首页> 外文OA文献 >Precipitation, soil moisture and runoff variability in a small river catchment (Ardèche, France) during HyMeX Special Observation Period 1
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Precipitation, soil moisture and runoff variability in a small river catchment (Ardèche, France) during HyMeX Special Observation Period 1

机译:HyMeX特别观测期1期间,小河流域(法国阿德什)的降水,土壤湿度和径流变化1

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摘要

Flash flooding is a potentially destructive natural hazard known to occur in the Cévennes-Vivarais region in southern France. HyMeX (Hydrological Cycle in the Mediterranean Experiment) is an international program focused on understanding the hydrological cycle in the Mediterranean basin. Soil moisture is known to be a useful indicator of catchment response, however, establishing a meaningful estimation of soil moisture at the catchment level can be difficult due to its high variability in space and time. In a small gauged catchment in the Cévennes-Vivarais region in southern France, a series of manual soil moisture measurements was taken from September to December 2012 at both the field and catchment scale during the Special Observation Period 1 (SOP1) as part of the HyMeX program. Six plots were selected along a trajectory of a microwave link installed in the catchment and were chosen to represent different elevations in the catchment. Within each field plot, surface soil moisture was measured along a 50 m transect at 2 m intervals. This allowed the study of changes in within-field variability as well as between-field variability in response to precipitation events and during the drying out phase. Several precipitation events occurred over this autumn 2012 period which caused a significant wetting-up of the catchment, allowing the study of soil moisture processes over a wide range of wetness conditions. The influence of antecedent catchment conditions (soil moisture) on rainfall–runoff dynamics is demonstrated through the comparison of storm hydrographs for the various events. Dry catchment conditions result in minimal response in event flow, whereas large precipitation events occurring during wetter conditions produce much stronger responses in event flow. This further confirms the importance of quantifying catchment initial conditions to enhance the prediction of flash flood occurrences.
机译:暴发性洪水是一种潜在的破坏性自然灾害,已知发生在法国南部的塞文纳斯-维瓦莱伊斯地区。 HyMeX(地中海水文循环实验)是一项国际计划,旨在了解地中海盆地的水文循环。已知土壤水分是集水区响应的有用指标,但是,由于集水区在空间和时间上的高度可变性,很难在集水区建立有意义的土壤水分估算。在法国南部Cévennes-Vivarais地区的一个小规模集水区,作为特别观测期1(SOP1)的一部分,于2012年9月至2012年12月在田间和集水区进行了一系列手动土壤湿度测量,这是HyMeX的一部分程序。沿着安装在集水区中的微波链路的轨迹选择了六个地块,并选择它们代表集水区中的不同高度。在每个田地中,沿50 m的横断面以2 m的间隔测量地表土壤湿度。这允许研究响应降水事件和干旱期的田间变异性和田间变异性。在2012年秋季这一期间发生了几次降水事件,导致该流域大量湿润,从而使人们能够研究各种湿度条件下的土壤水分过程。通过比较各种事件的暴雨水位图,可以证明先前的流域条件(土壤水分)对降雨-径流动力学的影响。干流域条件导致事件流的响应最小,而在潮湿条件下发生的大降水事件在事件流中产生更强的响应。这进一步证实了量化流域初始条件以增强对山洪泛滥发生的预测的重要性。

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