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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-1703-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/1703/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/1703/2009/acpd-9-1703-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/1703/2009/acpd-9-1703-2009.pdf</fulltext_pdf>
	<start_page>1703</start_page>
	<end_page>1726</end_page>
	<publication_date>2009-01-16</publication_date>
	<article_title content_type="html">Antarctic stratospheric warming since 1979</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Hu</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>Q. Fu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, Peking University, Beijing, China</affiliation>
		<affiliation numeration="2" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, USA</affiliation>
	</affiliations>
	<abstract content_type="html">In the present study, we show evidence of significant stratospheric warming
over large portions of the Antarctic polar region in winter and spring
seasons, with a maximum warming of 7–8&amp;deg;C in September and October,
using satellite Microwave Sounding Unit observations for 1979–2006. It is
found that this warming is associated with increasing wave activity from the
troposphere into the stratosphere, suggesting that the warming is caused by
enhanced wave-driven dynamical heating. We show that the Antarctic
stratospheric warming has close correlations with sea surface temperature
(SST) increases, and that general circulation model simulations forced with
observed time-varying SSTs reproduce similar warming trend patterns in the
Antarctic stratosphere. These findings suggest that the Antarctic
stratospheric warming is likely induced by SST warming. As SST warming
continues as a consequence of greenhouse gas increases due to anthropogenic
activity, Antarctic stratospheric warming would also continue, which has
important implications to the recovery of the Antarctic ozone hole.</abstract>
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