基于标准化降水指数(SPI)的孟加拉国北部干旱分析

R. Afrin, F. Hossain, S. Mamun
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引用次数: 10

摘要

干旱是指一个地区缺水的一段时间。本研究采用标准化降水指数(SPI)方法进行干旱分析。孟加拉国北部地区是研究区域。孟加拉国北部地区的月降雨量数据来自孟加拉国气象局。获得的降水数据为1991 ~ 2011年,2012 ~ 2026年的数值采用马尔可夫模型生成。利用干旱分析SPI公式计算1991 ~ 2026年的SPI值。SPI分析表明,孟加拉国北部地区的干旱从中度干旱到严重干旱,未来可能从中度干旱到严重干旱,但在某些情况下也可能发生极端干旱。研究发现,孟加拉国北部地区在1991年、1992年、1994年、1995年、1997年、1998年、2000年、2003年、2005年、2007年、2009年和2010年已经经历了严重干旱。该地区可能在2012年、2015年、2016年、2018年、2019年、2021年、2022年、2023年、2024年、2025年和2026年经历严重干旱,并在2012年、2014年、2016年、2023年和2024年经历极端干旱。j .包围。科学。与自然资源,11(1-2):199-216 2018
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Analysis of Drought in the Northern Region of Bangladesh Using Standardized Precipitation Index (SPI)
Drought is an extended period when a region notes a deficiency in its water supply. The Standardized Precipitation Index (SPI) method was used in this study to analyze drought. Northern region of Bangladesh was the area of study. Monthly rainfall data of northern region of Bangladesh was obtained from the Meteorological Department of Bangladesh. Obtained rainfall data was from 1991 to 2011 and values from 2012 to 2026 were generated using Markov model. Then SPI values from 1991 to 2026 were calculated by using SPI formula for analyzing drought. Analysis with SPI method showed that droughts in northern region of Bangladesh varied from moderately dry to severely dry conditions and it may vary from moderately dry to severely dry conditions normally in future but in some cases extreme drought may also take place. From the study, it is observed that the northern region of Bangladesh has already experienced severe drought in 1991, 1992, 1994, 1995, 1997, 1998, 2000, 2003, 2005, 2007, 2009 and 2010. The region may experience severe drought in 2012, 2015, 2016, 2018, 2019, 2021, 2022, 2023, 2024, 2025 and 2026 and extreme drought in 2012, 2014, 2016, 2023 and 2024. J. Environ. Sci. & Natural Resources, 11(1-2): 199-216 2018
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