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首页> 外文期刊>Arabian journal of geosciences >Dam-induced changes in flood hydrology and flood frequency of tropical river: a study in Damodar River of West Bengal, India
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Dam-induced changes in flood hydrology and flood frequency of tropical river: a study in Damodar River of West Bengal, India

机译:大坝诱发的热带河流洪水水文和洪水频率变化:印度西孟加拉邦达莫达河的一项研究

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摘要

The Damodar River of West Bengal is popularized as 'Sorrow of Bengal' due to massive unpredictable destruction in the monsoonal floods, recorded since 1665. After establishment of Damodar Valley Corporation (DVC) of India in 1948, Tilaiya, Tenughat, Konar, Maithon and Panchet dams (Jharkhand) and Durgapur barrage (West Bengal) are built to regulate flood flow to a certain limit. But, as the floods were unpredictable in pre-dam phase, even now, lower Damodar Basin is not secure from the monsoonal floods. To assess the flood risk and nature of flood discharge, we have focused here to fit extreme value distribution (EVD) to the annual peak flow of the Damodar River using mainly Gumbel and log Pearson type III distributions. Pre-dam (1934-1957) and post-dam (1958-2007) flood frequency analysis has significantly projected maximum probable flood discharge of Damodar at Rhondia with a certain return period of occurrence, and it provides an idea about future flood risk in lower Damodar Basin.
机译:自1665年以来,由于季风洪水中发生了无法预测的大规模破坏,西孟加拉邦的达莫达河被普遍称为“孟加拉之苦”。1948年,印度达莫达河谷公司(DVC)成立后,蒂拉耶,特努哈特,科纳尔,梅森和建立Panchet大坝(贾坎德邦)和Durgapur拦河坝(西孟加拉邦)是为了将洪水流量调节到一定限度。但是,由于洪水在大坝前期是不可预测的,因此即使在现在,下达莫达盆地也无法摆脱季风性洪水。为了评估洪水的风险和洪水的性质,我们在这里集中讨论了极值分布(EVD)与Damodar河的年峰值流量的拟合,主要使用Gumbel和log Pearson III型分布。大坝发生前(1934-1957年)和大坝发生后(1958-2007年)的洪水频率分析已显着地预测了罗迪亚Damodar的最大可能洪涝流量,并有一定的返还期,并为未来较低的洪水风险提供了一个思路。达莫达盆地。

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