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isothermal atmosphere |
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isothermal atmosphere [¦ī·sə¦thər·məl ′at·mə‚sfir] (meteorology) An atmosphere in hydrostatic equilibrium, in which the temperature is constant with height and the pressure decreases exponentially upward. Also known as exponential atmosphere. 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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