RT - TY - Jour YR - 2015-10-24 JF - 当前世界环境Jo - SP - Op - Vo - 30是 - 33 UL - www.a-i-l-s-a.com/article/842 / do - 10.12944 / cwe.10.3。31 N2 - 影响地下水充值的气候变化的估计有助于为盆地制定未来的地下水开发和管理计划计划。它对农业以及其他资源规划也将有所帮助。也可以判断裁剪模式所需的转变。该研究是为Shefrunji River盆地开展的，面积为5646.98 km2。整个区域被发现由17个流域组成。评估了3种不同方法对降雨，径流和估计地下水充电的气候变化的影响。地下水补给水分从3.11％达49.28％，0％〜15.34％，水平，克里希纳·饶（1970）和水台式变异分别降雨量为0％至15.34％和0.72％至14.62％。气候变化影响利于17分水岭中的6个中的6个，在17个流域中的6个中增加了降雨量，而在17分水岭中有5个。降雨和径流受到盆地上部北部北部的气候变化和盆地中部最南端的影响。 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. ER -