Statistical analysis of rainfall trend and its variability (1901–2020) in Kolkata, India

Pub Date : 2022-09-26 DOI:10.12775/bgeo-2022-0006
MD JUBER ALAM, A. Majumder
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Abstract

The current study focuses on the altering historical rainfall data analysis and its variability in Kolkata (Kolkata Municipal Corporation), a metropolitan city in India. The research area experiences detrimental urban floods (pluvial floods) at near-annual regularity during the monsoon, and during the pre-monsoon seasons it commonly experiences water shortage problems. Analysing trends and temporal variability of rainfall over 120 years from 1901 to 2020 is the main objective of this study. The original Mann–Kendall (M–K) test has been applied to the rainfall dataset in conjunction with Sen’s Slope Estimator using Python 3.10, after the Durbin-Watson (DW) statistic initially suggested that there is no serial correlation effect. The M–K test, with a Kendall’s tau of 0.17058 (significant at a 5% level), shows an upward trend in annual rainfall between 1901 and 2020. The Sen’s slope, which measures the rate of change annually, has a value of 2.48152. Regression analysis and other dispersion measures are also used in this study to investigate the monthly rainfall trend and its variability. The phase-wise (30-year) analysis of annual rainfall variability reveals a considerable variation over 120 years. While fitting the linear regression line month by month over the entire period, mostly negative trends were found in the pre-monsoon and positive trends in the monsoon and post-monsoon seasons. The findings of this analysis could be useful to urban planners for water supply and management in the study area. The primary concern of planners for effectively managing rainwater and the accompanying issues should be the growing variability of annual precipitation.
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印度加尔各答1901-2020年降水趋势及其变率的统计分析
目前的研究重点是印度大都市加尔各答(Kolkata Municipal Corporation)不断变化的历史降雨数据分析及其变异性。在季风期间,研究区几乎每年都会经历一次有害的城市洪水(雨洪),在季风前季节,它通常会经历缺水问题。本研究的主要目的是分析从1901年到2020年120年的降水趋势和时间变率。在Durbin-Watson (DW)统计数据最初表明没有序列相关效应之后,原始的Mann-Kendall (M-K)检验已与使用Python 3.10的Sen斜率估计器一起应用于降雨数据集。肯德尔τ值为0.17058(在5%水平上显著)的M-K检验显示,1901年至2020年的年降雨量呈上升趋势。衡量年变化率的森氏斜率的值为2.48152。本研究亦采用回归分析及其他离散度方法探讨月降水趋势及其变异。年降雨量变率的分阶段(30年)分析显示,在120年期间有相当大的变化。逐月拟合的线性回归线显示,季风前和季风后季节多为负趋势,季风前和季风后季节多为正趋势。这一分析的结果可能对研究地区的供水和管理城市规划者有用。规划人员对有效管理雨水及其相关问题的主要关注应该是年降水量的日益变化。
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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