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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>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-8619-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/8619/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/8619/2009/acpd-9-8619-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/8619/2009/acpd-9-8619-2009.pdf</fulltext_pdf>
	<start_page>8619</start_page>
	<end_page>8633</end_page>
	<publication_date>2009-04-01</publication_date>
	<article_title content_type="html">Sensitivity of ensemble Lagrangian reconstructions to assimilated wind time step resolution</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>I. Pisso</name>
			<email>ipisso@damtp.cam.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>V. Marécal</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>B. Legras</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>G. Berthet</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Météorologie Dynamique (UMR 8539), ENS – CNRS, Paris, France</affiliation>
		<affiliation numeration="2" content_type="html">Laboratoire de Physique et Chimie de l&apos;Environnement et de l&apos;Espace (UMR 6115), Université d&apos;Orléans – CNRS, Orléans, France</affiliation>
		<affiliation numeration="3" content_type="html">now at: Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The aim of this study is to define the optimal temporal and spatial
resolution required for accurate offline diffusive Lagrangian
reconstructions of high resolution in-situ tracers measurements based on
meteorological wind fields and on coarse resolution 3-D tracer
distributions. Increasing the time resolution of the advecting winds from
three to one hour intervals has a modest impact on diffusive
reconstructions in the case studied. This result is discussed in terms of
the effect on the geometry of transported clouds of points in order to set
out a method to assess the effect of meteorological flow on the transport
of atmospheric tracers.</abstract>
	<references>
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		<reference numeration="5" content_type="text"> Lefèvre, F.,~Figarol, F.,~Carslaw, K., and~Peter, T.: The 1997 arctic ozone depletion quantified from three-dimensional model simulations, Geophys. Res. Lett., 25, 2425–2428, 1998. </reference>
		<reference numeration="6" content_type="text"> Legras, B., Joseph, B., and~~Lefèvre, F.: Vertical diffusivity in the lower stratosphere from Lagrangian back-trajectory reconstructions of ozone profiles, J. Geophys. Res., 108(D18), 4562, doi:10.1029/2002JD003045, 2003. </reference>
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	</references>
</article>

