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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Land-atmosphere feedbacks exacerbate concurrent soil drought and atmospheric aridity
Sha Zhou1,2,3, A Park Williams4, Alexis M Berg5
1Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964; sz2766@columbia.edu.
Compound extremes of soil drought and atmospheric aridity frequently co-occur globally. Land-atmosphere feedbacks significantly worsen these extremes, increasing their frequency and intensity, posing risks to ecosystems and society.
Area of Science:
- Climate Science
- Ecology
- Earth System Science
Background:
- Compound extremes, specifically co-occurring soil drought (low soil moisture) and atmospheric aridity (high vapor pressure deficit), pose significant threats to natural and societal systems.
- These conditions are primary physiological stressors leading to widespread vegetation mortality and reduced carbon uptake by terrestrial ecosystems.
Purpose of the Study:
- To empirically demonstrate the global prevalence of coupled soil moisture and vapor pressure deficit.
- To investigate the role of land-atmosphere feedbacks in exacerbating concurrent soil drought and atmospheric aridity.
- To project future changes in the frequency and intensity of these compound extreme events.
Main Methods:
- Empirical analysis of global soil moisture and vapor pressure deficit data to identify co-occurrence patterns.
- Utilized the Global Land Atmosphere Coupling Experiment (GLACE)-CMIP5 experiment to simulate and analyze land-atmosphere feedbacks.
- Analysis of CMIP5 model projections to assess future trends in compound extreme events.
Main Results:
- A strong negative coupling between soil moisture and vapor pressure deficit was observed globally, indicating a high probability of their co-occurrence.
- Land-atmosphere feedbacks, particularly the feedback of soil drought on the atmosphere, significantly exacerbate concurrent soil drought and atmospheric aridity.
- The soil moisture-precipitation feedback amplifies deficits in both soil moisture and precipitation across most regions.
Conclusions:
- Concurrent soil drought and atmospheric aridity are a widespread phenomenon, intensified by land-atmosphere feedbacks.
- These feedbacks are crucial in driving atmospheric aridity extremes and amplifying moisture deficits.
- CMIP5 models project an increase in the frequency and intensity of these compound extremes throughout the 21st century due to land-atmosphere feedbacks.
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