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subsidence inversion |
Also found in: Wikipedia | 0.01 sec. |
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subsidence inversion [səb′sīd·əns in‚vər·zhən]
(meteorology) A temperature inversion produced by the adiabatic warming of a layer of subsiding air; this inversion is enhanced by vertical mixing in the air layer below the inversion. 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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