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Quick and Slow Components of the Hydrologic Response at the Hillslope Scale

2016

It is widely recognized that the Hortonian mechanism of runoff generation occurs in arid and semi-arid regions, generally characterized by high rainfall intensity on soils exhibiting low infiltrabilities. Differently, in steeply sloping forested watersheds in humid climates, by infiltrating through a highly permeable upper soil horizon, water moves beneath the soil surface determining a slow response. However, in most real cases, for example when in arid regions mountain forested areas take place, both (quick and slow) runoff generation processes coexist and together contribute to the hydrologic hillslope response. In this paper, based on analytical solutions of the hydrologic response, ins…

HydrologySubsurface stormflowGamma probability density function0208 environmental biotechnologyhillslope scale overland flow subsurface stormflow instantaneous response function gamma probability density function02 engineering and technologySoil surfaceAgricultural and Biological Sciences (miscellaneous)Arid020801 environmental engineeringInstantaneous response functionOverland flowSoil waterEnvironmental scienceSoil horizonSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSlow responseHillslope scaleScale (map)Surface runoffIntensity (heat transfer)Water Science and TechnologyCivil and Structural Engineering
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