Satellite retrieval of actual evapotranspiration in the Tibetan Plateau: Components partitioning, multidecadal trends and dominated factors identifying

2018 ◽  
Vol 559 ◽  
pp. 471-485 ◽  
Author(s):  
Weiguang Wang ◽  
Jinxing Li ◽  
Zhongbo Yu ◽  
Yimin Ding ◽  
Wanqiu Xing ◽  
...  
2017 ◽  
Vol 132 (3-4) ◽  
pp. 1039-1047 ◽  
Author(s):  
Mijun Zou ◽  
Lei Zhong ◽  
Yaoming Ma ◽  
Yuanyuan Hu ◽  
Lu Feng

2017 ◽  
Vol 38 ◽  
pp. e48-e56 ◽  
Author(s):  
Tangtang Zhang ◽  
Mekonnen Gebremichael ◽  
Xianhong Meng ◽  
Jun Wen ◽  
Mudassar Iqbal ◽  
...  

2021 ◽  
Author(s):  
Cunbo Han ◽  
Yaoming Ma ◽  
Binbin Wang ◽  
Lei Zhong ◽  
Weiqiang Ma ◽  
...  

Abstract. Terrestrial actual evapotranspiration (ETa) is a key parameter controlling the land-atmosphere interaction processes and the water cycle. However, the spatial distribution and temporal changes of ETa over the Tibetan Plateau (TP) remain very uncertain. Here we estimate the multiyear (2001–2018) monthly ETa and its spatial distribution on the TP by a combination of meteorological data and satellite products. Validation against data from six eddy-covariance monitoring sites yielded a root mean square errors ranging from 9.3 to 14.5 mm mo−1, and correlation coefficients exceeding 0.9. The domain mean of annual ETa on the TP decreased slightly (−1.45 mm yr−1, p 


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