Global evapotranspiration from high-elevation mountains has decreased significantly at a rate of 3.923 %/a over the last 22 years-Reference-Cited by-同舟云学术

Global evapotranspiration from high-elevation mountains has decreased significantly at a rate of 3.923 %/a over the last 22 years

Published:2024-06 Issue: Volume:931 Page:172804
ISSN:0048-9697
Container-title:Science of The Total Environment
language:en
Short-container-title:Science of The Total Environment

Author:

Wang Yunying,Li Zongxing,Feng Qi,Si Lanping,Gui Juan,Cui Qiao,Zhao Yue,Xu Chong

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference77 articles.

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3. Chen, R. S., K, E. S., Yang, J. P., Zhang, J. S., Wang, S. G. 2003. Application of Topmodel to simulate runoff from Heihe mainstream Mountainous Basin. Desert China, (04): 94–100.

4. Simulation of reference crop evapotranspiration in hilly area of Central Sichuan based on MARS;Chen;Transactions of the Chinese Society of Agricutural Engineering,2019

5. Improving the penman-Monteith evapotranspiration model based on the coupling principle of carbon and water fluxes;Chen;Trans. Atmos. Sci.,2020

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1. Corrigendum to “Global evapotranspiration from high-elevation mountains has decreased significantly at a rate of 3.923 %/a over the last 22 years” [Sci. Total Environ. 931 (2024) 172804];Science of The Total Environment;2024-08