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Spatio-Temporal Patterns in Soil Water Content Time Series: Influence of the Time Series Length and Precipitation Events

机译:土壤含水量的时空模式序列:时间序列长度和降水事件的影响

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Soil water content is a key link among environmental compartments. We discuss the influence of the time series length and precipitation events on the spatio-temporal patterns in soil water content time series as an ex post assessment of the operatingmonitoring network. To analyze different spatio-temporal patterns in the soil water content, we applied the concept of time stability and wavelet filtering (wavelet power spectra and wavelet coherency). Wavelet filtering allowed us to get insight into the response of the monitoring points at different time scales, while the time stability concept allowed us to identify representative locations, i.e., monitoring points which have the property of representing some statistical features of the whole monitoring system. Our results show that the representative monitoring points change as new data is added, and that the location of the most stable point depends on the hydrological condition of the sites (e.g. precipitation and lateral flows). Also, in our case study upper strata are proxies for hourly-to-daily changes in soil water content, while deeper strata are proxies for medium-term stored water. The coupling between precipitation and soil water content depends on the precipitation volume, the number ofevents, the monitoring depth and the hydrogeological setting.
机译:土壤含水量是环境隔间之间的关键环节。我们讨论了时间序列长度和降水事件对土壤水分序列时空模式的影响,作为工作通风网络的EX后评估。为了分析土壤含水量中的不同时空模式,我们应用了时间稳定性和小波滤波的概念(小波功率谱和小波一致性)。小波滤波允许我们在不同时间尺度上深入了解监视点的响应,而时间稳定性概念允许我们识别具有代表整个监控系统的一些统计特征的特性的代表位置。我们的结果表明,当添加新数据时,代表监测点变化,并且最稳定的点的位置取决于位点的水文条件(例如降水和横向流动)。此外,在我们的案例中,研究上层是土壤含水量的每日到日常变化的代理,而深层次的地层是用于中期储存水的代理。沉淀和土壤含水量之间的偶联取决于沉淀体积,非凡,监测深度和水文地质环境。

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