Effect of bedrock permeability on subsurface stormflow and the water balance of a trenched hillslope at the Panola Mountain Research Watershed, Georgia, USA

The effect of bedrock permeability on subsurface stormflow initiation and the hillslope water balance is poorly understood. Previous hillslope hydrological studies at the Panola Mountain Research Watershed (PMRW), Georgia, USA, have assumed that the bedrock underlying the trenched hillslope is effec...

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Veröffentlicht in:Hydrological processes 2007-03, Vol.21 (6), p.750-769
Hauptverfasser: Tromp-van Meerveld, H. J., Peters, N. E., McDonnell, J. J.
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Sprache:eng
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