POTENSI BANJIR BANDANG MENGGUNAKAN ANALISIS MORFOMETRI DI DAERAH ALIRAN SUNGAI KLAGISON KOTA SORONG

Anif Farida, Mierta Dwangga
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Abstract

Flash flood is water level increases rapidly in the river beyond flood level and occurs due to extreme weather. It's happened quickly without warning. The Klagison Watershed in Sorong City has grown rapidly and often had flooded. Settlements dominate almost on watershed areas and there are many hills that are deforested due to mining activities upstream. This study aims to examine the morphometric conditions and to analyze the spatial distribution of the potential flash flood in the Klagison Watershed of Sorong City based on morphometric analysis. GIS is used to obtain morphometric parameters such as linear, relief and aerial parameters. The correlation coefficient between each morphometric parameter was calculated using Pearson Correlation. Determination of potential flash flood areas using the priority zone formula. The result shows that the Klagison watershed has high erosion potential and large runoff based on morphometric analysis. This can be seen in the high value of the texture ratio (T) and low Constant channel maintenance (C) so that the runoff volume is also large. The Lof value in all sub-watersheds is small, which means that surface runoff will quickly to the channel. The flash flood potential in the Klagison watershed is very low (Sub-watershed 1 and Sub-watershed 5), moderate (Sub-watershed 3 and Sub-watershed 4), high (Sub-watershed 2) and very high (Sub-watershed 6 and Sub-watershed 7). It means that Sub-watershed 2, Sub-watershed 6 and Sub-watershed 7 need management priorities related to disaster mitigation. Keywords: flash flood; morphometry; watershed
利用SORONG镇KLAGISON河流域的形态分析,可能会引发洪水
山洪是指由于极端天气导致的河流水位迅速上升超过洪水水位。这一切发生得太快,没有任何预兆。索龙市的克拉格森流域发展迅速,经常发生洪水。住区几乎在流域地区占主导地位,由于上游的采矿活动,许多山丘被砍伐。基于形态计量学分析,研究了索容市克拉格森流域潜在山洪暴发的形态计量条件,并对其空间分布进行了分析。利用地理信息系统(GIS)获取地形参数,如线形参数、地形参数和航空参数。采用Pearson相关法计算各形态计量参数之间的相关系数。使用优先区域公式确定潜在的山洪暴发区域。基于形态计量学分析的结果表明,克拉格森流域具有较高的侵蚀潜力和较大的径流量。这可以从纹理比(T)的高值和恒定通道维持(C)的低值中看出,因此径流量也很大。所有子流域的Lof值都很小,这意味着地表径流会很快流入河道。Klagison流域的山洪暴发潜力为极低(分流域1和分流域5)、中等(分流域3和分流域4)、高(分流域2)和极高(分流域6和分流域7)。这意味着分流域2、分流域6和分流域7需要与减灾相关的优先管理。关键词:山洪暴发;形态测量学;分水岭
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