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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-9-18597-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/18597/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/18597/2009/acpd-9-18597-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/18597/2009/acpd-9-18597-2009.pdf</fulltext_pdf>
	<start_page>18597</start_page>
	<end_page>18619</end_page>
	<publication_date>2009-09-09</publication_date>
	<article_title content_type="html">Increase of upper troposphere/lower stratosphere wave baroclinicity during the second half of the 20th century</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. M. Castanheira</name>
			<email>jcast@ua.pt</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>J. A. AÃ±el</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. A. F. Marques</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. C. AntuÃ±a</name>
		</author>
		<author numeration="5" affiliations="4,5">
			<name>M. L. R. Liberato</name>
		</author>
		<author numeration="6" affiliations="1,2">
			<name>L. de la Torre</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>L. Gimeno</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CESAM, Department of Physics, University of Aveiro, Portugal</affiliation>
		<affiliation numeration="2" content_type="html">EPhysLab, Faculty of Sciences of Ourense, University of Vigo, Spain</affiliation>
		<affiliation numeration="3" content_type="html">EstaciÃ³n Lidar de CamagÃ¼ay, CamagÃ¼ay, Cuba</affiliation>
		<affiliation numeration="4" content_type="html">Department of Physics, University of TrÃ¡s-os-Montes e Alto Douro, Portugal</affiliation>
		<affiliation numeration="5" content_type="html">CGUL, IDL, University of Lisbon, Portugal</affiliation>
	</affiliations>
	<abstract content_type="html">A strengthening of the equatorward temperature gradient in the upper
troposphere/lower stratosphere (UTLS), at subtropics and
midlatitudes, is consistently reproduced in several modelling
studies of the atmospheric response to the increase of greenhouse
gas radiative forcing. Some of those studies suggest an increase of
the baroclinicity in the UTLS region because of the enhanced
meridional temperature gradient.
&lt;br&gt;&lt;br&gt;
This study presents observational evidence of an increase of UTLS
wave baroclinicity, during the second half of the 20th century. The
evidence is given by significant positive trends in the energy of
baroclinic normal modes of the NCEP/NCAR reanalysis, and significant
positive trends in the eddy available potential energy of the ERA-40
reanalysis as well as in the eddy available potential energy of the
JRA-25 reanalysis. Significant positive trends in the frequency of
double tropopause events in radiosonde data are also interpreted as
a manifestation of an increase of the UTLS wave baroclinicity.</abstract>
	<references>
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</article>

