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Viscous motion in an oceanic circulation model
Journal article   Open access   Peer reviewed

Viscous motion in an oceanic circulation model

A.F. Bennett and P.E. Kloeden
Bulletin of the Australian Mathematical Society, Vol.23(3), pp.443-460
1981
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Abstract

The barotropic motion of a viscous fluid in a laboratory simulation of ocean circulation may be modelled by Beards ley's vorticity equations. It is established here that these equations have unique smooth solutions which depend continuously on initial conditions. To avoid a boundary condition which involves an integral operator, the vorticity equations are replaced by an equivalent system of momentum equations. The system resembles the two-dimensional incompressible Navier-Stokes equations in a rotating reference frame. The existence of unique generalized solutions of the system in a square domain is established by modifying arguments used by Ladyzhenskaya for the Navier-Stokes equations. Smoothness of the solutions is then established by modifying Golovkin's arguments, again originally for the Navier- Stokes equations. A numerical procedure for solving the vorticity equations is discussed, as are the effects of reentrant corners in the domain modelling islands and peninsulae.

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Collaboration types
Domestic collaboration
Citation topics
8 Earth Sciences
8.19 Oceanography, Meteorology & Atmospheric Sciences
8.19.153 Ocean Circulation
Web Of Science research areas
Mathematics
ESI research areas
Mathematics
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