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isothermal layer |
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isothermal layer [¦ī·sə¦thər·məl ′lā·ər] (meteorology) The approximately isothermal region of the atmosphere immediately above the tropopause. (thermodynamics) A layer of fluid, all points of which have the same temperature. 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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