<?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>8</volume_number>
		<issue_number>1/2</issue_number>
		<publication_year>2001</publication_year>
	</journal>
	<doi>10.5194/npg-8-21-2001</doi>
	<article_url>http://www.nonlin-processes-geophys.net/8/21/2001/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/8/21/2001/npg-8-21-2001.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/8/21/2001/npg-8-21-2001.pdf</fulltext_pdf>
	<start_page>21</start_page>
	<end_page>36</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Bifurcations and instabilities in rotating two-layer fluids: I.f-plane</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>A. F. Lovegrove</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>I. M. Moroz</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. L. Read</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric, Oceanic &amp; Planetary Physics, University of Oxford, United Kingdom</affiliation>
		<affiliation numeration="2" content_type="html">Mathematical Institute, University of Oxford, United Kingdom</affiliation>
		<affiliation numeration="3" content_type="html">Present address: Smiths System Engineering, Guildford, UK</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper, we
      show that the behaviour of weakly nonlinear waves in a 2-layer model of
      baroclinic instability on an f-plane with varying viscosity is determined
      by a single, degenerate codimension three bifurcation. In the process, we
      show how previous studies, using the method of multiple scales to derive
      evolution equations for the slowly varying amplitude of the growing wave,
      arise as special limits of the general evolution description. A companion
      study will extend the results to a &lt;i&gt;&amp;#946;&lt;/i&gt;-plane.</abstract>
	<references>
	</references>
</article>

