2014
DOI: 10.1016/j.jconhyd.2014.07.005
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Implications of hydrologic connectivity between hillslopes and riparian zones on streamflow composition

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Cited by 56 publications
(64 citation statements)
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“…On the other hand, water within the layer is able to flow laterally because of its sandy texture and the imbricate structure of the coarse clasts. Besides, with high antecedent soil moisture above field capacity, the local groundwater near the spring is connected with the lateral flow paths from the hillslope, which is comparable to the results of von Freyberg et al (2014), Tetzlaff et al (2014) and Voeckler et al (2014). This linkage causes a fast and considerable discharge increase similar to the ''fill and spill hypothesis'' of Tromp-van Meerfeld and McDonnell (2006).…”
Section: Discussionsupporting
confidence: 70%
“…On the other hand, water within the layer is able to flow laterally because of its sandy texture and the imbricate structure of the coarse clasts. Besides, with high antecedent soil moisture above field capacity, the local groundwater near the spring is connected with the lateral flow paths from the hillslope, which is comparable to the results of von Freyberg et al (2014), Tetzlaff et al (2014) and Voeckler et al (2014). This linkage causes a fast and considerable discharge increase similar to the ''fill and spill hypothesis'' of Tromp-van Meerfeld and McDonnell (2006).…”
Section: Discussionsupporting
confidence: 70%
“…several hours), the chemical composition of the water that enters the stream might be comparable to the composition of precipitation or throughfall. Furthermore, if the riparian zone is near saturation, which occurs in the relatively flat valley bottoms in NF, only a small fraction of the precipitation can infiltrate and storage capacity is limited, resulting in 5 shallow flow from the riparian zone during rainfall events (von Freyberg et al, 2014;Mosquera et al, 2015). Similar to our study, Chaves et al (2008) found that the precipitation/throughfall end member contributed most to streamflow in a forested Amazonian catchment.…”
Section: Dominant Water Sources 20supporting
confidence: 83%
“…Clockwise loops and complex-shaped loops with a water table peak preceding streamflow peak were rarely found and were more typical of large rainfall events and/or wet moisture conditions. Other studies analysed the temporal and spatial variation of hysteresis (e.g., Detty and McGuire, 2008;McGuire and McDonnell, 2010) highlighting the role of hillslopes in runoff generation during wet periods and for large rainfall events (Ocampo et al, 2006;von Freyberg et al, 2014). At LCC, we observed similar hysteretic relations between depth to water table and streamflow.…”
Section: Long-term Monitoring In the Rio Vaduz Catchment Italy Figursupporting
confidence: 79%