Experiment XI: Baroclinic Instability of the Thermal Wind (Eddies)
DIYnamics: Baroclinic eddies in a tank and in Earth's atmosphere
Baroclinic instability in the presence of forced convection
Baroclinity - Video Learning - WizScience.com
Baroclinic Instability demo
In fluid dynamics, the baroclinity of a stratified fluid is a measure of how misaligned the gradient of pressure is from the gradient of density in a fluid. In meteorology a baroclinic atmosphere is one for which the density depends on both the temperature and the pressure; contrast this with a barotropic atmosphere, for which the density depends only on the pressure. In atmospheric terms, the barotropic zones of the Earth are generally found in the central latitudes, or tropics, whereas the baroclinic areas are generally found in the mid-latitude/polar regions.
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