Numerical simulation of the Benjamin-Feir instability and its consequences
Full nonlinear equations for one-dimensional potential surface waves were used for investigation of the evolution of an initially homogeneous train of exact Stokes waves with steepness A K = 0.01 – 0.42 . The numerical algorithm for the integration of nonstationary equations and the calculation of e...
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Veröffentlicht in: | Physics of fluids (1994) 2007-01, Vol.19 (1), p.016602-016602-15 |
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creator | Chalikov, Dmitry |
description | Full nonlinear equations for one-dimensional potential surface waves were used for investigation of the evolution of an initially homogeneous train of exact Stokes waves with steepness
A
K
=
0.01
–
0.42
. The numerical algorithm for the integration of nonstationary equations and the calculation of exact Stokes waves is described. Since the instability of the exact Stokes waves develops slowly, a random small-amplitude noise was introduced in initial conditions. The development of instability occurs in two stages: in the first stage the growth rate of disturbances was close to that established for small steepness by Benjamin and Feir [J. Fluid. Mech.
27, 417 (1967)] and for medium steepness [McLean, J. Fluid Mech.
114, 315 (1982)]. For any steepness, the Stokes waves disintegrate and create random superposition of waves. For
A
K
<
0.13
, waves do not show a tendency to breaking, which is recognized by approaching a surface to non-single-value shape. Sooner or later, if
A
K
>
0.13
, one of the waves increases its height, and finally it comes to the breaking point. For large steepness of
A
K
>
0.35
the rate of growth is slower than for medium steepness. The data for spectral composition of disturbances and their frequencies are given. |
doi_str_mv | 10.1063/1.2432303 |
format | Article |
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A
K
=
0.01
–
0.42
. The numerical algorithm for the integration of nonstationary equations and the calculation of exact Stokes waves is described. Since the instability of the exact Stokes waves develops slowly, a random small-amplitude noise was introduced in initial conditions. The development of instability occurs in two stages: in the first stage the growth rate of disturbances was close to that established for small steepness by Benjamin and Feir [J. Fluid. Mech.
27, 417 (1967)] and for medium steepness [McLean, J. Fluid Mech.
114, 315 (1982)]. For any steepness, the Stokes waves disintegrate and create random superposition of waves. For
A
K
<
0.13
, waves do not show a tendency to breaking, which is recognized by approaching a surface to non-single-value shape. Sooner or later, if
A
K
>
0.13
, one of the waves increases its height, and finally it comes to the breaking point. For large steepness of
A
K
>
0.35
the rate of growth is slower than for medium steepness. The data for spectral composition of disturbances and their frequencies are given.</description><identifier>ISSN: 1070-6631</identifier><identifier>EISSN: 1089-7666</identifier><identifier>DOI: 10.1063/1.2432303</identifier><identifier>CODEN: PHFLE6</identifier><language>eng</language><publisher>Melville, NY: American Institute of Physics</publisher><subject>Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Physics of the oceans ; Sea-air exchange processes</subject><ispartof>Physics of fluids (1994), 2007-01, Vol.19 (1), p.016602-016602-15</ispartof><rights>American Institute of Physics</rights><rights>2007 American Institute of Physics</rights><rights>2007 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c384t-e51ddf02ea008f4a7bc08d3f9a58af62a9be3f18e168d548ff7d7c318bbbbeed3</citedby><cites>FETCH-LOGICAL-c384t-e51ddf02ea008f4a7bc08d3f9a58af62a9be3f18e168d548ff7d7c318bbbbeed3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,794,1559,4512,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18534052$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Chalikov, Dmitry</creatorcontrib><title>Numerical simulation of the Benjamin-Feir instability and its consequences</title><title>Physics of fluids (1994)</title><description>Full nonlinear equations for one-dimensional potential surface waves were used for investigation of the evolution of an initially homogeneous train of exact Stokes waves with steepness
A
K
=
0.01
–
0.42
. The numerical algorithm for the integration of nonstationary equations and the calculation of exact Stokes waves is described. Since the instability of the exact Stokes waves develops slowly, a random small-amplitude noise was introduced in initial conditions. The development of instability occurs in two stages: in the first stage the growth rate of disturbances was close to that established for small steepness by Benjamin and Feir [J. Fluid. Mech.
27, 417 (1967)] and for medium steepness [McLean, J. Fluid Mech.
114, 315 (1982)]. For any steepness, the Stokes waves disintegrate and create random superposition of waves. For
A
K
<
0.13
, waves do not show a tendency to breaking, which is recognized by approaching a surface to non-single-value shape. Sooner or later, if
A
K
>
0.13
, one of the waves increases its height, and finally it comes to the breaking point. For large steepness of
A
K
>
0.35
the rate of growth is slower than for medium steepness. The data for spectral composition of disturbances and their frequencies are given.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Physics of the oceans</subject><subject>Sea-air exchange processes</subject><issn>1070-6631</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNqNkM9LwzAUgIMoOKcH_4NcPCh0Jk2bphdBh_MHQy96DmnyghltOpNM2H9v58SdFHN5OXzvg_chdErJhBLOLukkL1jOCNtDI0pEnVWc8_3NvyIZ54weoqMYF4QQVud8hB6fVh0Ep1WLo-tWrUqu97i3OL0BvgG_UJ3z2QxcwM7HpBrXurTGyhvsUsS69xHeV-A1xGN0YFUb4eR7jtHr7PZlep_Nn-8eptfzTDNRpAxKaowlOShChC1U1WgiDLO1KoWyPFd1A8xSAZQLUxbC2spUmlHRDA_AsDE633p16GMMYOUyuE6FtaREbiJIKr8jDOzZll2qONxog_Laxd2CKFlBynzgrrZc1C59Nfhd-lNM7ooNgot_C_6CP_qwA-XSWPYJZm6PGQ</recordid><startdate>20070101</startdate><enddate>20070101</enddate><creator>Chalikov, Dmitry</creator><general>American Institute of Physics</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20070101</creationdate><title>Numerical simulation of the Benjamin-Feir instability and its consequences</title><author>Chalikov, Dmitry</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c384t-e51ddf02ea008f4a7bc08d3f9a58af62a9be3f18e168d548ff7d7c318bbbbeed3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Physics of the oceans</topic><topic>Sea-air exchange processes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chalikov, Dmitry</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chalikov, Dmitry</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Numerical simulation of the Benjamin-Feir instability and its consequences</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2007-01-01</date><risdate>2007</risdate><volume>19</volume><issue>1</issue><spage>016602</spage><epage>016602-15</epage><pages>016602-016602-15</pages><issn>1070-6631</issn><eissn>1089-7666</eissn><coden>PHFLE6</coden><abstract>Full nonlinear equations for one-dimensional potential surface waves were used for investigation of the evolution of an initially homogeneous train of exact Stokes waves with steepness
A
K
=
0.01
–
0.42
. The numerical algorithm for the integration of nonstationary equations and the calculation of exact Stokes waves is described. Since the instability of the exact Stokes waves develops slowly, a random small-amplitude noise was introduced in initial conditions. The development of instability occurs in two stages: in the first stage the growth rate of disturbances was close to that established for small steepness by Benjamin and Feir [J. Fluid. Mech.
27, 417 (1967)] and for medium steepness [McLean, J. Fluid Mech.
114, 315 (1982)]. For any steepness, the Stokes waves disintegrate and create random superposition of waves. For
A
K
<
0.13
, waves do not show a tendency to breaking, which is recognized by approaching a surface to non-single-value shape. Sooner or later, if
A
K
>
0.13
, one of the waves increases its height, and finally it comes to the breaking point. For large steepness of
A
K
>
0.35
the rate of growth is slower than for medium steepness. The data for spectral composition of disturbances and their frequencies are given.</abstract><cop>Melville, NY</cop><pub>American Institute of Physics</pub><doi>10.1063/1.2432303</doi><tpages>15</tpages></addata></record> |
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language | eng |
recordid | cdi_crossref_primary_10_1063_1_2432303 |
source | AIP Journals Complete; AIP Digital Archive |
subjects | Earth, ocean, space Exact sciences and technology External geophysics Physics of the oceans Sea-air exchange processes |
title | Numerical simulation of the Benjamin-Feir instability and its consequences |
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