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首页> 外文期刊>Journal of Hydrology >Precipitation areal-reduction factor estimation using an annual-maxima centered approach
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Precipitation areal-reduction factor estimation using an annual-maxima centered approach

机译:使用年度最大值中心法估算降水面积减少因子

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The adjustment of precipitation depth of a point storm to an effective (mean) depth over a watershed is important for characterizing rainfall-runoff relations and for cost-effective designs of hydraulic structures when design storms are considered. A design storm is the precipitation point depth having a specified duration and frequency (recurrence interval). Effective depths are often computed by multiplying point depths by areal-reduction factors (ARF). ARF range from 0 to 1, vary according to storm characteristics, such as recurrence interval; and are a function of watershed characteristics, such as watershed size, shape, and geographic location. This paper presents a new approach for estimating ARF and includes applications for the 1-day design storm in Austin, Dallas, and Houston, Texas. The approach, termed "annual-maxima centered," specifically considers the distribution of concurrent precipitation surrounding an annual-precipitation maxima, which is a feature not seen in other approaches. The approach does not require the prior spatial averaging of precipitation, explicit determination of spatial correlation coefficients, nor explicit definition of a representative area of a particular storm in the analysis. The annual-maxima centered approach was designed to exploit the wide availability of dense precipitation gauge data in many regions of the world. The approach produces ARF that decrease more rapidly than those from TP-29. Furthermore, the ARF from the approach decay rapidly with increasing recurrence interval of the annual-precipitation maxima. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 13]
机译:将点暴雨的降水深度调整为流域上的有效(平均)深度,对于表征降雨与径流的关系以及考虑设计暴雨时水工建筑物的经济有效设计非常重要。设计风暴是具有指定持续时间和频率(重复间隔)的降水点深度。有效深度通常是通过将点深度乘以面积缩小因子(ARF)来计算的。 ARF范围从0到1,根据风暴特征(例如复发间隔)而变化;是分水岭特征的函数,例如分水岭的大小,形状和地理位置。本文提出了一种估计ARF的新方法,并包括了在达拉斯奥斯汀和德克萨斯州休斯顿的1天设计风暴的应用。该方法被称为“年最大集中值”,专门考虑了围绕年降水量最大值的并发降水的分布,这是其他方法所没有的特征。该方法不需要事先进行降水的空间平均,空间相关系数的明确确定,也不需要分析中特定风暴代表区域的明确定义。年度最大值为中心的方法旨在利用世界上许多地区的密集降水量表数据的广泛可用性。该方法产生的ARF比TP-29的下降更快。此外,随着年降水最大值的复发间隔的增加,该方法的ARF迅速衰减。 (C)2000 Elsevier Science B.V.保留所有权利。 [参考:13]

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