about
Global satellite monitoring of climate-induced vegetation disturbances.FOREST ECOLOGY. Pervasive drought legacies in forest ecosystems and their implications for carbon cycle models.Impact of anthropogenic climate change on wildfire across western US forests.The influence of summertime fog and overcast clouds on the growth of a coastal Californian pine: a tree-ring study.Integrating physiological threshold experiments with climate modeling to project mangrove species' range expansion.The critical amplifying role of increasing atmospheric moisture demand on tree mortality and associated regional die-offEmpirical and process-based approaches to climate-induced forest mortality models.Evaluating theories of drought-induced vegetation mortality using a multimodel-experiment framework.Seasonal and episodic moisture controls on plant and microbial contributions to soil respiration.Trends toward an earlier peak of the growing season in Northern Hemisphere mid-latitudes.Contribution of anthropogenic warming to California drought during 2012-2014Improving operational land surface model canopy evapotranspiration in Africa using a direct remote sensing approachSwitching on the Big Burn of 2017Climatic influences on interannual variability in regional burn severity across western US forestsThe 2016 southeastern US drought: an extreme departure from centennial wetting and coolingThe Curious Case of Projected Twenty-First-Century Drying but Greening in the American WestExacerbation of the 2013-2016 Pan-Caribbean Drought by Anthropogenic WarmingTemperature as a potent driver of regional forest drought stress and tree mortalityUrbanization causes increased cloud base height and decreased fog in coastal Southern CaliforniaProjected Future Changes in Vegetation in Western North America in the Twenty-First CenturyPatterns and correlates of giant sequoia foliage dieback during California’s 2012–2016 hotter droughtA range of possibilities: Assessing geographic variation in climate sensitivity of ponderosa pine using tree ringsWhither the 100th Meridian? The Once and Future Physical and Human Geography of America’s Arid–Humid Divide. Part I: The Story So FarFog drip maintains dry season ecological function in a California coastal pine forestSpatial and Temporal Patterns of Cloud Cover and Fog Inundation in Coastal California: Ecological ImplicationsNorth American megadroughts in the Common Era: reconstructions and simulationsRecent Advances and Remaining Uncertainties in Resolving Past and Future Climate Effects on Global Fire ActivityClimatology, Variability, and Trends in the U.S. Vapor Pressure Deficit, an Important Fire-Related Meteorological Quantity*Correlations between components of the water balance and burned area reveal new insights for predicting forest fire area in the southwest United StatesSea Surface Temperature Warming Patterns and Future Vegetation ChangeCauses and Implications of Extreme Atmospheric Moisture Demand during the Record-Breaking 2011 Wildfire Season in the Southwestern United States*Recent summer precipitation trends in the Greater Horn of Africa and the emerging role of Indian Ocean sea surface temperatureA westward extension of the warm pool leads to a westward extension of the Walker circulation, drying eastern AfricaUsing Tree Rings to Predict the Response of Tree Growth to Climate Change in the Continental United States during the Twenty-First CenturySignificance of summer fog and overcast for drought stress and ecological functioning of coastal California endemic plant speciesProjected increases in intensity, frequency, and terrestrial carbon costs of compound drought and aridity eventsStrengthened scientific support for the Endangerment Finding for atmospheric greenhouse gasesClimate-driven regime shifts in a mangrove-salt marsh ecotone over the past 250 yearsLarge and projected strengthening moisture limitation on end-of-season photosynthesisLarge contribution from anthropogenic warming to an emerging North American megadrought
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P. Williams
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Park Williams
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P108
P1053
B-8214-2016
P106
P108
P31
P3829
P496
0000-0001-8176-8166