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Threshold effects in catchment storm response and the occurrence and magnitude of flood events: implications for flood frequency

机译:流域风暴响应中的阈值效应以及洪水事件的发生和程度:对洪水频率的影响

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摘要

The aim of this paper is to illustrate the effects of selected catchmentstorage thresholds upon runoff behaviour, and specifically their impact uponflood frequency. The analysis is carried out with the use of a stochasticrainfall model, incorporating rainfall variability at intra-event,inter-event and seasonal timescales, as well as infrequent summer tropicalcyclones, coupled with deterministic rainfall-runoff models that incorporaterunoff generation by both saturation excess and subsurface stormflowmechanisms. Changing runoff generation mechanisms (i.e. from subsurface flowto surface runoff) associated with a given threshold (i.e. saturationstorage capacity) is shown to be manifested in the flood frequency curve asa break in slope. It is observed that the inclusion of infrequent summerstorm events increases the temporal frequency occurrence and magnitude ofsurface runoff events, in this way contributing to steeper flood frequencycurves, and an additional break in the slope of the flood frequency curve.The results of this study highlight the importance of thresholds on floodfrequency, and provide insights into the complex interactions betweenrainfall variability and threshold nonlinearities in the rainfall-runoffprocess, which are shown to have a significant impact on the resulting floodfrequency curves.
机译:本文的目的是说明所选集水区存储阈值对径流行为的影响,尤其是它们对洪水频率的影响。分析是通过使用随机降雨模型进行的,该模型纳入了事件内,事件间和季节时间尺度的降雨变化性,以及夏季热带气旋的偶发性,并结合了确定性降雨-径流模型,该模型结合了由饱和度过高和过高引起的径流产生地下风暴流机制。与给定阈值(即饱和存储能力)相关的变化的径流生成机制(即从地下流量到地表径流)显示为洪水频率曲线中的坡度折断。可以看出,罕见的夏季暴风雨事件的加入增加了时间频率的发生和地表径流事件的强度,从而导致了陡峭的洪水频率曲线,并导致洪水频率曲线的斜率进一步断裂。阈值对洪水频率的重要性,并提供了降雨-径流过程中降雨变异性和阈值非线性之间复杂相互作用的见解,这些相互作用对所得的洪水频率曲线具有显着影响。

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