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首页> 外文期刊>Indian journal of power and river valley development >Design storm studies over the Bhagirathi and the Dhauliganga river catchments in Uttranchal State
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Design storm studies over the Bhagirathi and the Dhauliganga river catchments in Uttranchal State

机译:Uttranchal州Bhagirathi和Dhauliganga河流域的设计风暴研究

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摘要

For all round developments of any region, knowledge of precipitation climatology is most essential. Large number of rainfall studies are available for plain area river basins. It is now essential to carry out such studies in the mountainous regions like the Garhwal Himalayan region where orography plays important role in rainfall distribution. These studies can be useful for planning and design of barrages to generate hydropower by storing surface runoff. The knowledge about space time distribution of precipitation is also useful for agricultural operations over hilly terrain where irrigation through a network of canals is not feasible as in plains. Moreover, knowledge of maximum precipitation is also required for the design of dams and drinking water tanks for villages in the interior of hilly terrain. In this paper, design storm studies have been carried out over the two catchments in Garhwal Himalayan region, viz. (a) the Bhagirathi up to Loharinag Pala (area 3316 km~2) and (b) the Dhauliganga up to Tapovan Vishnugad (area 3100 km~2) using rainfall data of about 73 stations around the study region for their available period from 1901. Standard projects storms (SPS) and probable maximum precipitation (PMP) rain depths were estimated by physical and statistical methods. Using SRRG data from nearby stations, lime distribution analysis has been carried out. The time distribution can be used to estimate design rain depths of shorter intervals
机译:对于任何地区的全面发展,最重要的是要有降水气候学知识。平原地区的流域可进行大量的降雨研究。现在至关重要的是,在诸如地形在降雨分布中起着重要作用的Garhwal喜马拉雅山等山区进行此类研究。这些研究对于通过存储地表径流来发电的拦河坝的规划和设计很有用。关于降水的时空分布的知识对于在丘陵地带的农业操作也很有用,因为在丘陵地带无法像平原那样通过运河网络进行灌溉。此外,对于丘陵地带内部村庄的水坝和饮用水水箱的设计,还需要最大降水知识。本文对设在加尔瓦尔·喜马拉雅地区的两个流域进行了设计风暴研究。 (a)Bhagirathi到Loharinag Pala(区域3316 km〜2)和(b)Dhauliganga到Tapovan Vishnugad(区域3100 km〜2),使用研究区域周围1901年以来可用期间的约73个气象站的降雨数据通过物理和统计方法估算标准项目的风暴(SPS)和可能​​的最大降水(PMP)雨深。利用附近车站的SRRG数据,进行了石灰分布分析。时间分布可用于估计较短间隔的设计雨深

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