Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China

In this paper we analyse the effects of different spatial input data resolution on water balance simulation using a simple distributed hydrological model: PCR-XAJ model. A data set consisting of land use and digital elevation model at 25 m resolution of Xitiaoxi catchment in South China is used for...

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Main Authors: J. F. Gao, N. Fohrer, G. Hörmann, G. J. Zhao
Format: Article
Language:English
Published: Copernicus Publications 2009-08-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/21/131/2009/adgeo-21-131-2009.pdf
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spelling doaj-95db88b40f7945189f5077c8881acfbd2020-11-25T00:48:44ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592009-08-0121131137Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South ChinaJ. F. GaoN. FohrerG. HörmannG. J. ZhaoIn this paper we analyse the effects of different spatial input data resolution on water balance simulation using a simple distributed hydrological model: PCR-XAJ model. A data set consisting of land use and digital elevation model at 25 m resolution of Xitiaoxi catchment in South China is used for investigation. The model was first calibrated and validated at 50 m cell size, thereafter an aggregation of the digital elevation model (DEM) and land use maps at 100 m, 200 m, 300 m, 500 m and 1 km are applied to evaluate the effects of spatial data resolution on simulated discharge. The simulation results at a grid size of 50 m show a good correlation between measured and simulated daily flows at Hengtangcun station with Nash-Suttcliffe efficiency larger than 0.75 for both calibration and validation periods. In contrast, the model performs slightly worse at Fanjiacun station. The increasing grid size affects the characteristics of the slope and land use aggregation and causes important information loss. The aggregation of input data does not lead to significant errors up to a grid of 1 km. Model efficiencies decrease slightly with cell size increasing, and more significantly up to the grid size of 1 km. http://www.adv-geosci.net/21/131/2009/adgeo-21-131-2009.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. F. Gao
N. Fohrer
G. Hörmann
G. J. Zhao
spellingShingle J. F. Gao
N. Fohrer
G. Hörmann
G. J. Zhao
Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
Advances in Geosciences
author_facet J. F. Gao
N. Fohrer
G. Hörmann
G. J. Zhao
author_sort J. F. Gao
title Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
title_short Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
title_full Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
title_fullStr Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
title_full_unstemmed Impacts of spatial data resolution on simulated discharge, a case study of Xitiaoxi catchment in South China
title_sort impacts of spatial data resolution on simulated discharge, a case study of xitiaoxi catchment in south china
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2009-08-01
description In this paper we analyse the effects of different spatial input data resolution on water balance simulation using a simple distributed hydrological model: PCR-XAJ model. A data set consisting of land use and digital elevation model at 25 m resolution of Xitiaoxi catchment in South China is used for investigation. The model was first calibrated and validated at 50 m cell size, thereafter an aggregation of the digital elevation model (DEM) and land use maps at 100 m, 200 m, 300 m, 500 m and 1 km are applied to evaluate the effects of spatial data resolution on simulated discharge. The simulation results at a grid size of 50 m show a good correlation between measured and simulated daily flows at Hengtangcun station with Nash-Suttcliffe efficiency larger than 0.75 for both calibration and validation periods. In contrast, the model performs slightly worse at Fanjiacun station. The increasing grid size affects the characteristics of the slope and land use aggregation and causes important information loss. The aggregation of input data does not lead to significant errors up to a grid of 1 km. Model efficiencies decrease slightly with cell size increasing, and more significantly up to the grid size of 1 km.
url http://www.adv-geosci.net/21/131/2009/adgeo-21-131-2009.pdf
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