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multiple tropopause |
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multiple tropopause [′məl·tə·pəl ′trō·pə‚pȯz]
(geophysics) A frequent condition in which the tropopause appears not as a continuous single “surface” of discontinuity between the troposphere and the stratosphere, but as a series of quasi-horizontal “leaves,” which are partly overlapping in steplike arrangement. 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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