The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin
The UP (Upscaled Physically-based) hydrological modelling system to the Arkansas-Red River basin (USA) is designed for macro-scale simulations of land surface processes, and aims for a physical basis and, avoids the use of discharge records in the direct calibration of parameters. This is achieved i...
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1999-01-01
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doaj-19408d8cbd3d445e996953c3759544c02020-11-25T02:24:25ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79381999-01-0131137149The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basinC. G. KilsbyC. G. KilsbyJ. EwenJ. EwenW. T. SloanW. T. SloanA. BurtonA. BurtonC. S. FallowsC. S. FallowsP. E. O'ConnellP. E. O'ConnellThe UP (Upscaled Physically-based) hydrological modelling system to the Arkansas-Red River basin (USA) is designed for macro-scale simulations of land surface processes, and aims for a physical basis and, avoids the use of discharge records in the direct calibration of parameters. This is achieved in a two stage process: in the first stage parametrizations are derived from detailed modelling of selected representative small and then used in a second stage in which a simple distributed model is used to simulate the dynamic behaviour of the whole basin. The first stage of the process is described in a companion paper (Ewen <i>et al.</i>, this issue), and the second stage of this process is described here. The model operated at an hourly time-step on 17-km grid squares for a two year simulation period, and represents all the important hydrological processes including regional aquifer recharge, groundwater discharge, infiltration- and saturation-excess runoff, evapotranspiration, snowmelt, overland and channel flow. Outputs from the model are discussed, and include river discharge at gauging stations and space-time fields of evaporation and soil moisture. Whilst the model efficiency assessed by comparison of simulated and observed discharge records is not as good as could be achieved with a model calibrated against discharge, there are considerable advantages in retaining a physical basis in applications to ungauged river basins and assessments of impacts of land use or climate change.http://www.hydrol-earth-syst-sci.net/3/137/1999/hess-3-137-1999.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
C. G. Kilsby C. G. Kilsby J. Ewen J. Ewen W. T. Sloan W. T. Sloan A. Burton A. Burton C. S. Fallows C. S. Fallows P. E. O'Connell P. E. O'Connell |
spellingShingle |
C. G. Kilsby C. G. Kilsby J. Ewen J. Ewen W. T. Sloan W. T. Sloan A. Burton A. Burton C. S. Fallows C. S. Fallows P. E. O'Connell P. E. O'Connell The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin Hydrology and Earth System Sciences |
author_facet |
C. G. Kilsby C. G. Kilsby J. Ewen J. Ewen W. T. Sloan W. T. Sloan A. Burton A. Burton C. S. Fallows C. S. Fallows P. E. O'Connell P. E. O'Connell |
author_sort |
C. G. Kilsby |
title |
The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin |
title_short |
The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin |
title_full |
The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin |
title_fullStr |
The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin |
title_full_unstemmed |
The UP modelling system for large scale hydrology: simulation of the Arkansas-Red River basin |
title_sort |
up modelling system for large scale hydrology: simulation of the arkansas-red river basin |
publisher |
Copernicus Publications |
series |
Hydrology and Earth System Sciences |
issn |
1027-5606 1607-7938 |
publishDate |
1999-01-01 |
description |
The UP (Upscaled Physically-based) hydrological modelling system to the Arkansas-Red River basin (USA) is designed for macro-scale simulations of land surface processes, and aims for a physical basis and, avoids the use of discharge records in the direct calibration of parameters. This is achieved in a two stage process: in the first stage parametrizations are derived from detailed modelling of selected representative small and then used in a second stage in which a simple distributed model is used to simulate the dynamic behaviour of the whole basin. The first stage of the process is described in a companion paper (Ewen <i>et al.</i>, this issue), and the second stage of this process is described here. The model operated at an hourly time-step on 17-km grid squares for a two year simulation period, and represents all the important hydrological processes including regional aquifer recharge, groundwater discharge, infiltration- and saturation-excess runoff, evapotranspiration, snowmelt, overland and channel flow. Outputs from the model are discussed, and include river discharge at gauging stations and space-time fields of evaporation and soil moisture. Whilst the model efficiency assessed by comparison of simulated and observed discharge records is not as good as could be achieved with a model calibrated against discharge, there are considerable advantages in retaining a physical basis in applications to ungauged river basins and assessments of impacts of land use or climate change. |
url |
http://www.hydrol-earth-syst-sci.net/3/137/1999/hess-3-137-1999.pdf |
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