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SURFACE RUNOFF MODELLING IN STEEP TERRAIN IN A GIS ENVIRONMENT

机译:GIS环境中陡坡地表径流模拟

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摘要

The GIS implicit incorporation into hydraulic modelling is not yet a common practice. The attempts for introducing such approach may face definite problems, of which overcoming needs some new specific developments. Such specific approach has been discussed in this paper for the case of surface runoff modelling on steep terrain in the GIS environment. Crucial problem in this case is the velocity vectors transfer from their actual values, associated with the inclined planes of their origin, to a horizontal GIS layer. Equations (22), (44) and (45) are contributions in this respect and are an alternative to the usual approach of employing 1D Saint-Venant equations in hydraulic modelling in 2D space, which is incorrect in principal.
机译:将GIS隐式合并到水力模型中还不是一种普遍的做法。引入这种方法的尝试可能会遇到明确的问题,克服这些问题需要一些新的具体发展。本文针对GIS环境中陡峭地形上的地表径流建模情况讨论了这种特定方法。在这种情况下,最关键的问题是速度矢量从与它们的原点的倾斜平面相关联的实际值传递到水平GIS层。公式(22),(44)和(45)是这方面的贡献,并且是在二维空间水力建模中采用一维圣维南方程的常用方法的替代方法,这在原理上是不正确的。

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