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Analysing the effect of land use/cover changes at sub-catchment levels on downstream flood peaks : a semi-distributed modelling approach with sparse data.

机译:分析子流域水平的土地利用/覆盖变化对下游洪峰的影响:一种稀疏数据的半分布式建模方法。

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摘要

This paper aims to evaluate how varying degrees of land-use/cover (LULC) changes across sub-catchments affect a flood peak at the catchment outlet. The study site was the Konar catchment, a part of the upper Damodar Basin in eastern India. A HEC-HMS model was set up to simulate rainfall–runoff processes for two LULC scenarios three decades apart. Because of sparse data availability at the study site, we used the Natural Resource Conservation Service (NRCS) curve number (CN) approach to account for the effect of LULC and soil on the hydrologic response of the catchment. Although a weak (r = 0.53) but statistically significant positive linear correlation was found between sub-catchment wise LULC changes and the magnitude of the flood peak at the catchment outlet, a number of sub-catchments showed marked deviations from this relationship. The varying timing of flow convergence at different stream orders due to localised LULC changes makes it difficult to upscale the conventional land-use and runoff relationship, evident at the plot scale, to a large basin. However, a simple modelling framework is provided based on easily accessible input data and a freely available and widely used hydrological model (HEC-HMS) to check the possible effect of LULC changes at a particular sub-catchment on the hydrograph at the basin outlet.
机译:本文旨在评估子集水区不同程度的土地利用/覆盖(LULC)变化如何影响集水区出口处的洪峰。研究地点是印度东部上达莫达盆地的一部分的科纳尔流域。建立了一个HEC-HMS模型来模拟相隔三十年的两个LULC情景的降雨-径流过程。由于研究地点的数据稀疏,因此我们使用自然资源保护服务(NRCS)曲线数(CN)方法来计算LULC和土壤对流域水文响应的影响。虽然在子集水区的LULC变化与集水口出口的洪峰幅度之间存在弱(r = 0.53),但在统计上具有显着的正线性相关性,但许多子集水区显示出与该关系的明显偏差。由于局部LULC的变化,在不同的水流阶上,水流收敛的时间变化,使得很难将传统的土地利用和径流关系放大到一个大盆地,这在地块尺度上很明显。但是,基于易于获得的输入数据和可自由获取且广泛使用的水文模型(HEC-HMS),提供了一个简单的建模框架,以检查流域出口处水文图上特定子汇水面积上LULC变化的可能影响。

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