Use of pan evaporation to estimate terrestrial evaporation trends: The case of the Tibetan Plateau

被引：32

作者：

Brutsaert, Wilfried ^{[1
]}

机构：

[1] Cornell Univ, Sch Civil & Environm Engn, Ithaca, NY 14853 USA

来源：

WATER RESOURCES RESEARCH | 2013年 / 49卷 / 05期

关键词：

REFERENCE EVAPOTRANSPIRATION; SURFACE-LAYER; CLIMATE; CHINA; FLUX;

D O I：

10.1002/wrcr.20247

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

There is still no general agreement on the relationship between the evaporation of open water from a small pan and the terrestrial evaporation from the surrounding landscape under drying conditions. A possible way out of this impasse is reviewed and applied to the harsh and extreme climatic conditions of the Tibetan Plateau. It is confirmed herein that during 1966-2000 with a pan evaporation trend of -4.57 mm a-2, the terrestrial evaporation trend was +0.7 mm a-2, in agreement with the experimental findings of Zhang et al. (2007). ©2013. American Geophysical Union. All Rights Reserved.

引用

页码：3054 / 3058

页数：5

共 48 条

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