Benefit of coupling the ISBA land surface model with a TOPMODEL hydrological model version dedicated to Mediterranean flash-floods

被引:49
作者
Vincendon, Beatrice [1 ]
Ducrocq, Veronique
Saulnier, Georges-Marie [2 ]
Bouilloud, Ludovic [3 ]
Chancibault, Katia [4 ]
Habets, Florence [5 ]
Noilhan, Joel
机构
[1] CNRS, GMME MICADO, GAME CNRM, Meteo France, F-31057 Toulouse, France
[2] Univ Savoie, EDYTEM, CNRS, UMR 5204, FR-73376 Le Bourget Du Lac, France
[3] CNRS, UJF, INPG, IRD,LTHE,UMR 5564, F-38041 Grenoble, France
[4] LCPC Nantes, F-44341 Bouguenais, France
[5] Equipe SHR, Ctr Geosci, UMR SISYPHE ENSMP, F-77305 Fontainebleau, France
关键词
Hydro-meteorological coupling; SVAT; ISBA; TOPMODEL; Flash-flood; CATCHMENT-BASED APPROACH; RADAR RAINFALL PRODUCT; PART I; PARAMETERIZATION; MOISTURE; PREDICTION; BALANCE; RUNOFF; FRANCE; SCHEME;
D O I
10.1016/j.jhydrol.2010.04.012
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The ISBA land surface model and a version of the TOPMODEL hydrological model have been coupled to simulate Mediterranean flash-floods This coupling makes use of the watershed topography to compute the sub-surface lateral water fluxes and spatial and temporal dynamics of the saturated areas following the TOPMODEL principles The ISBA model governs the overall water budget and estimates the runoff supplied to the flow routing model When applied to six flash-flooding events that occurred recently over South-eastern France the coupled system proved its ability to better forecast both timing and intensity of the flood peaks compared with the ISBA model used alone To highlight further the differences between the two systems an idealized framework was set up The benefit of using ISBA-TOPMODEL instead of the ISBA model alone is clearly shown and leads to more physically consistent soil moisture and discharge simulations The coupled system is able to simulate soil moisture and discharges that are not only governed by the rainfall but also by the topography of the watershed (C) 2010 Elsevier B V All rights reserved
引用
收藏
页码:256 / 266
页数:11
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