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<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/npg-9-11-2002</doi>
	<article_url>http://www.nonlin-processes-geophys.net/9/11/2002/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/9/11/2002/npg-9-11-2002.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/9/11/2002/npg-9-11-2002.pdf</fulltext_pdf>
	<start_page>11</start_page>
	<end_page>23</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Impulse exchange at the surface of the ocean and the fractal dimension of drifter trajectories</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. M. Summers</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Mathematics and Statistics, Napier University, 219 Colinton Road, Edinburgh EH14 1DJ, UK</affiliation>
	</affiliations>
	<abstract content_type="html">An impulse-based
      model is developed to represent a coupling between turbulent flow in the
      atmosphere and turbulent flow in the ocean. In particular, it is argued
      that the atmosphere flowing horizontally over the ocean surface generates
      a velocity fluctuation field in the latter&apos;s near-surface flow. The
      mechanism for this can be understood kinematically in terms of an exchange
      of tangentially-oriented fluid impulse at the air-sea interface. We
      represent this exchange numerically through the creation of Lagrangian
      elements of impulse density. An indication of the efficacy of such a model
      would lie in its ability to predict the observed fractal dimension of
      lateral trajectories of submerged floats set adrift in the ocean. To this
      end, we examine the geometry of lateral tracer-paths determined from the
      present model.</abstract>
	<references>
	</references>
</article>

