@article{CWE/842/2017，作者={}，期刊={当前世界环境}，出版商={}，标题={印度古吉拉特邦Shetrunji盆地受气候变化影响的地下水资源。}，年={}，月= {}，volume = {30}， url = {www.a-i-l-s-a.com/article/842/}， pages ={994-1003}，摘要={估计气候变化对地下水补给的影响将有助于制定流域地下水开发和管理规划的未来计划。这也将有助于农业和其他资源规划。还可以判断种植方式需要的转变。这项研究是针对面积为5646.98平方公里的Shetrunji河流域进行的。整个地区由17个分水岭组成。评价了气候变化对降雨、径流和地下水补给的影响。地下水补给占降雨量的比例分别为3.11% ~ 49.28%、0% ~ 15.34%和0.72% ~ 14.62%。Krishna Rao(1970)和地下水位变化。在17个流域中，气候变化的影响有利于6个流域的降雨量显著增加，而在17个流域中，5个流域的径流量显著增加。流域上游北部和中游最南端的降水和径流受气候变化的影响。 The area weighted rainfall of the Shetrunji river basin was found increasing significantly. The areal mean depth of monsoon runoff for entire Shetrunji basin was increasing significantly at the rate of 17.7 mm per decade. The groundwater recharge assessed by water balance method was found higher as compared to Krishna Rao (1970) and water level fluctuation method. The groundwater recharge expected by water balance, Krishna Rao (1970) and water level fluctuation methods is found to be enlarged in 13, 9 and 6 watersheds out of 17 watershed of the basin. The areal mean depth of groundwater recharge in Shetrunji basin during monsoon season in water level fluctuation method was found increasing significantly at the rate of 13.01 mm per decade due to climate change impacts. }, number = {33}, doi = {10.12944/CWE.10.3.31} }