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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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The hydrology of high-elevation headwaters in midlatitudes is typically dominated by snow processes, which are very sensitive to changes in energy inputs at the top of the snowpack. We present a data analyses that reveal how snowmelt and transpiration waves induced by the diurnal solar cycle generate water pressure fluctuations that propagate through the snowpack–hillslope–stream system. Changes in diurnal energy inputs alter these pressure cycles with potential ecohydrological consequences.
HESS | Articles | Volume 22, issue 8
Hydrol. Earth Syst. Sci., 22, 4295–4310, 2018
https://doi.org/10.5194/hess-22-4295-2018

Special issue: Assessing impacts and adaptation to global change in water...

Hydrol. Earth Syst. Sci., 22, 4295–4310, 2018
https://doi.org/10.5194/hess-22-4295-2018

Research article 14 Aug 2018

Research article | 14 Aug 2018

The influence of diurnal snowmelt and transpiration on hillslope throughflow and stream response

Brett Woelber et al.

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Latest update: 16 Jan 2021
Publications Copernicus
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Short summary
The hydrology of high-elevation headwaters in midlatitudes is typically dominated by snow processes, which are very sensitive to changes in energy inputs at the top of the snowpack. We present a data analyses that reveal how snowmelt and transpiration waves induced by the diurnal solar cycle generate water pressure fluctuations that propagate through the snowpack–hillslope–stream system. Changes in diurnal energy inputs alter these pressure cycles with potential ecohydrological consequences.
Citation