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• W4382896721 endingPage "744" @default.
• W4382896721 startingPage "735" @default.
• W4382896721 abstract "Drought is a regional phenomenon that is naturally affected by climate conditions. Climate change, which changes the pattern of rainfall and temperature, is very influential on the drought conditions in an area. Yogyakarta Province is one of the regions in the south of Indonesia with a distinctive regional character. By using rainfall data and the Palmer Drought Severity Index (PDSI) from 1958 to 2019, it can be shown that there is a change in the potential for two drought periods of 30 years for five districts in Yogyakarta Province. Changes are distinguished for the December–January–February period (DJF) which represents the wet season, and the June–July–August period (JJA), which represents the dry season. The results of the data analysis have shown an increase in rainfall for the wet season and a decrease in rainfall in the two periods. However, an increase in rainfall during the wet season does not mean that there has been a decrease in the level of drought. PDSI data for the first period showed an opportunity for an index of more than four by 21.55% for Bantul, 38.87% for Gunung Kidul, and 39.85% for Yogyakarta City, 39.63% for Kulon Progo, and 39.49% for Sleman. This figure has increased for Bantul in the second period, but for other districts, it has increased. This indicates that the data increase in rainfall that occurred, accompanied by an increase in temperature and evapotranspiration, causes the level of drought continues to increase. If this trend persists, there will be indications that rainfall in DIY will increase during the DJF season, but the potential for drought will continue." @default.
• W4382896721 created "2023-07-03" @default.
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• W4382896721 date "2023-01-01" @default.
• W4382896721 modified "2023-09-23" @default.
• W4382896721 title "The Impact of Climate Change on Meteorological Drought in Yogyakarta" @default.
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• W4382896721 doi "https://doi.org/10.1007/978-981-19-9768-6_68" @default.
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