Use of pan evaporation to estimate terrestrial evaporation trends: The case of the Tibetan Plateau
DOI: 10.1002/WRCR.20247
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摘要: [1] There is still no general agreement on the relationship between evaporation of open water from a small pan and terrestrial surrounding landscape under drying conditions. A possible way out this impasse reviewed applied to harsh extreme climatic conditions Tibetan Plateau. It confirmed herein that during 1966–2000 with trend −4.57 mm a−2, was +0.7 in experimental findings Zhang et al. (2007).
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