Subgrid runoff parameterization

被引:23
作者
Habets, F
Saulnier, GM
机构
[1] CNRM, Meteo France, F-31057 Toulouse, France
[2] LTHE, F-38041 Grenoble 9, France
来源
PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE | 2001年 / 26卷 / 5-6期
关键词
D O I
10.1016/S1464-1909(01)00034-X
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A subgrid parameterization of runoff based on the TOPMODEL hydrological framework is introduced within the ISBA surface scheme. Indeed, by the mean of a topographic index of hydrological similarity, the TOPMODEL framework suggests an explicit scaling equation linking; local scale and macro scale water deficit.. The idea is then to couple this scaling equation with ISBA to be able to associate the water con tent of each macro pixel (here 64km(2)) simulated hy ISBA to the corresponding subgrid spatial distribution of the local pixels (here 75x75m(2)) of the digital elevation model (DEM). The main advantage is that this subgrid runoff parameterization depends only on the topography, without any calibration parameters. The ISBA-TOPMODEL model is tested in the Ardeche basin (France), for the period 1981-1995. Soil, vegetation and atmospheric forcing are taken form the GEWEX-Rhone database.
引用
收藏
页码:455 / 459
页数:5
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