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爱尔兰水文专家 J.E 纳希教授1978年来华讲学时介绍了延迟演算模型和线性水库模型(称为纳希瞬时单位线)。为了检验这两个流域汇流计算的数学模型对我国山区暴雨河流的适用性和运用方法,我们选用青衣江罗坝水文站以上的资料进行分析研究。流域面积为10799平方公里,位于暴雨区,共选了十一次大小不同的典型洪水进行分析,还对两个模型作了多种应用方式的探讨。发现如果不划分地表与地下径流,直接用总的出流过程进行计算,效果
Irish hydrologist J. E. Nash introduced the Delayed Calculus Model and Linear Reservoir Model (called Nathan Instantaneous Unit Line) when he spoke in China in 1978. In order to test the applicability and application of the mathematical model of confluence calculation in the two basins to the rainstorm rivers in mountainous areas in China, we selected the above data from the Jiangluoba Hydrological Station in Qingyi for analysis and research. Basin area of 10,799 square kilometers, located in the heavy rain area, selected a total of eleven different times the size of the typical flood analysis, but also for a variety of applications for two models to explore. Found that if you do not divide the surface and subsurface flow, directly with the total outflow process to calculate the effect