地表水地下水耦合模型在大型山丘平原交错区的研发与应用
A coupled surface water-groundwater model and its application in a large-scale hill-plain region
注：图a中上面部分为降水量,下面为降水入渗补给系数;图b中上面部分为总径流量,下面为基流指数。
地表水地下水耦合模型在大型山丘平原交错区的研发与应用 |
| 孙青言, 陆垂裕, 郭辉, 严聆嘉, 张博 |
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A coupled surface water-groundwater model and its application in a large-scale hill-plain region |
| SUN Qingyan, LU Chuiyu, GUO Hui, YAN Lingjia, ZHANG Bo |
| 图10 三江平原分区降水入渗补给系数和基流指数对比 注：图a中上面部分为降水量,下面为降水入渗补给系数;图b中上面部分为总径流量,下面为基流指数。 |
| Fig.10 Comparison of precipitation recharge coefficient and base flow index in different regions of the Sanjiang Plain |
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