The Effects of El Nino Southern Oscillation on Rainfall in the Karst Area of Maros, National Park Bantimurung Bulusaraung South Sulawesi and its Impact on Flood Disasters

Muhammad Arsyad, Fitriani Fitriani, V. A. Tiwow, P. Palloan, Sulistiawaty Sulistiawaty, Agus Susanto
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Abstract

The aims of this study were to describe rainfall profiles, to analyze the effect of the El Nino Southern Oscillation (ENSO) on rainfall and its impact on flood disasters in the karst area of Maros, National Park Bantimurung Bulusaraung South Sulawesi. The data used were monthly data of ENSO parameters and monthly data on rainfall of Karst Maros TN Babul area in the range of 2011-2020. The monthly data of ENSO parameters consist of Oceanic Nino Index (ONI) data, namely Nino Index 3.4 and Southern Oscillation Index (SOI) obtained from the official website of NOAA (National Oceanic and Atmospheric Administration) and from the official website of BOM (Bureau of Meteorology), respectively. Whereas, the monthly data of rainfall of Karst Maros TN Babul area was obtained from Maros Climatology Station, South Sulawesi. The data was analyzed (i.e. graph analysis and simple linear regression) using Microsoft Excel 2010 Software and ArcGIS Software for map creation. The results showed that the rainfall profile of the karst Maros TN Babul region for the period 2011-2020 has a monsoon rainfall pattern with the highest rainfall in December, January, and February, while the lowest rainfall occurs in June, July, and August. The significant effect of ENSO on rainfall in the Karst Maros TN Babul Area for the period 2011-2020 was categorized as a moderate with an ONI correlation coefficient value of 0.521 and SOI of 0.465. The effect of ENSO on rainfall is in the range from 25.9 to 33.1% which result in flood disasters in the karst Maros TN Babul area such as Bantimurung, Tompobulu, Camba, and Simbang districts. The flood disasters mostly occurs in January and December with rainfall intensity from high to very high category.
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厄尔尼诺南方涛动对南苏拉威西岛 Bantimurung Bulusaraung 国家公园马罗斯喀斯特地区降雨量的影响及其对洪水灾害的影响
本研究旨在描述降雨概况,分析厄尔尼诺南方涛动(ENSO)对降雨的影响及其对南苏拉威西岛班蒂穆隆-布卢萨拉恩国家公园马罗斯岩溶地区洪水灾害的影响。所使用的数据是 2011-2020 年期间厄尔尼诺/南方涛动参数的月度数据和喀斯特马罗斯 TN 巴布地区的月度降雨量数据。厄尔尼诺/南方涛动参数的月度数据包括海洋尼诺指数(ONI)数据,即尼诺指数3.4和南方涛动指数(SOI),分别从美国国家海洋和大气管理局(NOAA)官方网站和英国气象局(BOM)官方网站获得。喀斯特马罗斯 TN 巴布勒地区的月降雨量数据则来自南苏拉威西马罗斯气候站。数据使用 Microsoft Excel 2010 软件进行分析(即图表分析和简单线性回归),并使用 ArcGIS 软件绘制地图。结果表明,2011-2020 年期间,岩溶马罗斯 TN Babul 地区的降雨分布呈季风降雨模式,降雨量最高的月份为 12 月、1 月和 2 月,降雨量最低的月份为 6 月、7 月和 8 月。厄尔尼诺/南方涛动对喀斯特马罗斯 TN 巴布勒地区 2011-2020 年期间降雨量的明显影响被归类为中度影响,其 ONI 相关系数值为 0.521,SOI 为 0.465。厄尔尼诺/南方涛动对降雨的影响范围在 25.9%至 33.1%之间,导致岩溶马罗斯-TN-巴布勒地区(如班蒂穆隆、通博布鲁、坎巴和辛邦地区)发生洪水灾害。洪水灾害主要发生在 1 月和 12 月,降雨强度从高到非常高。
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