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convective instability |
Also found in: Wikipedia | 0.03 sec. |
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convective instability [kən′vek·div in·stə′bil·əd·ē] (meteorology) The state of an unsaturated layer or column of air in the atmosphere whose wet-bulb potential temperature (or equivalent potential temperature) decreases with elevation. Also known as potential instability. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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