Pemodelan Numerik Hubungan Pola Curah Hujan Wilayah Equatorial di Pulau Sumatera Terhadap Fenomena ENSO dan IOD

Melly Ariska, Adam Darmawan, H. Akhsan, Supari Supari, Muhammad Irfan, Iskhaq Iskandar
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Abstract

A numerical modeling has been built for the relationship between rainfall in the equatorial region of Sumatra to the ENSO and IOD phenomena by taking data from 1991 to 2020 at three stations located in the western region of Sumatra Island, namely SM Japura, SM Minangkabau and SM Hang Nadim. The method used in this study is the method of correlation and linear regression on the Niño3.4 Index variable and the Dipole Mode Index on the amount of rainfall. The data visualization process is carried out with the output in the form of plots and graphs with Goole Colab coding. The resulting graph is a graph of the ENSO and IOD phenomena, as well as a regression graph between The Niño3.4, DMI and the amount of rainfall per month. This study was conducted with the aim of knowing how much influence the El Niño Southern Oscillation (ENSO) variable represented by the Niño3.4 Index and the Indian Ocean Dipole (IOD) represented by DMI had on rainfall in the equatorial region in the 1991 – 2020 period and to see the trend of significance between the two towards the equatorial region on the island of Sumatra. Rainfall in Indonesia's equatorial region tends to be influenced by IOD compared to ENSO. The combination of the two at the same time can cause a significant change in the amount of rainfall. La-Niña and negative IOD occurred in 1992, 1996, 1999, 2000, 2005, 2008, 2011 and 2016. The average rainy day index (SDII) tended to decrease in Japura Island in 1996, 2005, 2011, 2016 , at SM Minangkabau in 1992, 1996, 1999, 2000, 2016 and at SM Hang Nadim in 1996, 1999 and 2008. Meanwhile the longest series of wet days tended to decrease in SM Japura in 1992, 1996, 1999, 2005, in SM Minangkabau in 1992, 1996, 2005, 2008, and in SM Hang Nadim in 1992, 2000, 2005, 2008 and 2011. The longest series of dry days tended to increase in SM Japura in 1996, 2011, in SM Minangkabau in 1996, 2000, 2011, and at SM Hang Nadim in 1996.
利用1991 - 2020年苏门答腊岛西部SM Japura、SM Minangkabau和SM Hang Nadim 3个台站的资料,建立了苏门答腊岛赤道地区降雨与ENSO和IOD现象的关系的数值模拟。本研究采用的方法是对Niño3.4指数变量和偶极子模式指数对降雨量进行相关和线性回归的方法。数据可视化过程采用google Colab编码,以图形和图形的形式输出。得到的图是ENSO和IOD现象的图,以及Niño3.4、DMI和每月降雨量之间的回归图。本研究的目的是了解以Niño3.4指数为代表的厄尔Niño南方涛动(ENSO)变量和以DMI为代表的印度洋偶极子(IOD)变量对1991 - 2020年期间赤道地区降水的影响程度,以及两者之间对苏门答腊岛赤道地区的显著性趋势。与ENSO相比,印度尼西亚赤道地区的降雨更容易受到IOD的影响。两者同时结合会导致降雨量的显著变化。La-Niña和负IOD分别出现在1992年、1996年、1999年、2000年、2005年、2008年、2011年和2016年。1996年、2005年、2011年和2016年Japura岛、1992年、1996年、1999年、2000年和2016年米南卡保岛和1996年、1999年和2008年Hang Nadim岛的平均雨天指数(SDII)呈下降趋势。1992年、1996年、1999年、2005年日本、1992年、1996年、2005年、2008年米南卡保和1992年、2000年、2005年、2008年和2011年杭纳丁的最长连续湿日数呈减少趋势。1996年、2011年日本稻、1996年、2000年、2011年米南卡堡稻和1996年汉纳迪姆稻连续最长干旱日数呈增加趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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