A continuous/discontinuous Galerkin framework for modeling coupled subsurface and surface water flow

DOI10.1007/s10596-008-9085-yzbMath1259.86001OpenAlexW1974044990MaRDI QIDQ1000895

Clint N. Dawson

Publication date: 11 February 2009

Published in: Computational Geosciences (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s10596-008-9085-y

zbMATH Keywords

Galerkin methodshallow water equationscoupled methodground water flow equations

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Flows in porous media; filtration; seepage (76S05) Finite element methods applied to problems in fluid mechanics (76M10) Finite element, Rayleigh-Ritz and Galerkin methods for initial value and initial-boundary value problems involving PDEs (65M60) Computational methods for problems pertaining to geophysics (86-08)

Related Items (10)

A scalable coupled surface-subsurface flow model ⋮ Analysis of the Stokes–Darcy problem with generalised interface conditions ⋮ Justification of Generalized Interface Conditions for Stokes–Darcy Problems ⋮ Discontinuous Galerkin method for coupling hydrostatic free surface flows to saturated subsurface systems ⋮ Stochastic multiscale flux basis for Stokes-Darcy flows ⋮ Unsaturated subsurface flow with surface water and nonlinear in- and outflow conditions ⋮ Validation and calibration of coupled porous-medium and free-flow problems using pore-scale resolved models ⋮ Multirate time integration for coupled saturated/unsaturated porous medium and free flow systems ⋮ Unsuitability of the Beavers–Joseph interface condition for filtration problems ⋮ Effective Coupling Conditions for Arbitrary Flows in Stokes--Darcy Systems

Uses Software

• WASH123D

Cites Work

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