A new method of describing bottom stress in two-dimensional hydrodynamical models of shallow homogeneous seas, estuaries, and lakes

DOI10.1016/0307-904X(88)90054-6zbMath0659.76024MaRDI QIDQ1112659

J. R. Hunter, Clifford J. Hearn

Publication date: 1988

Published in: Applied Mathematical Modelling (Search for Journal in Brave)

zbMATH Keywords

relaxation approximationbottom frictionestuariesexplicit time-stepping modellakesshallow homogeneous seastwo-dimensional hydrodynamical modelswind-driven circulation in shallow systems

Mathematics Subject Classification ID

Related Items (5)

On obtaining the steady-state solutions of the linearized three- dimensional hydrodynamic equations ⋮ A new method of describing bottom stress in two-dimensional hydrodynamical models of shallow homogeneous seas, estuaries, and lakes ⋮ Decision support for the design of constructed wetlands ⋮ A note on the equivalence of some two- and three-dimensional models of wind-driven barotropic flow in shallow seas ⋮ Response of a uniform unbounded ocean to a moving tropical cyclone

Cites Work

• On determining the profile of steady wind-induced currents
• A new method of describing bottom stress in two-dimensional hydrodynamical models of shallow homogeneous seas, estuaries, and lakes
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