Some General Properties of Transverse Motions of the Geostrophic Front

Some General Properties of Transverse Motions of the Geostrophic Front Within the framework of the reduced-gravity model of the ocean taking into account the effect of friction in the Rayleigh form, we study the two-dimensional problem of nonlinear motions of a subsurface front of finite width. We consider the conservation laws and the character of motion of the center-of-mass of the cross section of the front and their variations caused by the losses of energy. For fields with special structure, the problem is reduced to the solution of a system of nonlinear ordinary differential equations. It is shown that the initially geostrophic frontal current decays with time according to a power law. The deviations of the initial state of the front from the state of geostrophic balance result in the generation of superinertial oscillations of the hydrodynamic fields. Physical Oceanography Springer Journals

Some General Properties of Transverse Motions of the Geostrophic Front

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Kluwer Academic Publishers-Plenum Publishers
Copyright © 2003 by Plenum Publishing Corporation
Earth Sciences; Oceanography; Remote Sensing/Photogrammetry; Atmospheric Sciences; Climate Change; Environmental Physics
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