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-Reference-Cited by-同舟云学术

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

Published:2021-05-17 Issue:10 Volume:126 Page:
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:Geophys Res Atmos

Author:

Fang Yilin¹^ORCID,Leung L. Ruby¹^ORCID,Wolfe Brett T²^ORCID,Detto Matteo³^ORCID,Knox Ryan G⁴,McDowell Nate G¹^ORCID,Grossiord Charlotte⁵^ORCID,Xu Chonggang⁶^ORCID,Christoffersen Bradley O⁷^ORCID,Gentine Pierre⁸^ORCID,Koven Charles D⁴^ORCID,Chambers Jeffrey Q⁴

Affiliation:

1. Pacific Northwest National Laboratory Richland WA USA

2. Smithsonian Tropical Research Institute School of Renewable Natural Resources Louisiana State University Agricultural Center Baton Rouge LA USA

3. Department of Ecology and Evolutionary Biology Princeton University Princeton NJ USA

4. Lawrence Berkeley National Laboratory Berkeley CA USA

5. Swiss Federal Institute for Forest, Snow and Landscape Research WSL Birmensdorf Switzerland

6. Earth and Environmental Sciences Division Los Alamos National Laboratory Los Alamos NM USA

7. Department of Biology University of Texas Rio Grande Valley Edinburg TX USA

8. Department of Earth and Environmental Engineering Columbia University New York NY USA

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JD035004

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3. Hydraulic traits explain differential responses of Amazonian forests to the 2015 El Niño‐induced drought

4. Predicting shifts in the functional composition of tropical forests under increased drought and CO 2 from trade‐offs among plant hydraulic traits

5. Field quantification of wetting–drying cycles to predict temporal changes of soil pore size distribution

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