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Process-based flood frequency analysis in an agricultural watershed exhibiting nonstationary flood seasonality

机译:基于过程的农业分水岭泛频分析,展出非间断的洪水季节性

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摘要

Floods are the product of complex interactions among processes including precipitation, soil moisture, and watershed morphology. Conventional flood frequency analysis (FFA) methods such as design storms and discharge-based statistical methods offer few insights into these process interactions and how they "shape" the probability distributions of floods. Understanding and projecting flood frequency in conditions of nonstationary hydroclimate and land use require deeper understanding of these processes, some or all of which may be changing in ways that will be undersampled in observational records. This study presents an alternative "process-based" FFA approach that uses stochastic storm transposition to generate large numbers of realistic rainstorm "scenarios" based on relatively short rainfall remote sensing records. Long-term continuous hydrologic model simulations are used to derive seasonally varying distributions of watershed antecedent conditions. We couple rainstorm scenarios with seasonally appropriate antecedent conditions to simulate flood frequency. The methodology is applied to the 4002 km(2) Turkey River watershed in the Midwestern United States, which is undergoing significant climatic and hydrologic change. We show that, using only 15 years of rainfall records, our methodology can produce accurate estimates of "present-day" flood frequency. We found that shifts in the seasonality of soil moisture, snow, and extreme rainfall in the Turkey River exert important controls on flood frequency. We also demonstrate that process-based techniques may be prone to errors due to inadequate representation of specific seasonal processes within hydrologic models. If such mistakes are avoided, however, process-based approaches can provide a useful pathway toward understanding current and future flood frequency in nonstationary conditions and thus be valuable for supplementing existing FFA practices.
机译:洪水是过程中复杂相互作用的产品,包括降水,土壤水分和流域形态。传统的洪水频率分析(FFA)方法,如设计风暴和基于出院的统计方法,对这些过程相互作用以及它们“形状”的概率分布提供了很少的见解。在非营养的水池和土地使用条件下,理解和投影洪水频率需要更深入地了解这些过程,其中一些或全部可能是在观察记录中欠采样的方式变化。本研究提出了一种替代的“基于过程的”FFA方法,该方法使用随机风暴转换来产生基于相对短的降雨遥感记录的大量现实暴雨“情景”。长期连续水文模型模拟用于导出流域的前一种条件的季节变化。我们将暴雨情景与季节性适当的先行条件耦合以模拟洪水频率。该方法适用于美国中西部的4002公里(2)土耳其河流域,正在进行显着的气候和水文变化。我们表明,只使用15年的降雨记录,我们的方法可以产生“当今”洪水频率的准确估计。我们发现在土壤水分,雪地季节性,土耳其河的季节性转变为洪水频率的重要控制。我们还证明基于过程的技术可能易于由于水文模型中特定季节性过程的表示不足而易受误差。然而,如果避免这种错误,基于过程的方法可以提供有用的途径,以了解非间断条件中的电流和未来的洪水频率,因此对补充现有的FFA实践有价值。

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