Hubei Key Laboratory of Petroleum Geochemistry and Environment,
Yangtze University, Wuhan 430100, Hubei, China
College of Resources and Environment, Yangtze University, Wuhan
430100, Hubei, China
Lei Wang
College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling 712100, Shaanxi, China
Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A & F University,
Yangling 712100, Shaanxi, China
Jie Yang
College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling 712100, Shaanxi, China
Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A & F University,
Yangling 712100, Shaanxi, China
Bingcheng Si
Department of Soil Science, University of Saskatchewan, Saskatoon, SK S7N 5A8, Canada
Guo-Yue Niu
Biosphere 2, the University of Arizona, Tucson, AZ 85623, USA
Department of Hydrology and Water Resources, University of Arizona,
Tucson, AZ 85721, USA
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Total article views: 778 (including HTML, PDF, and XML)
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1,109
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Total article views: 2,154 (including HTML, PDF, and XML)
Thereof 1,928 with geography defined
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Total article views: 778 (including HTML, PDF, and XML)
Thereof 734 with geography defined
and 44 with unknown origin.
Total article views: 1,376 (including HTML, PDF, and XML)
Thereof 1,194 with geography defined
and 182 with unknown origin.
This study aimed to improve runoff simulations and explore deep soil hydrological processes for a highly varying soil depth and complex terrain watershed in the Loess Plateau, China. The actual soil depths and river channels were incorporated into the model to better simulate the runoff in this watershed. The soil evaporation scheme was modified to better describe the evaporation processes. Our results showed that the model significantly improved the runoff simulations.
This study aimed to improve runoff simulations and explore deep soil hydrological processes for...