Spatiotemporal variability of rainfall linked to ground water level under changing climate in northwestern region, Bangladesh

Fatematuz Zannat, A. Islam, M. A. Rahman
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引用次数: 19

Abstract

Bangladesh is one of the most climatic hazard-prone countries in the world. Rainfall in Bangladesh is highly variable which depends on each season and location. This study aims to investigate spatiotemporal variability of rainfall linked to groundwater level under changing climate in the northwestern region, Bangladesh during the period of 1976-2016 using rainfall and groundwater level data. A number of statistical approaches such as Mann-Kendall (MK) test, linear regression model, Sen’s slope estimator and Spearman’s rho (SK) test, Coefficient of Variation (CV) were employed to reveal trends and variability of rainfall and groundwater level. Additionally, wavelet transform was applied to assess temporal variability of rainfall time series in the northwestern region, Bangladesh. The results show that the annual rainfall variability was the highest in the Ishwardi station (25.39%) and the lowest was found in Rajshahi (20.70%). The MK test results reveal that the trends of annual and seasonal rainfall decreased gradually, where the highest significant decreasing trend of annual rainfall was found in Rajshahi (-2.976 mm/year) and the lowest decreasing trend was found in Syedpur (-1.278 mm/year). Furthermore, monsoon and winter seasons represent the decreasing trends of rainfall for all the stations. The results of wavelet analysis demonstrate that the monthly rainfall variance of average rainfall in the northwestern region was low from the period of 2006 to 2014, indicating the dry years. The annual and seasonal rainfall trends in the northwestern region were decreased, particularly in the recent decade. The relationship between rainfall and groundwater level indicates that rainfall was decreased and the ground water level was also declining at the same time in the study region. Interestingly, it is observed that a significant high decreasing trend of annual rainfall is found in Rangpur but the annual groundwater level depth is less increased in Rangpur at the same time.
气候变化下孟加拉国西北地区降水与地下水位的时空变异
孟加拉国是世界上最容易发生气候灾害的国家之一。孟加拉国的降雨量变化很大,这取决于每个季节和地点。利用1976-2016年孟加拉国西北地区降水和地下水位数据,研究气候变化背景下降水与地下水位的时空变化特征。采用Mann-Kendall (MK)检验、线性回归模型、Sen’s斜率估计、Spearman’s rho (SK)检验、变异系数(CV)等统计方法揭示了降水和地下水位的变化趋势和变异性。此外,应用小波变换对孟加拉西北地区降雨时间序列进行了时间变率分析。结果表明:年降水变异率以伊什瓦迪站最高(25.39%),拉杰沙希站最低(20.70%);MK检验结果表明,年降水量和季节降水量的变化趋势呈逐渐减小的趋势,其中年降水量减少趋势最大的地区为拉杰沙希(-2.976 mm/年),减少趋势最小的地区为赛德普尔(-1.278 mm/年)。此外,季风和冬季代表了所有站点的降雨量减少趋势。小波分析结果表明,2006 ~ 2014年西北地区月平均降雨量方差较小,为干旱年;西北地区年、季降水趋势呈减少趋势,尤其是近10年。降水与地下水位的关系表明,研究区降水减少的同时,地下水位也在下降。有趣的是,Rangpur的年降雨量有明显的高减少趋势,但同时地下水位深度的年增加较少。
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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来源期刊
Central European Journal of Geosciences
Central European Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
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