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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>16</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/npg-16-665-2009</doi>
	<article_url>http://www.nonlin-processes-geophys.net/16/665/2009/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/16/665/2009/npg-16-665-2009.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/16/665/2009/npg-16-665-2009.pdf</fulltext_pdf>
	<start_page>665</start_page>
	<end_page>675</end_page>
	<publication_date>2009-12-14</publication_date>
	<article_title content_type="html">Low-frequency variability of the Kuroshio Extension</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Pierini</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>H. A. Dijkstra</name>
			<email>dijkstra@phys.uu.nl</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dipartimento di Scienze per l&apos;Ambiente, Università di Napoli Parthenope, Naples, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Marine and Atmospheric research Utrecht, Department of Physics and Astronomy, Utrecht University, Utrecht, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper, we provide a review of recent results targeted at the
understanding of the low-frequency variability of the Kuroshio Extension. We
provide the background and main arguments of two views which have recently
been proposed to explain this variability. In the first view, wind-induced
Rossby waves and the effects of mesocale eddies are crucial. The second view
is based on low-dimensional equivalent-barotropic large-scale nonlinear
dynamics, with neither Rossby wave dynamics nor baroclinic instability being
important. Results from models supporting each view are discussed and
confronted with results from available observations.</abstract>
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</article>

