首页> 外文期刊>Journal of Hydrology: Regional Studies >Runoff response to rainfall events considering initial soil moisture – Analysis of 9-year records in a small Alpine catchment (Brixenbach valley, Tyrol, Austria)
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Runoff response to rainfall events considering initial soil moisture – Analysis of 9-year records in a small Alpine catchment (Brixenbach valley, Tyrol, Austria)

机译:考虑初始土壤水分的降雨事件的径流响应 - 小型高山集水区9年记录(Brixenbach Valley,Tyrol,奥地利)分析

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Study region:Brixenbach catchment (10 km2), Kitzbuehel Alps, Tyrol, Austria. Study focus:This study presents the data of one of the rare soil moisture networks in the Alps, a 9-year soil moisture time series recorded at 8 sites with in-situ measurements (six pasture and two forest sites). We aim at understanding the soil moisture behaviour in general, its reaction to rainfall considering the site characteristics and the runoffreaction depending on the antecedent soil moisture content. We analysed soil moisture, rainfall and discharge data with a temporal resolution of one hour (summer months) and two hours (autumn to spring) respectively and interpreted the results in terms of land use and topographical features. New hydrological insights for the region:The medians of the soil moisture positively correlate with the sites’ altitude. Comparing spatial standard deviation of soil moisture versus spatial mean shows a high scatter of the standard deviations, contrary to previous studies, which use considerably shorter time series. The spatial variability increases with spatial mean, thus the highest spatial variability is recorded at wet conditions. The catchment shows clear threshold behaviour: Runoffcoefficients above 0.23 only occurred when the soil moisture spatial mean of the eight sites overrun 43.5 vol% which can be translated into a saturation deficit of 0.28.
机译:学习区:Brixenbach集水区(10 km2),Kitzbuehel阿尔卑斯山,塔罗尔,奥地利。研究重点:本研究介绍了阿尔卑斯山中稀土水分网络之一的数据,这是一个9年的土壤湿度时间序列,在8个网站上记录,具有原位测量(六场牧场和两个森林网站)。我们的目标是了解土壤水分行为一般,对降雨的反应,考虑到现场特征和润滑率取决于先前的防治水分含量。我们分析了土壤湿度,降雨量和排放数据,时间分辨率为一小时(夏季)和两个小时(秋至春季),并在土地利用和地形特征方面解释了结果。该地区的新水文见解:土壤水分的中位于与场地的高度呈正相关。比较土壤水分的空间标准偏差与空间平均值显示出标准偏差的高散射,与之前的研究相反,使用相当较短的时间序列。空间可变性随空间平均值而增加,因此在潮湿条件下记录最高的空间变异性。该集水区显示出明确的阈值行为:仅在八个位点的土壤水分空间平均值超过43.5 Vol%时才发生在0.23以上的跑道高于0.23,这可以转化为0.28的饱和缺陷。

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