Hydrological daily rainfall-runoff simulation with BTOPMC model and comparison with Xin'anjiang model  

作　　者：Hong-jun BAO Li-li WANG Zhi-jia LI Lin-na ZHAO Guo-ping ZHANG 

机构地区：[1]National Meteorological Center, China Meteorological Administration, Beijing 100081, P. R. China [2]Numerical Prediction Center, China Meteorological Administration, Beijing 100081, P. R. China [3]College of Hydrology and Water Resources, Hohai University, Nanjing 210098, P. R. China

出　　处：《Water Science and Engineering》2010年第2期121-131,共11页水科学与水工程（英文版）

基　　金：supported by the Research Fund for Commonweal Trades (Meteorology) (Grants No.GYHY200706037, GYHY (QX) 2007-6-1,GYHY200906007,and GYHY201006038);the National Natural Science Foundation of China (Grants No.50479017 and 40971016);Program for Changjiang Scholars and Innovative Research Team in University (Grant No.IRT0717)

摘　　要：A grid-based distributed hydrological model, the Block-wise use of TOPMODEL （BTOPMC）, which was developed from the original TOPMODEL, was used for hydrological daily rainfall-runoff simulation. In the BTOPMC model, the runoff is explicitly calculated on a cell-by-cell basis, and the Muskingum-Cunge flow concentration method is used. In order to test the model＇s applicability, the BTOPMC model and the Xin＇anjiang model were applied to the simulation of a humid watershed and a semi-humid to semi-arid watershed in China. The model parameters were optimized with the Shuffle Complex Evolution （SCE-UA） method. Results show that both models can effectively simulate the daily hydrograph in humid watersheds, but that the BTOPMC model performs poorly in semi-humid to semi-arid watersheds. The excess-infiltration mechanism should be incorporated into the BTOPMC model to broaden the model＇s applicability.A grid-based distributed hydrological model, the Block-wise use of TOPMODEL （BTOPMC）, which was developed from the original TOPMODEL, was used for hydrological daily rainfall-runoff simulation. In the BTOPMC model, the runoff is explicitly calculated on a cell-by-cell basis, and the Muskingum-Cunge flow concentration method is used. In order to test the model＇s applicability, the BTOPMC model and the Xin＇anjiang model were applied to the simulation of a humid watershed and a semi-humid to semi-arid watershed in China. The model parameters were optimized with the Shuffle Complex Evolution （SCE-UA） method. Results show that both models can effectively simulate the daily hydrograph in humid watersheds, but that the BTOPMC model performs poorly in semi-humid to semi-arid watersheds. The excess-infiltration mechanism should be incorporated into the BTOPMC model to broaden the model＇s applicability.

关 键 词：digital elevation model BTOPMC model Xin＇ anjiang model daily rainfall-runoff simulation SCE-UA method humid watershed semi-humid to semi-arid watershed 

分 类 号：TV121.7[水利工程—水文学及水资源] P334.92[天文地球—水文科学]