<?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>9</volume_number>
		<issue_number>3/4</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/npg-9-367-2002</doi>
	<article_url>http://www.nonlin-processes-geophys.net/9/367/2002/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/9/367/2002/npg-9-367-2002.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/9/367/2002/npg-9-367-2002.pdf</fulltext_pdf>
	<start_page>367</start_page>
	<end_page>371</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Numerical wind wave model with a dynamic boundary layer</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. G. Polnikov</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Y. A. Volkov</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. A. Pogarskii</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">A. M. Obukhov Institute for Atmospheric Physics of the Russian Academy of Sciences, Pyzhevskii lane, 3, 109017 Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">A modern version of
      a numerical wind wave model of the fourth generation is constructed for a
      case of deep water. The following specific terms of the model source
      function are used: (a) a new analytic parameterization of the nonlinear
      evolution term proposed recently in Zakharov and Pushkarev (1999); (b) a
      traditional input term added by the routine for an atmospheric boundary
      layer fitting to a wind wave state according to Makin and Kudryavtsev
      (1999); (c) a dissipative term of the second power in a wind wave spectrum
      according to Polnikov (1991). The direct fetch testing results showed an
      adequate description of the main empirical wave evolution effects.
      Besides, the model gives a correct description of the boundary layer
      parameters&apos; evolution, depending on a wind wave stage of development.
      This permits one to give a physical treatment of the dependence mentioned.
      These performances of the model allow one to use it both for application
      and for investigation aims in the task of the joint description of wind
      and wave fields.</abstract>
	<references>
	</references>
</article>

