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2015 | OriginalPaper | Buchkapitel

2. Rainfall-Induced Runoff and Subsurface Stormflow at the Hillslope Scale

verfasst von : Vyacheslav G. Rumynin

Erschienen in: Overland Flow Dynamics and Solute Transport

Verlag: Springer International Publishing

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Abstract

Surface runoff (or overland flow), which is generated by the precipitation that falls within a drainage area (catchment, watershed), is governed by several factors and processes, including rainfall rate and duration, the characteristics of infiltration (capillary imbibition and gravity-driven) and the temperature regime of soil, landscape surface characteristics, vegetation type, and some others. Hillslopes are regarded as a basic element of catchments, therefore the mathematical and physical description of the hydrological processes that occur at the hillslope scale is the first step to designing more general hydrological models describing hydrological response at catchment/watershed scale.

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Vorheriges Kapitel Surface Runoff Generation, Vertical Infiltration and Subsurface Lateral Flow

Nächstes Kapitel Models of Dissolved Component Transport at the Hillslope Scale

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Titel: Rainfall-Induced Runoff and Subsurface Stormflow at the Hillslope Scale
verfasst von: Vyacheslav G. Rumynin
Verlag: Springer International Publishing
Buch: Overland Flow Dynamics and Solute Transport
Print ISBN: 978-3-319-21800-7

Electronic ISBN: 978-3-319-21801-4

Copyright-Jahr: 2015
DOI: https://doi.org/10.1007/978-3-319-21801-4_2