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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>4</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-8327-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/8327/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/8327/2004/acpd-4-8327-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/8327/2004/acpd-4-8327-2004.pdf</fulltext_pdf>
	<start_page>8327</start_page>
	<end_page>8355</end_page>
	<publication_date>2004-12-15</publication_date>
	<article_title content_type="html">Analysis of water vapor LIDAR measurements during the MAP campaign: evidence of sub-structures of stratospheric intrusions</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>P. D’Aulerio</name>
			<email>p.daulerio@isac.cnr.it</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Fierli</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. Congeduti</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>G. Redaelli</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Atmospheric Sciences and Climate, CNR, Roma, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics, University of L’Aquila, L’Aquila, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">This paper presents case studies of dehydration in the free troposphere
measured by a ground based Raman LIDAR in the Northern-Italy, during the
Mesoscale Alpine Programme (MAP). Two observations characterized by the
presence of anomalously dry layers, below 6 km height, were analyzed using
Lagrangian techniques. These events are related to upper-tropospheric, high
Potential Vorticity streamers crossing the Alpine region and are interpreted
as small-scale features of stratospheric intrusions associated to the PV
ridge during its breakout phase. One of the measurements also shows the
presence of two distinct dehydrated structures associated to the same event.
The water vapor concentration also suggests dilution processes of dry
stratospheric air in the troposphere. Lagrangian simulations allowed to
successfully reproduce the observed water vapor distribution and the air
parcel histories confirmed the stratospheric origin of the dry layers.</abstract>
	<references>
	</references>
</article>

