Soil Evaporation Stress Determines Soil Moisture‐Evapotranspiration Coupling Strength in Land Surface Modeling-Reference-Cited by-同舟云学术

Soil Evaporation Stress Determines Soil Moisture‐Evapotranspiration Coupling Strength in Land Surface Modeling

Published:2020-10-31 Issue:21 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Dong Jianzhi¹^ORCID,Dirmeyer Paul A.²^ORCID,Lei Fangni³,Anderson Martha C.¹^ORCID,Holmes Thomas R. H.⁴^ORCID,Hain Christopher⁵^ORCID,Crow Wade T.¹^ORCID

Affiliation:

1. Hydrology and Remote Sensing Laboratory, USDA‐ARS Beltsville MD USA

2. Center for Ocean‐Land‐Atmosphere Studies George Mason University Fairfax VA USA

3. Geosystems Research Institute Mississippi State University Starkville MS USA

4. Hydrological Sciences Laboratory NASA Goddard Space Flight Center Greenbelt MD USA

5. Earth Science Office NASA Marshall Space Flight Center Huntsville AL USA

Funder

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL090391

Reference51 articles.

1. A Model Predicting Stomatal Conductance and its Contribution to the Control of Photosynthesis under Different Environmental Conditions

2. Evapotranspiration Partitioning in CMIP5 Models: Uncertainties and Future Projections

3. Improving canopy processes in the Community Land Model version 4 (CLM4) using global flux fields empirically inferred from FLUXNET data

4. Why Do Large‐Scale Land Surface Models Produce a Low Ratio of Transpiration to Evapotranspiration?

5. Soil Moisture–Evapotranspiration Overcoupling and L-Band Brightness Temperature Assimilation: Sources and Forecast Implications

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