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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-935-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/935/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/935/2007/cpd-3-935-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/935/2007/cpd-3-935-2007.pdf</fulltext_pdf>
	<start_page>935</start_page>
	<end_page>960</end_page>
	<publication_date>2007-07-10</publication_date>
	<article_title content_type="html">Maintenance of polar stratospheric clouds in a moist stratosphere</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. B. Kirk-Davidoff</name>
			<email>dankd@atmos.umd.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J.-F. Lamarque</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Maryland, Department of Atmospheric and Oceanic Science, USA</affiliation>
		<affiliation numeration="2" content_type="html">National Center for Atmospheric Research, Atmospheric Chemistry Division, Boulder, Colorado, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Previous work has shown that polar stratospheric clouds (PSCs) could have
acted to substantially warm high latitude regions during past warm climates
such as the Eocene (55 Ma). Using a simple model of stratospheric water vapor
transport and polar stratospheric cloud (PSC) formation, we investigate the
dependence of PSC optical depth on tropopause temperature, cloud
microphysical parameters, stratospheric overturning, and tropospheric
methane. We show that PSC radiative effects can help slow removal of water
from the stratosphere via self-heating. However, we also show that the
ability of PSCs to have a substantial impact on climate depends strongly on
the PSC particle number density and the strength of the overturning
circulation. Thus even a large source of stratospheric water vapor (e.g. from
methane oxidation) will not result in substantial PSC radiative effects
unless PSC ice crystal number density is high, and stratospheric overturning
(which modulates polar stratospheric temperatures) is low. These results are
supported by analysis of a series of runs of the NCAR WACCM model with
methane concentrations varying up to one thousand times present levels.</abstract>
	<references>
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</article>

