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Updating Flood Records Using Historic Water Profiles

机译:使用历史水剖面更新洪水记录

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摘要

The statistical evaluation of flood records requires long data series to extrapolate reliable peak discharges and related recurrence intervals. Often the records are extended with historical information concerning the water level. As the distribution functions are usually fitted to the discharge values historic stage-discharge-relations must be found to convert these values. Regarding the Elbe river at the Dresden gauge the history of a water course and its morphology is investigated. Using the former flow cross sections water profile calculations are carried out yielding different stage-discharge-curves for each historic period. Checking the flood stages since 1501 A.D. and the related peak discharges, resulted in reduced discharge values. The new peak discharge values allow an update of the flood records as well as recurrence periods and lead to the result that e.g. the 2002 flood seems to have a recurrence period three times longer than it was assumed up to now.
机译:洪水记录的统计评估需要较长的数据序列以推断可靠的峰值流量和相关的重复间隔。通常,记录会扩展有关水位的历史信息。由于分配函数通常适合于排放值,因此必须找到历史的阶段排放关系来转换这些值。关于德累斯顿水位计的易北河,研究了水道的历史及其形态。使用前一个流动横截面,对每个历史时期进行水廓线计算,得出不同的水位流量曲线。检查自公元1501年以来的洪水阶段以及相关的峰值流量,导致流量降低。新的峰值排放值允许更新洪水记录和复发周期,并导致结果如2002年的洪灾复发周期似乎比现在所设想的要长三倍。

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