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首页> 外文期刊>Journal of the American Water Resources Association >AN EVALUATION OF FLOOD FREQUENCY ESTIMATES BASED ON RAINFALL/RUNOFF MODELING1
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AN EVALUATION OF FLOOD FREQUENCY ESTIMATES BASED ON RAINFALL/RUNOFF MODELING1

机译:基于降雨量/径流MODELING1的洪水频率估计评估

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ABSTRACT:An evaluation of flood frequency estimates simulated from a rainfall/runoff model is based on (1) computation of the equivalent years of record for regional estimating equations based on 50 small stream sites in Oklahoma and (2) computation of the bias for synthetic flood estimates as compared to observed estimates at 97 small stream sites with at least 20 years of record in eight eastern states. Because of the high intercorrelation of synthetic flood estimates between watersheds, little or no regional (spatial) information may be added to the network as a result of the modeling activity. The equivalent years of record for the regional estimating equations based totally on synthetic flood discharges is shown to be considerably less than the length of rainfall record used to simulate the runoff. Furthermore, the flood estimates from the rainfall/runoff model consistently underestimate the flood discharges based on observed record, particularly for the larger floods. Depending on the way bias is computed, the synthetic estimate of the 100‐year flood discharge varies from 11 to 29 percent less than the value based on observed record.In addition, the correlation between observed and synthetic flood frequency estimates at the same site is also investigated. The degree of correlation between these estimates appears to vary with recurrence interval. Unless the correlation between these two estimates is known, it is not possible to compute a weighted estimate with minimum varianc
机译:摘要:对降雨/径流模型模拟的洪水频率估计的评估基于 (1) 基于俄克拉荷马州 50 个小溪流站点的区域估计方程的等效记录年数的计算和 (2) 计算合成洪水估计的偏差与东部八个州至少有 20 年记录的 97 个小溪流站点的观测估计值相比。由于流域之间合成洪水估计值的高度相互相关性,因此由于建模活动,很少或根本没有区域(空间)信息可以添加到网络中。完全基于合成洪水排放的区域估算方程的等效记录年数大大小于用于模拟径流的降雨记录的长度。此外,降雨量/径流模型的洪水估计值始终低估了基于观测记录的洪水排放量,特别是对于较大的洪水。根据偏差的计算方式,100年一遇洪水排放的综合估计值比基于观测记录的值低11%至29%。此外,还研究了同一地点观测到的洪水频率估计值与合成洪水频率估计值之间的相关性。这些估计值之间的相关性似乎随复发间隔而变化。除非知道这两个估计值之间的相关性,否则不可能计算出具有最小方差的加权估计值

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