由于降雨,新卡旺市洪水易发地区的分区

Fahrul Razi, S. Soeryamassoeka, Eko Yulianto
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引用次数: 2

摘要

新卡旺市是一个沿海和丘陵城市。洪水事件造成了相当大的物质损失、人民流离失所和生命损失。新加坡卡旺几乎每年都会发生洪水。总的来说,新卡旺的洪水是由自然因素引起的,异常高的降雨量。考虑到洪水对新卡旺市发展的重大影响,有必要建立基于城市降雨量的洪水易损性分区。通过对土地坡度、高程、土壤类型、土地覆被、降雨数据水文分析等影响洪水事件的参数进行分析,绘制Singkawang市洪水易损性分区图。然后,对影响洪水的四个参数进行叠加,得到基于降雨的水文分析生成的最大计划洪流量(Q)导致的洪水分布地图。基于4个影响洪水事件的数据参数的洪水易损性图分析结果表明,新加坡卡旺市洪水安全区域面积为14863.97 ha(27.04%)。相比之下,不易发生洪水的地区面积为24571.74公顷(44.70%)。易发洪涝地区面积11476.22 ha(20.87%),高发洪涝地区面积3567.28 ha(6.49%)。根据基于降雨的水文分析结果得出,新加坡卡旺市大部分地区遭受淹没的原因是,小塞美拉吉河区最大计划泄洪间隔为2年(353.5 ha),小塞美拉吉河区间隔为5年(327.4公顷),塞拉高河区间隔为10年(401.4公顷),塞拉高河区间隔为20年(473.1公顷)。在塞拉考河地区(545.9公顷)间隔50年,在塞拉考河地区(617.7公顷)间隔100年。
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ZONING OF FLOOD PRONE AREAS IN SINGKAWANG CITY DUE TO RAINFALL
Singkawang City is a coastal and hilly city. Flooding incidents have caused considerable material damage, displacement of people, and loss of lives. Floods in Singkawang occur almost yearly. In general, the floods in Singkawang are caused by natural factors, exceptionally high rainfall. Considering the significant impact of floods on the development of Singkawang City, it is necessary to establish flood vulnerability zoning based on rainfall in the city.An analysis is conducted on parameters that influence flood incidents, including the slope of the land, elevation, soil type, land cover, and hydrological analysis of rainfall data to create a flood vulnerability zoning map in Singkawang City. Then, an overlay is performed on the four parameters that affect floods, resulting in a map showing the distribution of inundation due to the maximum planned flood discharge (Q) generated from the hydrological analysis based on rainfall.The flood vulnerability map analysis results based on 4 data parameters that affect flood events obtained that the flood-safe area in Singkawang City covers an area of 14863.97 ha (27.04%). In contrast, areas not prone to floods cover 24571.74 ha (44.70%). Areas vulnerable to floods cover 11476.22 ha (20.87%), and regions highly vulnerable to floods cover 3567.28 ha (6.49%). Based on the results of hydrological analysis based on rainfall, it is obtained that the area of Singkawang City mostly experiences inundation due to the maximum planned flood discharge occurring at a 2-year interval in the Small Semelagi River Zone (353.5 ha), at a 5-year gap in the Small Semelagi River Zone (327.4 hectares), at a 10-year gap in the Selakau River Zone (401.4 ha), at a 20-year interval in the Selakau River Zone (473.1 ha), at a 50-year interval in the Selakau River Zone (545.9 ha), and at a 100-year gap in the Selakau River Zone (617.7 ha).
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