Calibration of the Hydrological Simulation Program Fortran (HSPF) model using automatic calibration and geographical information systems

被引:53
作者
Al-Abed, NA
Whiteley, HR
机构
[1] Jordan Univ Sci & Technol, Dept Agr Engn & Technol, Irbid 22110, Jordan
[2] Univ Guelph, Sch Engn, Guelph, ON N1G 2W1, Canada
关键词
model; calibration; GIS; watershed; hydrology;
D O I
10.1002/hyp.1094
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Calibrating a comprehensive, multi-parameter conceptual hydrological model, such as the Hydrological Simulation Program Fortran model, is a major challenge. This paper describes calibration procedures for water-quantity parameters of the HSPF version 10.11 using the automatic-calibration parameter estimator model coupled with a geographical information system (GIS) approach for spatially averaged properties. The study area was the Grand River watershed, located in southern Ontario, Canada, between 79degrees 30' and 80degrees 57'W longitude and 42degrees 51' and 44degrees 3 IN latitude. The drainage area is 6965 km(2). Calibration efforts were directed to those model parameters that produced large changes in model response during sensitivity tests run prior to undertaking calibration. A GIS was used extensively in this study. It was first used in the watershed segmentation process. During calibration, the GIS data were used to establish realistic starting values for the surface and subsurface zone parameters LZSN, UZSN, COVER, and INFILT and physically reasonable ratios of these parameters among watersheds were preserved during calibration with the ratios based on the known properties of the subwatersheds determined using GIs. This calibration procedure produced very satisfactory results; the percentage difference between the simulated and the measured yearly discharge ranged between 4 to 16%, which is classified as good to very good calibration. The average simulated daily discharge for the watershed outlet at Brantford for the years 1981-85 was 67 m(3) s(-1) and the average measured discharge at Brantford was 70 m(3) s(-1). The coupling of a GIS with automatice calibration produced a realistic and accurate calibration for the HSPF model with much less effort and subjectivity than would be required for unassisted calibration. Copyright (C) 2002 John Wiley Sons, Ltd.
引用
收藏
页码:3169 / 3188
页数:20
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