Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology

The unavailability of proper hydrological data quality combined with the complexity of most physical based hydrologic models limits research on rainfall-runoff relationships, particularly in the tropics. In this paper, an attempt has been made to use different resolutions of DEM generated from freel...

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Main Authors: Suliman, A. H. A., Katimon, A., Darus, I. Z. M., Shahid, S.
Format: Article
Published: Springer Netherlands 2016
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Online Access:http://eprints.utm.my/id/eprint/72339/
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84966289984&doi=10.1007%2fs11269-016-1338-2&partnerID=40&md5=e8cc112c8cdf9cdc7972a049792844f8
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spelling my.utm.723392017-11-20T08:23:45Z http://eprints.utm.my/id/eprint/72339/ Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology Suliman, A. H. A. Katimon, A. Darus, I. Z. M. Shahid, S. TA Engineering (General). Civil engineering (General) The unavailability of proper hydrological data quality combined with the complexity of most physical based hydrologic models limits research on rainfall-runoff relationships, particularly in the tropics. In this paper, an attempt has been made to use different resolutions of DEM generated from freely available 30 m-based ASTER imagery as primary input to the topographically-based hydrological (TOPMODEL) model to simulate the runoff of a medium catchment located in the tropics. Response surface methodology (RSM) was applied to optimize the most sensitive parameters for streamflow simulation. DEM resolutions from 30 to 300 m have been used to assess their effects on the topographic index distribution (TI) and TOPMODEL simulation. It is found that changing DEM resolutions reduces the TOPMODEL simulation performance as the resolutions are varied from 30 to 300 m. The study concluded that the ASTER 30 m DEM can be used for reasonable streamflow simulation of a data scarce tropical catchment compared with the resampled DEMs. Springer Netherlands 2016 Article PeerReviewed Suliman, A. H. A. and Katimon, A. and Darus, I. Z. M. and Shahid, S. (2016) Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology. Water Resources Management, 30 (9). pp. 3159-3173. ISSN 0920-4741 https://www.scopus.com/inward/record.uri?eid=2-s2.0-84966289984&doi=10.1007%2fs11269-016-1338-2&partnerID=40&md5=e8cc112c8cdf9cdc7972a049792844f8
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
topic TA Engineering (General). Civil engineering (General)
spellingShingle TA Engineering (General). Civil engineering (General)
Suliman, A. H. A.
Katimon, A.
Darus, I. Z. M.
Shahid, S.
Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
description The unavailability of proper hydrological data quality combined with the complexity of most physical based hydrologic models limits research on rainfall-runoff relationships, particularly in the tropics. In this paper, an attempt has been made to use different resolutions of DEM generated from freely available 30 m-based ASTER imagery as primary input to the topographically-based hydrological (TOPMODEL) model to simulate the runoff of a medium catchment located in the tropics. Response surface methodology (RSM) was applied to optimize the most sensitive parameters for streamflow simulation. DEM resolutions from 30 to 300 m have been used to assess their effects on the topographic index distribution (TI) and TOPMODEL simulation. It is found that changing DEM resolutions reduces the TOPMODEL simulation performance as the resolutions are varied from 30 to 300 m. The study concluded that the ASTER 30 m DEM can be used for reasonable streamflow simulation of a data scarce tropical catchment compared with the resampled DEMs.
format Article
author Suliman, A. H. A.
Katimon, A.
Darus, I. Z. M.
Shahid, S.
author_facet Suliman, A. H. A.
Katimon, A.
Darus, I. Z. M.
Shahid, S.
author_sort Suliman, A. H. A.
title Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
title_short Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
title_full Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
title_fullStr Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
title_full_unstemmed Topmodel for streamflow simulation of a tropical catchment using different resolutions of ASTER DEM: optimization through response surface methodology
title_sort topmodel for streamflow simulation of a tropical catchment using different resolutions of aster dem: optimization through response surface methodology
publisher Springer Netherlands
publishDate 2016
url http://eprints.utm.my/id/eprint/72339/
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84966289984&doi=10.1007%2fs11269-016-1338-2&partnerID=40&md5=e8cc112c8cdf9cdc7972a049792844f8
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score 13.160551