Willybrordus Kurniawan Hima, I. M. Udiana, Judi K. Nasjono
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摘要

由于降雨量少,帝汶登加西拉丹(TTS)摄政的每个分区相对不均匀。它导致一些河流在旱季容易干旱。本研究旨在确定最大的干旱指数和地图干旱分布在南中帝汶(TTS)摄政。干旱指数分析采用标准化降水指数(SPI)法。使用的数据是10个雨站10年(2009-2018)的月降雨量数据。然后,利用ArcGIS软件绘制干旱分布雨量图。干旱指数分析结果显示,1个月亏缺期干旱指数最大,为-3.61,发生在2014年3月的鄂甘姆雨站。3个月亏缺期最大干旱指数为-3.19,分别出现在2010年3月的空雨站和2015年11月的Kesetnana雨站。干旱分布图研究结果表明,在1个月的缺水期,所有街道均在1月、2月和4月发生干旱。同时,在3个月缺水期,各区仅在6月平均发生干旱。
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Analisis Indeks Kekeringan Menggunakan Standardized Precipitation Index (SPI) Method pada Daerah Kabupaten Timor Tengah Selatan
Due to the low rainfall, it is relatively uneven in each sub-district in Timor Tengah Selatan (TTS) Regency. It causes some rivers to be drought-prone in the dry season. This study aims to determine the largest drought index and map the drought distribution in the South Central Timor (TTS) Regency. The drought index analysis uses the Standardized Precipitation Index (SPI) Method. The data used is monthly rainfall data for ten years (2009-2018) of ten rain stations. Then, mapping of drought distribution rainfall using ArcGIS Software. The results of the drought index analysis showed that in the 1-month deficit period, the largest drought index was -3.61, which occurred in March 2014 at the Oeekam Rain Station. In the 3-month deficit period, the largest drought index was -3.19, which occurred in March 2010 at the Nulle Rain Station and in November 2015 at the Kesetnana Rain Station. The findings of the drought distribution map study suggest that during the 1-month shortfall period, all sub-districts experienced drought in January, February, and April. Meanwhile, in the 3-month deficit period, drought occurs evenly for all sub-districts only in June.
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