Assessment of Meteorological Drought using Standard Precipitation Index (SPI) in Western Maharashtra, India

A. Bhagat, S. Gorantiwar, V. Malunjkar
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Abstract

The crop production in rainy season in rainfed areas is dependent on vagaries of monsoon and is adversely influenced. The knowledge of different rainfall characteristics such as onset and withdrawal of monsoon, dry spell and drought would enable the optimal crop planning and implementation of protective irrigation strategies, thus mitigating the adverse impact of uncertainties of rainfall. The assessment of drought is one of the most important steps in risk management of drought analysis. The basis of drought indices is often based on measuring the deviation of precipitation values from long-term mean, during a specific period of time. The standard precipitation index (SPI) can be used for indicating the associated temporal and spatial variations. The aim of this research is the assessment of the characteristics such as intensity of meteorological drought using SPI with 12 months time scales in Western Maharashtra, India. The index has been computed in with 12 months time scales for 105 stations with 30 years record period in the study area and evaluated for the recent drought during 1983-2012. The results indicate that the rainfall pattern of Western Maharashtra exhibits non-uniform, irregular and erratic pattern of rainfall, as evidenced from SPI values. The meteorological drought shifted one step towards severity of drought condition for the time scales (month 1-12) i.e. from extremely wet to very wet; very wet to moderately wet; moderately wet to near normal; near normal to moderately dry; moderately dry to severely dry and severely dry to extremely dry condition.
用标准降水指数(SPI)评价印度马哈拉施特拉邦西部气象干旱
在雨季,雨养地区的作物生产依赖于季风的变幻莫测,并受到不利影响。了解不同的降雨特征,如季风的开始和结束、干旱期和干旱,将有助于制定最佳作物规划和实施保护性灌溉战略,从而减轻降雨不确定性的不利影响。干旱评估是干旱分析风险管理的重要环节之一。干旱指数的基础通常是在特定时期内测量降水值与长期平均值的偏差。标准降水指数(SPI)可用于指示相关的时空变化。本研究的目的是利用SPI对印度西部马哈拉施特拉邦12个月时间尺度的气象干旱强度等特征进行评估。该指数以12个月的时间尺度计算了研究区105个台站30年的记录期,并对1983-2012年的近期干旱进行了评价。结果表明,马哈拉施特拉邦西部降水模式表现出不均匀、不规则和不稳定的降水模式。气象干旱在时间尺度上(1-12月)向干旱严重程度转移了一步,即从极湿到极湿;非常潮湿到中度潮湿;中度湿润至接近正常;接近正常到中度干燥;中度干燥到严重干燥,严重干燥到极度干燥。
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