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基于地貌学和水文学的流域汇流模型
引用本文:夏岑岭.基于地貌学和水文学的流域汇流模型[J].水文,1994(1):9-14.
作者姓名:夏岑岭
作者单位:合肥工业大学土木系
摘    要:流域汇流是一个三维水文学问题,主要依赖于流域的河网地貌和河槽动力特征。本文在地貌学和水文学研究基顾上建立了概念性的流域模型,模型参数可由地貌参数和河槽动力特征值推求,该模型是非线性模型,概念清楚,求解地较简便,且可用于缺乏水文资料地区的流域汇流计算。

关 键 词:地貌学  水文学  流域  汇流模型

A Watershed4 Flow Concentration Model Based on Geomorphology and Hydrology
Xia Cenling.A Watershed4 Flow Concentration Model Based on Geomorphology and Hydrology[J].Hydrology,1994(1):9-14.
Authors:Xia Cenling
Affiliation:Hefei University of Technology
Abstract:Watershed flow concentration is a three dimension hydrological phenomenon, mainly concerning with thelandforms in river network and dynamic characteristics in river channels. Based on the geomorphology andhydrology, this paper gives out a concept model, in which parameters are compulated with the geomorphologicparameters and dynamic characteristic values of river channel. As a nonlinear model with clear concept, it is notonly simple for computation, but also can be used for the computation of watershed flow concentration inungaged basins.
Keywords:watershed flow concentration model  geomorphology  hydrology  physical prototype
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