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<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/nhess-7-33-2007</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/7/33/2007/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/7/33/2007/nhess-7-33-2007.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/7/33/2007/nhess-7-33-2007.pdf</fulltext_pdf>
	<start_page>33</start_page>
	<end_page>40</end_page>
	<publication_date>2007-01-15</publication_date>
	<article_title content_type="html">Extremal periodic wave profiles</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>E. van Groesen</name>
			<email>groesen@math.utwente.nl</email>
		</author>
		<author numeration="2" affiliations="1,2,3">
			<name>Andonowati</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Applied Mathematics, University of Twente, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">LabMath-Indonesia, Bandung, Indonesia</affiliation>
		<affiliation numeration="3" content_type="html">Department of Mathematics, Institut Teknologi Bandung, Indonesia</affiliation>
	</affiliations>
	<abstract content_type="html">As a contribution to deterministic investigations into extreme fluid surface
waves, in this paper wave profiles of prescribed period that have maximal
crest height will be investigated. As constraints the values of the momentum
and energy integrals are used in a simplified description with the KdV model.
The result is that at the boundary of the feasible region in the
momentum-energy plane, the only possible profiles are the well known cnoidal
wave profiles. Inside the feasible region the extremal profiles of maximal
crest height are &quot;cornered&quot; cnoidal profiles: cnoidal profiles of larger
period, cut-off and periodically continued with the prescribed period so that
at the maximal crest height a corner results.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Olagnon, M. and Prevosto, M. (Eds.): Proceedings Rogue Waves 2004, Ifremer, ISBN 2-84433-150-5, 2004. </reference>
		<reference numeration="2" content_type="text"> Proceedings Rogue Waves: Edinburgh, Scotland, 2005, http://www.icms.org.uk/meetings/2005/roguewaves/index.html, 2005. </reference>
		<reference numeration="3" content_type="text"> van Groesen, E. and de Jager, E. M.: Mathematical structures in continuous dynamical systems, North Holland, Elsevier, Amsterdam, 1994. \bibitem[Van Groesen and Andonowati(2006a)] GroAan06FinEn van Groesen, E. and Andonowati: Finite energy wave signals of extremal amplitude in the spatial NLS-dynamics, Phys. Lett. A, 357, 86&amp;ndash;91, 2006. </reference>
	</references>
</article>

