The ISBA surface scheme in a macroscale hydrological model applied to the Hapex-Mobilhy area -: Part I:: Model and database

被引:94
作者
Habets, F
Noilhan, J
Golaz, C
Goutorbe, JP
Lacarrère, P
Martin, E
Ottlé, C
Vidal-Madjar, D
机构
[1] Meteo France, CNRM, F-31057 Toulouse, France
[2] ENSMP, CIG, F-77305 Fontainebleau, France
[3] Irstea, F-69336 Lyon, France
[4] UVSQ, CNRS, CETP, F-78140 Velizy Villacoublay, France
关键词
land-surface scheme; macroscale hydrological model; evaporation;
D O I
10.1016/S0022-1694(99)00019-0
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
As a first step towards coupling atmospheric and hydrological models, this article describes the implementation of the Interface Soil Biosphere Atmosphere (ISBA) surface scheme within a macroscale hydrological model at the regional scale. The introduction of the diurnal cycle in the hydrological model allows a coupling with the atmosphere through the energy balance and water budget computations. The coupled model is used in a forced mode, i.e. atmospheric forcing is imposed on the surface scheme without any retroaction of the surface exchanges on the atmosphere. The initial version of ISBA was modified to account for sub-grid runoff. Existing classifications of soil and vegetation at high spatial resolution (1 km) were used in conjunction with satellite information to monitor the monthly evolution of the vegetation. A dense surface network facilitated the interpolation of atmospheric fields with a time step of 3 h, The two years considered show large differences of annual precipitation and potential evaporation, which have an impact on the regime of the river flows. A one-dimensional study presents the sensitivity of the partitioning of precipitation into evaporation and runoff to the sub-grid runoff and drainage parameterizations, soil depth, and vegetation cover. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:75 / 96
页数:22
相关论文
共 62 条
[1]   Application of a macroscale hydrologic model to estimate the water balance of the Arkansas Red River basin [J].
Abdulla, FA ;
Lettenmaier, DP ;
Wood, EF ;
Smith, JA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D3) :7449-7459
[2]   MULTICRITERION VALIDATION OF A SEMIDISTRIBUTED CONCEPTUAL-MODEL OF THE WATER CYCLE IN THE FECHT CATCHMENT (VOSGES MASSIF, FRANCE) [J].
AMBROISE, B ;
PERRIN, JL ;
REUTENAUER, D .
WATER RESOURCES RESEARCH, 1995, 31 (06) :1467-1481
[3]  
ANDRE JC, 1988, ANN GEOPHYS, V6, P477
[4]  
[Anonymous], CLIMATOLOGIE ZONE PR
[5]   TURBULENCE IN AN ALMOND ORCHARD - VERTICAL VARIATIONS IN TURBULENT STATISTICS [J].
BALDOCCHI, DD ;
HUTCHISON, BA .
BOUNDARY-LAYER METEOROLOGY, 1987, 40 (1-2) :127-146
[6]   DIFFERENTIAL BARE FIELD DRAINAGE PROPERTIES FROM AIRBORNE MICROWAVE OBSERVATIONS [J].
BERNARD, R ;
SOARES, JV ;
VIDALMADJAR, D .
WATER RESOURCES RESEARCH, 1986, 22 (06) :869-875
[7]  
BOUGEAULT P, 1991, MON WEATHER REV, V119, P2358, DOI 10.1175/1520-0493(1991)119<2358:AEWAAS>2.0.CO
[8]  
2
[9]  
Boukerma B., 1987, THESIS ECOLE NATL SU
[10]   Notes on radiation in the atmosphere [J].
Brunt, D .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1932, 58 :389-420