Related Experiment Video
Updated: Sep 13, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Decoupling vegetation and soil-moisture interaction in evapotranspiration interannual variability.
Xiaowen Huang1,2, Shijing Liang2,3,4, Alan D Ziegler5
1State Key Laboratory of Soil Pollution Control and Safety, Southern University of Science and Technology, Shenzhen, China.
Vegetation significantly influences evapotranspiration (ET) variability through land-atmosphere coupling (LAC). Understanding this dynamic is crucial for predicting climate variability and extreme weather events in a warming world.
Area of Science:
- Earth System Science
- Climate Science
- Ecology
Background:
- Evapotranspiration (ET) is a key driver of climate variability via land-atmosphere coupling (LAC).
- The interplay between vegetation, soil moisture, and ET in LAC is not fully understood.
- Existing research often underestimates the role of vegetation in ET dynamics.
Purpose of the Study:
- To differentiate the impacts of soil moisture and vegetation on ET interannual variability.
- To quantify the contribution of soil moisture versus vegetation to ET variability across different climate zones.
- To assess the implications of vegetation's role in ET for climate change projections.
Main Methods:
- Utilized the Community Earth System Model (CESM) for global simulations.
- Analyzed the coupling strength between soil moisture, vegetation, and ET.
- Differentiated ET variability contributions from soil evaporation and plant transpiration.
Main Results:
- Globally, 55.7% of land exhibits strong coupling between soil moisture, vegetation, and ET.
- Soil moisture-ET coupling is dominant in low-latitude LAC regions.
- Vegetation-ET coupling prevails in arid and high-latitude areas, with transpiration showing greater variability than soil evaporation in hot, dry regions.
Conclusions:
- Vegetation plays a critical, often underestimated, role in ET dynamics.
- Current LAC assessments may overlook vegetation's influence, potentially leading to underestimations of extreme event risks.
- Accurate representation of vegetation's impact on ET is vital for reliable climate change modeling and adaptation strategies.
More Related Videos
Related Concept Videos
Regulation of Transpiration by Stomata
Adaptations that Reduce Water Loss
Precipitation Processes
Precipitation and Co-precipitation
Responses to Drought and Flooding
Precipitation Gravimetry
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...

