Coupled Snow and Frozen Ground Physics Improves Cold Region Hydrological Simulations: An Evaluation at the upper Yangtze River Basin (Tibetan Plateau)

Author:

Qi Jia12,Wang Lei123,Zhou Jing1,Song Lei12,Li Xiuping1,Zeng Tian1

Affiliation:

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

2. University of Chinese Academy of Sciences Beijing China

3. CAS Center for Excellence in Tibetan Plateau Earth Sciences Beijing China

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

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

Reference65 articles.

1. Snow depth derived from passive microwave remote-sensing data in China

2. Improving land surface temperature modeling for dry land of China

3. Permafrost and groundwater on the Qinghai-Tibet Plateau and in northeast China

4. Trends in runoff of the source region of the Yangtze River and the Yellow River for 21st century;Cheng Z.;Research Environment Yangtze,2010

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