Barotropic instability of coastal flows as a boundary-value problem: linear and non-linear theory.

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Bibliographic Details
Title: Barotropic instability of coastal flows as a boundary-value problem: linear and non-linear theory.
Authors: WILLMOTT, ANDREW J.1 ajwil@pol.ac.uk, CUSHMAN-ROISIN, BENOIT2
Source: Geophysical & Astrophysical Fluid Dynamics. Aug2009, Vol. 103 Issue 4, p279-292. 14p. 1 Diagram, 2 Charts, 3 Graphs.
Subjects: Boundary value problems, Complex variables, Astronomical perturbation, Whirlwinds, Dynamic meteorology, Territorial waters, Continental shelf
Abstract: The barotropic instability is traditionally viewed as an initial-value problem wherein wave perturbations of a laterally sheared flow in a homogeneous uniformly rotating fluid that temporally grows into vortices. The vortices are capable of mixing fluid on the continental shelf with fluid above the continental slope and adjacent deep-sea region. However, the instability can also be viewed as a boundary-value problem. For example, a laterally sheared coastal flow is perturbed at some location, creating perturbations that grow spatially downstream. This process leads to a time periodic flow that exhibits instability in space. This article first examines the linear barotropic instability problem with real frequency and complex wavenumber. It is shown that there exists a frequency band within which a spatially growing wave is present. It is then postulated that far downstream the spatially unstable flow emerges into a chain of identically axisymmetric vortices. Conservation of mass, momentum and energy fluxes are applied to determine the diameter, spacing and the speed of translation of the vortices. [ABSTRACT FROM AUTHOR]
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Database: Engineering Source
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