<?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>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>1998</publication_year>
	</journal>
	<doi>10.5194/npg-5-3-1998</doi>
	<article_url>http://www.nonlin-processes-geophys.net/5/3/1998/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/5/3/1998/npg-5-3-1998.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/5/3/1998/npg-5-3-1998.pdf</fulltext_pdf>
	<start_page>3</start_page>
	<end_page>12</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Hamiltonian formulation for the description of interfacial solitary waves</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Grimshaw</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. R. Pudjaprasetya</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Mathematics and Statistics, Monash University, Clayton, Victoria 3168, Australia</affiliation>
		<affiliation numeration="2" content_type="html">Department of Mathematics, Institut Teknologi, Bandung 40132, Indonesia</affiliation>
	</affiliations>
	<abstract content_type="html">We consider solitary waves propagating on the interface
between two fluids, each of constant density, for the case when the upper fluid is bounded
above by a rigid horizontal plane, but the lower fluid has a variable depth. It is
well-known that in this situation, the solitary waves can be described by a
variable-coefficient Korteweg-de Vries equation. Here we reconsider the derivation of this
equation and present a formulation which preserves the Hamiltonian structure of the
underlying system. The result is a new variable-coefficient Korteweg-de Vries equation,
which conserves energy to a higher order than the more conventional well-known equation.
The new equation is used to describe the transformation of an interfacial solitary wave
which propagates into a region of decreasing depth.</abstract>
	<references>
	</references>
</article>

