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<article language="en">
	<journal>
		<journal_title>Geoscientific Model Development Discussions</journal_title>
		<journal_url>www.geosci-model-dev-discuss.net</journal_url>
		<issn>1991-9611</issn>
		<eissn>1991-962X</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/gmdd-3-517-2010</doi>
	<article_url>http://www.geosci-model-dev-discuss.net/3/517/2010/</article_url>
	<abstract_html>http://www.geosci-model-dev-discuss.net/3/517/2010/gmdd-3-517-2010.html</abstract_html>
	<fulltext_pdf>http://www.geosci-model-dev-discuss.net/3/517/2010/gmdd-3-517-2010.pdf</fulltext_pdf>
	<start_page>517</start_page>
	<end_page>540</end_page>
	<publication_date>2010-05-11</publication_date>
	<article_title content_type="html">Physically-based data assimilation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Levy</name>
			<email>gad@nwra.com</email>
		</author>
		<author numeration="2" affiliations="1,4">
			<name>M. Coon</name>
		</author>
		<author numeration="3" affiliations="2,3">
			<name>G. Nguyen</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>D. Sulsky</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NorthWest Research Associates, Seattle, Washington, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Mathematics and Statistics, University of New Mexico, Albuquerque, New Mexico, USA</affiliation>
		<affiliation numeration="3" content_type="html">currently at: The School of Civil Engineering, University of Sydney, Sydney, NSW, Australia</affiliation>
		<affiliation numeration="4" content_type="html">deceased</affiliation>
	</affiliations>
	<abstract content_type="html">Ideally, a validation and assimilation scheme should maintain the physical
principles embodied in the model and be able to evaluate and assimilate lower
dimensional features (e.g., discontinuities) contained within a bulk
simulation, even when these features are not directly observed or represented
by model variables. We present such a scheme and suggest its potential to
resolve or alleviate some outstanding problems that stem from making and
applying required, yet often non-physical, assumptions and procedures in
common operational data assimilation. As proof of concept, we use a sea-ice
model with remotely sensed observations of leads in a one-step assimilation
cycle. Using the new scheme in a sixteen day simulation experiment introduces
model skill (against persistence) several days earlier than in the control
run, improves the overall model skill and delays its drop off at later stages
of the simulation. The potential and requirements to extend
this scheme to different applications, and to both empirical and statistical
multivariate and full cycle data assimilation schemes, are discussed.</abstract>
	<references>
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</article>

