<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<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>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>1996</publication_year>
	</journal>
	<doi>10.5194/npg-3-284-1996</doi>
	<article_url>http://www.nonlin-processes-geophys.net/3/284/1996/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/3/284/1996/npg-3-284-1996.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/3/284/1996/npg-3-284-1996.pdf</fulltext_pdf>
	<start_page>284</start_page>
	<end_page>290</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">On the influence of a large scale coherent vortex on the turbulent cascade</article_title>
	<authors>
		<author numeration="1" affiliations="">
			<name>F. Chillà</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J.-F. Pinton</name>
		</author>
		<author numeration="3" affiliations="2,3">
			<name>R. Labbé</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">École Normale Supérieure de Lyon, Laboratoire de Physique, 46 allée d&apos;Italie, F-69364 Lyon cedex 07, France</affiliation>
		<affiliation numeration="2" content_type="html">École Normale Supérieure de Lyon, Laboratoire de Physique, 46 allée d&apos;Italie, F-69364 Lyon cedex 07, France</affiliation>
		<affiliation numeration="3" content_type="html">Present address: Universidad de Santiago de Chile, Casilla 307, Correo 2, Santiago, Chile</affiliation>
	</affiliations>
	<abstract content_type="html">We investigate  the flow  between
coaxial  rotating
          disks in the situation where  a strong axial vortex  is
present
          over  a  turbulent  background.   This  is nonstationary  and
          inhomogeneous  as  is  common  in  most  turbulent 
geophysical
          flows.    We  describe  the  s  scale  statistics  using 
tools
          recently introduced for homogeneous turbulent flows.  
It seems
          that the  cascade cess  is preserved although  modified
by  the
          large coherent structure.</abstract>
	<references>
	</references>
</article>

