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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>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/os-3-149-2007</doi>
	<article_url>http://www.ocean-sci.net/3/149/2007/</article_url>
	<abstract_html>http://www.ocean-sci.net/3/149/2007/os-3-149-2007.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/3/149/2007/os-3-149-2007.pdf</fulltext_pdf>
	<start_page>149</start_page>
	<end_page>157</end_page>
	<publication_date>2007-03-08</publication_date>
	<article_title content_type="html">Daily oceanographic analyses by Mediterranean Forecasting System at the basin scale</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Dobricic</name>
			<email>dobricic@bo.ingv.it</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>N. Pinardi</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Adani</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Tonani</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>C. Fratianni</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>A. Bonazzi</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>V. Fernandez</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Centro Interdipartimentale di Ricerche per le Scienze Ambientali, Ravenna, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">This study presents the upgrade of the Optimal Interpolation scheme used in
the basin scale assimilation scheme of the Mediterranean Forecasting System.
The modifications include a daily analysis cycle, the assimilation of ARGO
float profiles, the implementation of the geostrophic balance in the
background error covariance matrix and the initialisation of the analyses. A
series of numerical experiments showed that each modification had a positive
impact on the accuracy of the analyses: The daily cycle improved the
representation of the processes with the temporal variability shorter than a
week, the assimilation of ARGO floats profiles significantly improved the
salinity analyses quality, the geostrophically balanced background error
covariances improved the accuracy of the surface elevation analyses, and the
initialisation removed the barotropic adjustment in the forecast first time
steps starting from the analysis.</abstract>
	<references>
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		<reference numeration="2" content_type="text"> Castellari, S., Pinardi, N., and Leaman, K. D.: A model study of air-sea interactions in the Mediterranean Sea, J. Mar. Syst., 18, 89&amp;ndash;114, 1998. </reference>
		<reference numeration="3" content_type="text"> Daley, R.: Atmospheric data analysis. Cambridge atmospheric and space science series,Cambridge University Press, ISBN 0-521-38215-7, 1991. </reference>
		<reference numeration="4" content_type="text"> De Mey, P. and Benkiran, M.: A multivariate reduced-order optimal interpolation method and its application to the Mediterranean basin-scale circulation, Ocean Forecasting, edited by: Pinardi, N. and Woods, J., Springer Verlag, 281&amp;ndash;306, 2002. </reference>
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		<reference numeration="11" content_type="text"> Pinardi, N., Rosati, A., and Pacanowski, R. C.: The sea surface pressure formulation of rigid lid models. Implications for altimetric data assimilation studies, J. Mar. Syst., 6, 109&amp;ndash;119, 1995. </reference>
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</article>

