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<article language="en">
	<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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-14145-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/14145/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/14145/2008/acpd-8-14145-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/14145/2008/acpd-8-14145-2008.pdf</fulltext_pdf>
	<start_page>14145</start_page>
	<end_page>14168</end_page>
	<publication_date>2008-07-23</publication_date>
	<article_title content_type="html">Detection of reactive nitrogen containing particles in the tropopause region &amp;ndash; evidence for a tropical nitric acid trihydrate (NAT) belt</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Voigt</name>
			<email>christiane.voigt@dlr.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Schlager</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. Roiger</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>A. Stenke</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. de Reus</name>
		</author>
		<author numeration="6" affiliations="2,3">
			<name>S. Borrmann</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>E. Jensen</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>C. Schiller</name>
		</author>
		<author numeration="9" affiliations="5">
			<name>P. Konopka</name>
		</author>
		<author numeration="10" affiliations="6">
			<name>N. Sitnikov</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Deutsches Zentrum fÃ¼r Luft- und Raumfahrt, Institut fÃ¼r Physik der AtmosphÃ¤re, Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institut fÃ¼r Physik der AtmosphÃ¤re, UniversitÃ¤t Mainz, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Max-Planck-Institut fÃ¼r Chemie, Abteilung Wolkenphysik, Mainz, Germany</affiliation>
		<affiliation numeration="4" content_type="html">NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Institut fÃ¼r Chemie und Dynamik der GeosphÃ¤re, FZ JÃ¼lich, Germany</affiliation>
		<affiliation numeration="6" content_type="html">Central Aerological Observatory, Moscow, Soviet Union</affiliation>
	</affiliations>
	<abstract content_type="html">The detection of nitric acid trihydrate (NAT, HNO&lt;sub&gt;3&lt;/sub&gt;&amp;times;3H&lt;sub&gt;2&lt;/sub&gt;O)
particles in the tropical transition layer (TTL) harmonizes our understanding
of polar stratospheric cloud formation. Large reactive nitrogen (NO&lt;sub&gt;y&lt;/sub&gt;)
containing particles were observed on 8 August 2006 by instruments onboard
the high altitude research aircraft M55-Geophysica near and below the
tropical tropopause. The particles, most likely NAT, have diameters less than
6 &amp;mu;m and concentrations below 10&lt;sup&gt;&amp;minus;4&lt;/sup&gt; cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. The NAT particle
layer was repeatedly detected at altitudes between 15.1 and 17.5 km over
extended areas of 9.5 to 17.2&amp;deg; N and 1.5&amp;deg; W to 2.7&amp;deg; E
above the African continent. Satellite observations suggest that the NAT
particles could have nucleated on ice fed by convective activity. Once
nucleated, the NAT particles can slowly grow within the TTL for days, while
being transported over long distances. Their in-situ detection combined with
global model simulations of the NAT supersaturation near the tropical
tropopause indicate the potential for a tropical tropopause NAT particle
belt.</abstract>
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</article>

