上游流域和气候特征对坝后下游流量变化的影响评估:来自印度半岛的经验见解

Pub Date : 2023-11-24 DOI:10.1134/s0097807823600729
J. Sanyal
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引用次数: 0

摘要

摘要在科学文献中,水库规模和大坝运行是引起坝后下游水文曲线变化的主要原因。本研究探讨了上游流域和气候特征是否也有助于这种变化。通过对印度半岛18个站点的案例研究,我们采用多元线性回归(MLR)方法,将2个大坝相关因子和5个上游盆地的地球物理和气候因子作为预测因子,以确定关键影响因素。采用坝前和坝后水流持续时间曲线来表征坝后水流的变化。我们考虑了坝前和坝后降雨差异最小的时期,并消除了降雨对下游水文变化的影响。另外两种机器学习特征提取算法,如带有f_regression和互信息评分的SelectKBest,也被用于确定大坝后下游水文曲线变化的最具影响力的驱动因素。三种不同方法的结果提供了稳健和无偏的结果。三种方法一致认为,虽然大坝是典型季风流量峰值和总体流量变率变化的主要决定因素,但潜在蒸散量和以上游流域美国土壤保持服务曲线数(CN)为代表的土地利用-土壤-坡度也可能是影响坝后洪峰变化的关键因素。这些发现强调了在评估大坝建设对下游水文的影响时,考虑上游集水区的地球物理和气候特征的重要性,并可能有助于新建和现有水库的安置、大小和运行。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Assessing the Influence of Upstream Basin and Climatic Characteristics on Post-Dam Downstream Streamflow Changes: Empirical Insights from Peninsular India

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Assessing the Influence of Upstream Basin and Climatic Characteristics on Post-Dam Downstream Streamflow Changes: Empirical Insights from Peninsular India

Abstract

Size of the reservoir and dam operation are cited as the primary causes of changes in the post-dam downstream hydrograph in scientific literature. This study investigates whether upstream basin and climatological characteristics also contribute to such changes. Drawing upon the case study of 18 sites across Peninsular India, we employed Multiple Linear Regression (MLR) with two dam-related and five geophysical as well as climatological factors of upstream basins as predictors to determine key influencing causes. Pre- and post-dam flow duration curves were used to characterise changes in flow post dam construction. We considered periods with the least rainfall difference pre- and post-dam and eliminated rainfall’s effect on downstream hydrograph changes. Two additional machine learning feature extraction algorithms, such as SelectKBest with f_regression and mutual information score, were also deployed to identify the most influential driver of changes in the post-dam downstream hydrograph. The outcome of three separate methods provided a robust and unbiased result. The three methods agreed that while dams are the primary determinant of changes in the typical peak monsoon flow and overall flow variability, potential evapotranspiration and land use-soil-slope, represented by US Soil Conservation Service Curve Number (CN) of the upstream catchment, could also be key factors affecting changes in the post-dam flood peak. These findings highlight the importance of considering the geophysical and climatological characteristics of upstream catchments when assessing the impact of dam construction on downstream hydrology, and potentially aid in the placement, size, and operation of new and existing reservoirs.

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