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Magnitude-frequency relationship of coastal sand delivery by a southern California stream

机译:南加州溪流沿海沙子输送的量级-频率关系

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Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 m3/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood.
机译:南加州溪流的沿海沙子输送是根据数值模型估计的,该模型刺激了河流三角洲系统的非稳态流动、沉积物输送和相关的河道调整。据估计,圣迭吉托河的年平均沉积物产量为51,400立方米/年,该河排干了由大坝控制的半干旱流域。在溪流的总沙子输送量中,20.5%来自大于100年一遇洪水的洪水;17.6%来自50年至100年的事件;25 至 50 年一遇的洪水占 28.4%;33.5%来自那些小于25年一遇的洪水。

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