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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>9</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-17937-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/17937/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/17937/2009/acpd-9-17937-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/17937/2009/acpd-9-17937-2009.pdf</fulltext_pdf>
	<start_page>17937</start_page>
	<end_page>17962</end_page>
	<publication_date>2009-09-01</publication_date>
	<article_title content_type="html">Annual cycle of ozone at and above the tropical tropopause: observations versus simulations with the Chemical Model of the Stratosphere (CLaMS)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Konopka</name>
			<email>p.konopka@fz-juelich.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J.-U. Grooß</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>G. Günther</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>F. Plöger</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>R. Pommrich</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>R. Müller</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>N. Livesey</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Forschungszentrum Jülich (ICG-1: Stratosphere), Germany</affiliation>
		<affiliation numeration="2" content_type="html">Jet Propulsion Laboratory, California Institue of Technology, Pasadena, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Multi-annual simulations with the Chemical Model of the Stratosphere
(CLaMS) are used to study the seasonality of O&lt;sub&gt;3&lt;/sub&gt; and of the mean age
within the stratospheric part of the tropical tropopause layer (TTL)
In agreement with satellite (HALOE) and in-situ observations (SHADOZ),
CLaMS simulations show above &amp;asymp;360 K potential
temperature, a pronounced annual cycle in O&lt;sub&gt;3&lt;/sub&gt; and in the mean age of
air with highest values in the late boreal summer.
Within the model, this seasonality is driven by the seasonality of
both upwelling and in-mixing. The latter process describes enhanced meridional
transport from the extratropics into the TTL.
The strongest in-mixing occurs from the Northern Hemisphere during the
boreal summer in the potential temperature range between 380 and 420 K.
Contrary, an increase of upwelling with highest values in
winter reduces O&lt;sub&gt;3&lt;/sub&gt; up to the lowest values in early spring.
Both, CLaMS simulations and Aura MLS O&lt;sub&gt;3&lt;/sub&gt; observations show that
this enhanced equatorward transport in summer is mainly driven by the
Asian monsoon anticyclone.</abstract>
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</article>

