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Spatially variable water table recharge and the hillslope hydrologic response: Analytical solutions to the linearized hillslope Boussinesq equation

Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the dynamics of saturated, subsurface flow from hillslopes with shallow, unconfined aquifers. In this paper, we use a new analytical technique to solve the linearized hillslope Boussinesq equation to pre...

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Autori principali: David N. Dralle, Gabrielle F.S. Boisramé, Sally E. Thompson
Natura: Artigo
Lingua:Inglês
Pubblicazione: Wiley 2014-11-01
Serie:Water Resources Research
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Accesso online:https://doi.org/10.1002/2013WR015144
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