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Quantifying Transport Between the Tropical and Mid-Latitude Lower Stratosphere

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dc.contributor.author Volk, C. en_US
dc.contributor.author Elkins, J. en_US
dc.contributor.author Fahey, D. en_US
dc.contributor.author Salawitch, R. en_US
dc.contributor.author Dutton, G. en_US
dc.contributor.author Gilligan, J. en_US
dc.contributor.author Proffitt, M. en_US
dc.contributor.author Loewenstein, M. en_US
dc.contributor.author Podolske, J. en_US
dc.contributor.author Minschwaner, K. en_US
dc.contributor.author Margitan, J. en_US
dc.date.accessioned 2004-09-30T05:14:41Z
dc.date.available 2004-09-30T05:14:41Z
dc.date.issued 1996
dc.identifier.clearanceno 96-0643
dc.identifier.uri http://hdl.handle.net/2014/25015
dc.description.abstract Because exchange with the tropics is slower than multi-dimensional models generally assume, ozone at mid-latitudes apears to be more sensitive to elevated levels of industrial chlorine than currently predicted. Nevertheless, approximately 45% of air in the tropical ascent region at 21 km has been entrained from mid-latitudes, implying that emissions from supersonic aircraft could deplete ozone in the middle stratosphere. en_US
dc.format.extent 1401986 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other stratosphere en_US
dc.title Quantifying Transport Between the Tropical and Mid-Latitude Lower Stratosphere en_US


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