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Spatiotemporal distribution and prediction of groundwater level linked to ENSO teleconnection indices in the northwestern region of Bangladesh

机译:孟加拉国西北地区ENSO遥控指标与地下水位的时空分布与预测

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This study aims to investigate spatiotemporal trends and magnitudes of groundwater level for the period of 1981-2017 in the northwestern region of Bangladesh and to predict the groundwater level changes from 2018 to 2025 through autoregressive integrated moving average (ARIMA) modeling. The study explores the relationship between groundwater level and El-Nino Southern Oscillation (ENSO) teleconnection indices during 1981-2017 in the study area. Results of MMK (Modified Mann-Kendall) Z statistics showed a significant downward trend of groundwater level (p<0.05), and the years 1994, 2002, 2004, 2006 and 2007 were the trend turning points of groundwater level depletion identified by Pettitt's test. The overall decreasing rates of groundwater level vary from 0.1 to 1.3 (m/decade). Wavelet spectrum was employed to show the temporal distribution patterns of groundwater level, suggesting a prolonged drought period in Rangpur subregion of northwestern Bangladesh. The Pearson correlation and cross-correlation results revealed that there was a weak relation between ENSO indices and groundwater level due to less anthropogenic influence in the study area. The outcomes of ARIMA model were consistent with MMK test trend analysis which predicted a similar downward tendency of groundwater level from 2018 to 2025, indicating an alarming situation, especially for Rajshahi subregion (0.8 m/decade). Overall, all the test results indicate a strong concurrence relationship among them. The results of the study recommend the need for rainwater harvesting during monsoon season, multi-disciplinary groundwater researches and monitoring programs as measures for future sustainable groundwater management on northwestern Bangladesh.
机译:本研究旨在调查孟加拉国西北部地区1981 - 2017年地下水位的时空趋势和地下水位的大小,并通过自回归综合移动平均(ARIMA)建模来预测2018年至2025年的地下水位变化。该研究探讨了地下水位和EL-NINO SOREHENTH振荡(ENSO)电信连接指数在研究区内的关系。 MMK(改进的Mann-Kendall)Z统计结果表明,地下水位(P <0.05)的显着下降趋势,1994年,2002年,2004年,2006年和2007年是Pettitt测试所确定的地下水位耗尽的趋势转折点。地下水位的总体下降率从0.1到1.3(米/十年)不同。小波谱被用来展示地下水位的时间分布模式,孟加拉国西北地区的牧场次区域延长了干旱期。 Pearson相关性和互相关结果表明,由于研究区内的人为影响,ENSO指数和地下水位之间存在薄弱关系。 ARIMA模型的结果与MMK测试趋势分析一致,预测2018年至2025年的地下水位的类似下行趋势,表明令人震惊的情况,特别是对于拉贾莎利次区域(0.8米/十年)。总体而言,所有测试结果表明它们之间的强劲并发关系。研究结果建议在季风季节,多学科地下水研究和监测计划中雨水收获,作为孟加拉国西北部未来可持续地下水管理的措施。

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