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	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-20631-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/20631/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/20631/2009/acpd-9-20631-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/20631/2009/acpd-9-20631-2009.pdf</fulltext_pdf>
	<start_page>20631</start_page>
	<end_page>20675</end_page>
	<publication_date>2009-10-01</publication_date>
	<article_title content_type="html">Ice nucleation and cloud microphysical properties in tropical tropopause layer cirrus</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. J. Jensen</name>
			<email>eric.j.jensen@nasa.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Pfister</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T.-P. Bui</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>P. Lawson</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>D. Baumgardner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="2" content_type="html">SPEC Inc., Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Centro de Ciencias de la Atmosfera, Universidad Nacional Autonoma de Mexico, Circuito Exterior, Mexico</affiliation>
	</affiliations>
	<abstract content_type="html">In past modeling studies, it has generally been assumed that the
      predominant mechanism for nucleation of ice in the uppermost
      troposphere is homogeneous freezing of aqueous aerosols.  However,
      recent in situ and remote-sensing measurements of the properties of
      cirrus clouds at very low temperatures in the tropical tropopause
      layer (TTL) are broadly inconsistent with theoretial predictions based
      on the homogeneous freezing assumption.  The nearly ubiquitous
      occurence of gravity waves in the TTL makes the predictions from
      homogeneous nucleation theory particularly difficult to reconcile with
      measurements.  These measured properties include ice number
      concentrations, which are much lower than theory predicts; ice crystal
      size distributions, which are much broader than theory predicts; and
      cloud extinctions, which are much lower than theory predicts.
      Although other explanations are possible, one way to limit ice
      concentrations is to have on the order of 50 L&lt;sup&gt;&amp;minus;1&lt;/sup&gt; effective
      ice nuclei (IN) that could nucleate ice at relatively low
      supersaturations.  We suggest that ammonium sulfate particles, which
      would be dry much of the time in the cold TTL, are a potential IN
      candidate for TTL cirrus.  Possible implications of the observed cloud
      microphysical properties for ice sedimentation, dehydration, and cloud
      persistence are also discussed.</abstract>
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