采用 SWAT 模型对查谟和克什米尔杰鲁姆河进行水文和泥沙产量分析

Dr. Bashir Ahmad Pandit
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引用次数: 0

摘要

摘要:杰赫勒姆河发源于查漠和克什米尔联邦领地西部克什米尔地区的印控部分,位于弗纳格,源于一处深泉。河流流经克什米尔谷地,从皮尔潘贾尔山脉北坡向西北蜿蜒流向斯利那加的伍拉尔湖,该湖调节着河流的流量。杰赫勒姆河从湖中流出,向西流去,形成一条两侧几乎垂直的河谷,在约 7000 英尺(2100 米)的深处穿过皮尔潘贾尔山脉。杰赫勒姆河在穆扎法拉巴德附近与基桑加河汇合,穆扎法拉巴德是巴控克什米尔地区阿扎德-克什米尔的行政中心。杰赫勒姆河从这里向南弯曲,形成西面巴基斯坦开伯尔-普赫图赫瓦省和东面阿扎德-克什米尔之间的部分边界。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrology and Sediment Yield Analysis in the Jehlum River in Jammu & Kashmir, Employing the SWAT Model
Abstract: The Jhelum originates in the Indian-administered part of the Kashmir region, in western Jammu and Kashmir union territory, in Vernag, from a deep spring. The river flows through the Vale of Kashmir and meanders northwest from the northern slope of the Pir Panjal Range to Wular Lake in Srinagar, which regulates its flow. The Jhelum emerges from the lake and flows west, forming a valley with nearly perpendicular sides that passes the Pir Panjal at a depth of around 7,000 feet (2,100 meters). The Jhelum meets the Kishanganga River near Muzaffarabad, the administrative hub of Azad Kashmir in the Pakistani-administered region of Kashmir. From there, it bends southward, forming a portion of the border between Khyber Pakhtunkhwa province, Pakistan, to the west, and Azad Kashmir to the east
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