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Linear Instability of a Current Flowing Along a Bottom Slope Using a Three-Layer Model
Linear Instability Current Flowing Bottom Slope Using Three-Layer Model
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2009/1/22
A quasi-geostrophic model of a three-layer fluid on an f-plane is employed to study instability of a current flowing over a uniform bottom slope with isobaths parallel to the current. The model has a ...
Linear Instability of a Zonal Jet on an f Plane
potential vorticity quasigeostrophic
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2008/12/3
The linear instability of a zonal geostrophic jet with a cosh−2 meridional profile on an f plane is investigated in a reduced-gravity, shallow-water model. The stability theory developed here ex...
Linear Instability of Barotropic Submesoscale Coherent Vortices Observed in the Ocean
Linear Instability Barotropic Submesoscale Coherent Vortices Observed
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2008/7/16
The linear instability of circular quasigeostrophic vortices with horizontal cross sections of angular velocity identical to those that fit the observations of submesoscale eddies in the ocean is inve...