Source of atmospheric moisture and precipitation over China’s major river basins

Abstract

Oceanic evaporation via the East Asian Monsoon (EAM) has been regarded as the major source of precipitation over China, but a recent study estimated that terrestrial evaporation might contribute up to 80% of the precipitation in the country. To explain the contradiction, this study presents a comprehensive analysis of the contribution of oceanic and terrestrial evaporation to atmospheric moisture and precipitation in China’s major river basins. The results show that from 1980 to 2010, the mean annual atmospheric moisture (precipitable water) over China was 13.7 mm, 39% of which originates from oceanic evaporation and 61% from terrestrial evaporation. The mean annual precipitation was 737 mm, 43% of which originates from oceanic evaporation and 57% from terrestrial evaporation. Oceanic evaporation makes a greater contribution to atmospheric moisture and precipitation in the East Asian Monsoon Region in South and East China than terrestrial evaporation does. Particularly, for the Pearl River and southeastern rivers, oceanic evaporation contributes approximately 65% of annual precipitation and more than 70% of summer precipitation. Meanwhile, terrestrial evaporation contributes more precipitation in northwest China due to the westerly wind. For the northwestern rivers, terrestrial evaporation from the Eurasian continents contributes more than 70% of precipitation. There is a linear relation between mean annual precipitation and the contribution of oceanic evaporation to precipitation, with a correlation coefficient of 0.92, among the ten major river basins in China.

Keywords

oceanic evaporation / terrestrial evaporation / moisture transport / East Asian Monsoon / westerly wind / Tibetan Plateau

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Acknowledgements

The authors would like to thank Dr. Ruud van der Ent for helping to set up the water accounting model, and Prof. Glenn Patterson, Mr. Ragai Wanis and Dr. Junmei Lv for the helpful comments to improve the paper. The research has been financially supported by the National Natural Science Foundation of China (Grant Nos. 51409145 and 51179085) and the National Basic Research Program of China (Nos. 2011BAC09B07 and 2013BAB05B03).

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2015 Higher Education Press and Springer-Verlag Berlin Heidelberg