Probability of occurrence of drought in relation to rainfed rice productivity in the old alluvial region of West Bengal

Naffees Gowsar SR, Arunava Ghosh, Manoj Kanti Debnath, Sankalpa Ojha, Parthendu Poddar, Nishtha Pradarshika Rai
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Abstract

Climate change makes conditions suitable or unsuitable for growing crops in different regions. The greatest threat posed by climate change is change in monsoon. A period of drought is defined by low average precipitation, poor rain or higher evaporation rates which reduces crop growth and yield. In this study, an attempt was made to characterize agricultural drought with the help of rainfed rice crop yield rate and rainfall. Rainfall data and rainfed rice or Aman rice yield rate data from 1978 to 2020 of Malda district in West Bengal were analyzed for determining the probability of rainfed rice specific drought in Malda. An amount of 36.3 mm rainfall for three consecutive weeks was identified as drought threshold value in the test location. The recurrence of drought for the study area has also been studied.
西孟加拉邦老冲积区旱情发生的概率与雨养水稻产量的关系
气候变化使不同地区的条件适合或不适合种植作物。气候变化带来的最大威胁是季风的变化。干旱期的定义是平均降水量低、雨量少或蒸发率高,这会降低作物生长和产量。本研究尝试利用旱作水稻产量和降雨量对农业干旱进行表征。分析了西孟加拉邦马尔达地区1978 ~ 2020年的降雨资料和旱作稻或阿曼稻的产出率资料,以确定马尔达旱作稻发生特异性干旱的概率。将连续三周36.3 mm的降雨量确定为试验地点的干旱阈值。本文还对研究区干旱的再次发生进行了研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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