Analysing spatio-temporal drought characteristics and copula-based return period in Indian Gangetic Basin (1901-2021)

被引:2
|
作者
Bera, Debarati [1 ,2 ]
Dutta, Dipanwita [1 ,2 ]
机构
[1] Vidyasagar Univ, Dept Remote Sensing, Midnapore, West Bengal, India
[2] Vidyasagar Univ, GIS, Midnapore, West Bengal, India
关键词
IMD precipitation data; SPI; VCI; Run theory; Copula theory; AGRICULTURAL DROUGHT; CLIMATE-CHANGE; VEGETATION; INDEX; VARIABILITY; SEVERITY; IMPACTS; CHALLENGES; PREDICTION; RAJASTHAN;
D O I
10.1007/s11356-024-32286-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Uncertainty and uneven distribution of monsoonal rainfall and its consequences on crop production is a matter of serious concern in India, specifically, in the Indo-Gangetic plain region. In this study, drought patterns were investigated through standardised precipitation index (SPI) of varying timescales, using the India Meteorological Department (IMD) precipitation data (1901-2021). We analysed the spatio-temporal pattern of different drought characteristics (frequency, duration, severity, intensity) of the Indian Gangetic basin using run theory. The bivariate copula method has been incorporated to combine two drought properties (severity and duration). Copula integrates multivariate distribution and considers the dependency rate among the variables. The five most widely used copulas from various copula families, elliptical (normal, t-copula) and Archimedean (Clayton, Gumbel, Frank), were estimated for modelling, and the best fit copula was selected. The study revealed that seasonal drought is more frequent and intense in the Upper and Middle Gangetic Plain, whereas annual drought is quite scattered in nature. It is worthy to mention that downward drought trends were observed in this agricultural belts significantly after 1965; specifically, in the Upper, Middle, and Trans Gangetic Plain regions. With increasing drought duration and severity, the drought return period raised, but the frequency decreased gradually. Most of the droughts characterised by less duration and severity occurred with a return period below 10 years for the whole region. The major 100 + years return period droughts were to be found after 1960 and their frequencies were significantly higher after 2000. The most recent remarkable droughts with more than 100 years of return occurred during 2008-2011 and 2016-2018 in the Upper and Middle Gangetic plains, whereas in the Lower Gangetic plain, a hundred-year return period drought was occurred during 2010-2013. This study provides agroclimatic-zones-wise significant information of drought characteristics and its nature of occurrence in the Indian Ganga Basin. The results enhance the understanding of drought management and formulation of adaptive strategies to mitigate the adverse impact of droughts.
引用
收藏
页码:22471 / 22493
页数:23
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