <name>Massoud, Elias</name>
      </author>
      <author>
        <name>McDowell, Nathan G</name>
      </author>
      <author>
        <name>Muller-Landau, Helene C</name>
      </author>
      <author>
        <name>Needham, Jessica F</name>
        <uri>https://orcid.org/0000-0003-3653-3848</uri>
      </author>
      <author>
        <name>Norby, Richard J</name>
      </author>
      <author>
        <name>Powell, Thomas</name>
        <uri>https://orcid.org/0000-0002-3516-7164</uri>
      </author>
      <author>
        <name>Rogers, Alistair</name>
        <uri>https://orcid.org/0000-0001-9262-7430</uri>
      </author>
      <author>
        <name>Serbin, Shawn P</name>
      </author>
      <author>
        <name>Shuman, Jacquelyn K</name>
      </author>
      <author>
        <name>Swann, Abigail LS</name>
      </author>
      <author>
        <name>Varadharajan, Charuleka</name>
        <uri>https://orcid.org/0000-0002-4142-3224</uri>
      </author>
      <author>
        <name>Walker, Anthony P</name>
      </author>
      <author>
        <name>Wright, S Joseph</name>
      </author>
      <author>
        <name>Xu, Chonggang</name>
        <uri>https://orcid.org/0000-0002-0937-5744</uri>
      </author>
    </item>
    <item>
      <title>Southward Shift of Westerlies Intensifies the East Asian Early Summer Rainband Following El Niño</title>
      <link>https://escholarship.org/uc/item/1ft4c0cs</link>
      <description>An intensification of East Asian rainfall usually occurs in summers following El Niño. We propose that this teleconnection is mediated via the westerlies impinging on the Tibetan Plateau, through El Niño's control on tropical tropospheric temperature. This is distinct from previous studies that attribute the El Niño's influence to changes in the western Pacific subtropical anticyclone. The warming in the eastern equatorial Pacific leads to uniform warming of the entire tropical troposphere, which sharpens the temperature gradient between the tropics and the subtropics and shifts the westerlies southward. The westerlies impinge over the Tibetan Plateau for longer and, through interaction with the topography, induce intense and persistent extratropical northerlies downstream of the plateau that in turn intensifies the East Asian rainband. The rainband has previously been shown to intensify in a similar manner in a warming climate, suggesting that the El Niño response provides an...</description>
      <guid isPermaLink="true">https://escholarship.org/uc/item/1ft4c0cs</guid>
      <pubDate>Wed, 2 Sep 2020 00:00:00 +0000</pubDate>
      <author>
        <name>Kong, Wenwen</name>
      </author>
      <author>
        <name>Chiang, John CH</name>
        <uri>https://orcid.org/0000-0001-7723-9544</uri>
      </author>
    </item>
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