Modeling the land surface water and energy cycles of a mesoscale watershed in the central Tibetan Plateau during summer with a distributed hydrological model-Reference-Cited by-同舟云学术

Modeling the land surface water and energy cycles of a mesoscale watershed in the central Tibetan Plateau during summer with a distributed hydrological model

Published:2013-08-22 Issue:16 Volume:118 Page:8857-8868
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Xue Bao-Lin¹²,Wang Lei¹,Yang Kun¹,Tian Lide¹,Qin Jun¹,Chen Yingying¹,Zhao Long¹,Ma Yaoming¹,Koike Toshio³,Hu Zeyong⁴,Li Xiuping¹

Affiliation:

1. Key Laboratory of Tibetan Environmental Changes and Land Surface Processes; Institute of Tibetan Plateau Research, Chinese Academy of Sciences; Beijing China

2. State Key Laboratory of Vegetation and Environmental Change; Institute of Botany, Chinese Academy of Sciences; Beijing China

3. Department of Civil Engineering; University of Tokyo; Tokyo Japan

4. Cold and Arid Regions Environmental and Engineering Research Institute; Chinese Academy of Sciences; Lanzhou China

Funder

“Strategic Priority Research Program (B)” of the Chinese Academy of Sciences

National Natural Science Foundation of China

National Key Basic Research Program of China

Key Technologies R&D Program of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/jgrd.50696/fullpdf

Reference54 articles.

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4. A kinematic model of infiltration and runoff generation in layered and sloped soils;Cabral;Adv. Water Resour.,1992

5. River discharge changes in the Qinghai-Tibet Plateau;Cao;Chin. Sci. Bull.,2006

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