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<article language="en">
	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/os-3-205-2007</doi>
	<article_url>http://www.ocean-sci.net/3/205/2007/</article_url>
	<abstract_html>http://www.ocean-sci.net/3/205/2007/os-3-205-2007.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/3/205/2007/os-3-205-2007.pdf</fulltext_pdf>
	<start_page>205</start_page>
	<end_page>222</end_page>
	<publication_date>2007-05-04</publication_date>
	<article_title content_type="html">Simulations of ARGO profilers and of surface floating objects: applications in MFSTEP</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Pizzigalli</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Rupolo</name>
			<email>rupolo@casaccia.enea.it</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Climate Department, ENEA, Via Anguillarese 301 00060 Rome, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">In this work we describe part of the activities performed in the MFSTEP project by means
of numerical simulations of ARGO profilers and surface floating objects.
Simulations of ARGO floats were used to define the optimal time cycling in order
to maximize independent observations of vertical profiles of temperature and
salinity and to minimize the error on the estimate of the velocity at the parking depth of the profilers.
Instead, the Mediterranean Forecasting System archive of Eulerian velocity field from 2000
to 2004 was used to build a related surface Lagrangian archive, systematically integrating numerical
particles released and constrained to drift at surface. Here we use such Lagrangian archive to study the
interannual variability of the surface Lagrangian transport in two key areas of the Western Mediterranean,
also introducing an exponential decay in the particles concentration.</abstract>
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</article>

