水文集中时间的数值近似

Q3 Energy
J. R. Fernández, C. Calvo-Jurado
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引用次数: 0

摘要

浓缩时间,即一滴水从流域最远的点表面移动到出口点所需的时间,是水文分析的一个基本参数。许多研究提出了计算浓缩时间的经验公式。其中最著名的是Temez公式,该公式基于西班牙地区小于3000公里的账户收集的时间序列数据。与许多作品一样,该表达式使用主河道长度作为参数,因为小斜坡由起点和终点之间的地理坐标之间的距离近似,导致较大的集水区和斜坡的方法具有高误差。在这项工作中,通过对曲线进行适当的离散化,通过多项式插值方法,我们改进了主通道长度的计算,从而为使用Temez表达式计算集中时间提供了一种更可靠的方法。用不同的数值算例对所提出的方案进行了说明,并与其他方法的结果进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical approximation of the hydrological time of concentration
The time of concentration, that is the time it takes for a single "drop of water" to move superficially from the most distant point of the watershed to the exit point, is a fundamental parameter of the hydrological analysis. Many studies have been conducted to propose empirical formulas to calculate the time of concentration. One of the best known is the Temez formula based on time series data collected in accounts in Spain with areas of less than 3,000 km. This expression uses the main channel length as a parameter as in many works, for small slopes is approximated by the distance between the geographic coordinates between the starting and ending points, leading for larger catchments and slopes to approaches with a high error. In this work, using a proper discretization of the curve, by using polynomial interpolation methods, we improve the calculation of the length of the main channel and therefore, we provide a more reliable method for calculating the time of concentration using the Temez expression. We illustrate the proposed scheme with different numerical examples comparing the results with those provided by other methods.
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来源期刊
Journal of Energy Systems
Journal of Energy Systems Environmental Science-Management, Monitoring, Policy and Law
CiteScore
1.60
自引率
0.00%
发文量
29
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