Click on “Download PDF” for the PDF version or on the title for the HTML version.
If you are not an ASABE member or if your employer has not arranged for access to the full-text, Click here for options.
Spatio-Temporal Patterns in Soil Water Content Time Series: Influence of the Time Series Length and Precipitation Events
Published by the American Society of Agricultural and Biological Engineers, St. Joseph, Michigan www.asabe.orgCitation: 21st Century Watershed Technology: Improving Water Quality and the Environment Conference Proceedings, May 27-June 1, 2012, Bari, Italy 12-12496.(doi:10.13031/2013.41447)
Authors: Diego RIVERA, José Luis ARUMÍ, Mario LILLO-SAAVEDRA
Keywords: Soil water content, time series, time stability, wavelet filtering
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 operating monitoring 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 of events, the monitoring depth and the hydrogeological setting.(Download PDF) (Export to EndNotes)