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Effect of extreme rain and land covering change in Jatihandap on 20 March 2018 flash flood

机译:贾蒂汉达普的极端降雨和土地覆盖变化对2018年3月20日山洪的影响

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Flash flood occurred on March 20, 2018, in Jatihandap, Bandung City, West Java due to the overflow of Cipamokolan River. This has caused considerable losses, especially for people living in the area. The flood occurred due to high rainfall intensity and inadequate land covering, especially in the upstream area (North Bandung Region) where the area is filled with housing, villas, and open land. Consequently, the water catchment area decreases. The objective of this study is to identify flood discharge that occurs due to high rainfall intensity and land covering. Flood discharge is calculated using a rational method. Based on BMKG data, rain intensity on March 20, 2018, is 45 mm/hour. The results of this study show that with this intensity, the Cipamokolan River flow brings water with sediment and debris waste. The discharge of the river is 207 m3/s. It equals to 2.2 times river basin discharge and causing water to overflow into the land around the river. The debris flow also damage the levees in Jatihandap then it caused flash floods.
机译:由于Cipamokolan河的溢流,2018年3月20日在西爪哇省万隆市的Jatihandap发生了山洪暴发。这造成了相当大的损失,特别是对于居住在该地区的人们。洪水是由于高降雨强度和土地覆盖不足而引起的,尤其是在上游地区(北万隆地区),那里的房屋,别墅和空地都充满了。因此,集水面积减小。这项研究的目的是确定由于高降雨强度和土地覆盖而产生的洪水。洪水流量是使用合理方法计算的。根据BMKG数据,2018年3月20日的降雨强度为45毫米/小时。这项研究的结果表明,在这种强度下,Cipamokolan河的水流带来了沉积物和碎屑废物。河流流量为207 m3 / s。它等于流域流量的2.2倍,并导致水溢出到河周围的土地中。泥石流还破坏了贾蒂汉达普的堤防,继而引起山洪泛滥。

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