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Determination of unit watershed size for use in small watershed hydrological modeling

机译:确定用于小流域水文模型的单位流域大小

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摘要

Since the uniform rainfall over the watershed is the most fundamental assumption in small watershed modelling, the limitation on watershed size should be investigated. This study defines the unit watershed size as a dimensinal criteron which is associated with the storm size, and the extent and frequency of storm exclusion ( called spatial and temporal errors). Two approaches of determining average storm cell radius were proposed. One is related with the spatial variation in storm rainfall (DSIP), while another considers both spatial variation and storm exclusion events (RVIP). Both analytical and empirical solutions are obtained and the effect of multiplestorm events is discussed. The storm radius for Walnut Gulch is determined as 4.6 miles which is close to others' results. Given storm radius, a relationship between unit watershed size and the spatial and temporal errors is developed analytically. Based on this relationship, both selection and evaluation of unit watershed size are made possible. If the error levels are known, then the proper watershed size can be selected and if the watershed size is given, then the error levels can be evaluated. By using unit watershed size, the models of small watersheds may be extended to those of large watersheds.
机译:由于在小流域建模中流域上的均匀降雨是最基本的假设,因此应研究对流域大小的限制。这项研究将单位分水岭的大小定义为与风暴大小,风暴被排除的程度和频率(称为空间和时间误差)相关的维二阶标准。提出了两种确定平均风暴单元半径的方法。一种与暴雨的空间变化(DSIP)有关,而另一种则考虑了空间变化和暴雨排除事件(RVIP)。获得了解析和经验解,并讨论了多暴风雨事件的影响。核桃峡谷的风暴半径确定为4.6英里,与他人的测量结果相近。在给定风暴半径的情况下,分析得出单位流​​域大小与时空误差之间的关系。基于此关系,可以选择和评估单位分水岭的大小。如果知道误差水平,则可以选择适当的分水岭大小,如果给出了分水岭大小,则可以评估误差水平。通过使用单位流域大小,可以将小流域的模型扩展到大流域的模型。

著录项

  • 作者

    Long Junsheng1956-;

  • 作者单位
  • 年度 1986
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

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