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baroclinic instability |
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baroclinic instability [¦bar·ə¦klin·ik in·stə′bil·əd·ē]
(meteorology) A hydrodynamic instability arising from the existence of a meridional temperature gradient (and hence of a thermal wind) in an atmosphere in quasi-geostrophic equilibrium and possessing static stability. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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baroclinic instability |
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