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TOPMODEL for Streamflow Simulation of a Tropical Catchment Using Different Resolutions of ASTER DEM: Optimization Through Response Surface Methodology

机译:TOPMODEL用于使用不同分辨率的ASTER DEM的热带流域水流模拟:通过响应面法进行优化

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摘要

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.
机译:无法获得适当的水文数据质量,再加上大多数基于物理的水文模型的复杂性,限制了对降雨-径流关系的研究,特别是在热带地区。在本文中,已尝试使用从免费的基于30 m的ASTER影像生成的DEM的不同分辨率作为基于地形的水文(TOPMODEL)模型的主要输入,以模拟位于热带地区的中等集水区的径流。应用响应面方法(RSM)来优化用于流模拟的最敏感参数。 30至300 m的DEM分辨率已用于评估其对地形指数分布(TI)和TOPMODEL模拟的影响。发现随着分辨率从30到300 m的变化,更改DEM分辨率会降低TOPMODEL仿真性能。研究得出的结论是,与重新采样的DEM相比,ASTER 30 m DEM可用于对数据稀缺的热带流域进行合理的水流模拟。

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