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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>6</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acp-6-1221-2006</doi>
	<article_url>http://www.atmos-chem-phys.net/6/1221/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/6/1221/2006/acp-6-1221-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/6/1221/2006/acp-6-1221-2006.pdf</fulltext_pdf>
	<start_page>1221</start_page>
	<end_page>1230</end_page>
	<publication_date>2006-04-20</publication_date>
	<article_title content_type="html">MIPAS detects Antarctic stratospheric belt of NAT PSCs caused by mountain waves</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Höpfner</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>N. Larsen</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>R. Spang</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>B. P. Luo</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>J. Ma</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>S. H. Svendsen</name>
		</author>
		<author numeration="7" affiliations="6">
			<name>S. D. Eckermann</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>B. Knudsen</name>
		</author>
		<author numeration="9" affiliations="7,8">
			<name>P. Massoli</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>F. Cairo</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>G. Stiller</name>
		</author>
		<author numeration="12" affiliations="1">
			<name>T. v. Clarmann</name>
		</author>
		<author numeration="13" affiliations="1">
			<name>H. Fischer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Forschungszentrum Karlsruhe, Institut für Meteorologie und Klimaforschung, Karlsruhe, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Danish Meteorological Institute, Middle Atmosphere Research Division, Copenhagen, Denmark</affiliation>
		<affiliation numeration="3" content_type="html">Forschungszentrum Jülich, Institut für Chemie und Dynamik der Geosphäre, Jülich, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Institut für Atmosphäre und Klima, ETH-Hönggerberg, Zürich, Switzerland</affiliation>
		<affiliation numeration="5" content_type="html">Computational Physics, Inc., Springfield, VA, USA</affiliation>
		<affiliation numeration="6" content_type="html">E. O. Hulburt Center for Space Research, Naval Research Laboratory, Washington, USA</affiliation>
		<affiliation numeration="7" content_type="html">Consiglio Nazionale delle Ricerche, Istituto di Scienze dell’Atmosfera e del Clima, Rome, Italy</affiliation>
		<affiliation numeration="8" content_type="html">now at: University of Colorado, Cooperative Institute for Research in the Environmental Sciences, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Space borne infrared limb emission measurements by the  Michelson Interferometer for Passive Atmospheric Sounding
(MIPAS) reveal the formation of a belt of polar stratospheric clouds (PSCs) of  nitric acid trihydrate (NAT) particles
over Antarctica in mid-June 2003. By mesoscale microphysical simulations we show
that this sudden onset of NAT PSCs was caused by heterogeneous nucleation on ice in the
cooling phases of large-amplitude stratospheric mountain waves over the Antarctic
Peninsula and the Ellsworth Mountains.
MIPAS observations of PSCs before this event show
no indication for the presence of NAT clouds with volume densities larger than about 0.3 &amp;micro;m&lt;sup&gt;3&lt;/sup&gt;/cm&lt;sup&gt;3&lt;/sup&gt;
and radii smaller than 3 &amp;micro;m, but are consistent with supercooled droplets of
ternary H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;/HNO&lt;sub&gt;3&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;O solution (STS).
Simulations indicate that homogeneous surface  nucleation rates have to be
reduced by three orders of magnitude to comply with the observations.</abstract>
	<references>
	</references>
</article>

