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Crest-height statistics in finite water depth. Part 1: The role of the nonlinear interactions in uni-directional seas
This paper explores the competing nonlinear processes that define the largest crest heights in uni-directional random seas. In deep water, the third-order near-resonant interactions produce a focusing of the free-wave energy and hence larger crest elevations. However, as the effective water depth re...
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Published in: | Ocean engineering 2023-12, Vol.289, p.116369, Article 116369 |
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description | This paper explores the competing nonlinear processes that define the largest crest heights in uni-directional random seas. In deep water, the third-order near-resonant interactions produce a focusing of the free-wave energy and hence larger crest elevations. However, as the effective water depth reduces, theoretical considerations, based upon the assumption that the frequency spectrum is narrow-banded, suggest that this process weakens and below kpd=1.363 (kp being the wavenumber of the spectral peak frequency and d the water depth) energy defocusing occurs. This paper first explores how the near-resonant interactions affect the crest heights arising in broad-banded, non-breaking, uni-directional seas in a wide range of effective water depths. It also quantifies the role of the bound-wave interactions. The numerical calculations conclude that kpd=1.363 indeed defines the boundary between energy focusing and defocusing for realistic jonswap sea-states, irrespective of the spectral bandwidth and steepness. However, for kpd |
doi_str_mv | 10.1016/j.oceaneng.2023.116369 |
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•Numerical simulation of crest height statistics in broad-banded random seas.•Largest crests dependent on high-order bound waves and near-resonant interactions.•In deep water bound and near-resonant terms increase crest heights above second-order.In shallower water near-resonant defocusing reduces crests, but bound waves dominate.•Transition from resonant focusing/de-focusing independent of steepness and bandwidth.•Spatial/temporal evolution of near-resonant effects key to understanding laboratory data.</description><identifier>ISSN: 0029-8018</identifier><identifier>DOI: 10.1016/j.oceaneng.2023.116369</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Near-resonant interactions ; Nonlinear defocusing ; Nonlinear focusing ; Nonlinear waves ; Wave crest statistics</subject><ispartof>Ocean engineering, 2023-12, Vol.289, p.116369, Article 116369</ispartof><rights>2023 The Authors</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c307t-509713691f02c920e32a95326e72d6b5c7e3acd8b66b93978b685bca6e27de083</cites><orcidid>0000-0003-4925-8822 ; 0000-0001-6487-0230</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Zve, E.S.</creatorcontrib><creatorcontrib>Swan, C.</creatorcontrib><creatorcontrib>Hughes, G.O.</creatorcontrib><title>Crest-height statistics in finite water depth. Part 1: The role of the nonlinear interactions in uni-directional seas</title><title>Ocean engineering</title><description>This paper explores the competing nonlinear processes that define the largest crest heights in uni-directional random seas. In deep water, the third-order near-resonant interactions produce a focusing of the free-wave energy and hence larger crest elevations. However, as the effective water depth reduces, theoretical considerations, based upon the assumption that the frequency spectrum is narrow-banded, suggest that this process weakens and below kpd=1.363 (kp being the wavenumber of the spectral peak frequency and d the water depth) energy defocusing occurs. This paper first explores how the near-resonant interactions affect the crest heights arising in broad-banded, non-breaking, uni-directional seas in a wide range of effective water depths. It also quantifies the role of the bound-wave interactions. The numerical calculations conclude that kpd=1.363 indeed defines the boundary between energy focusing and defocusing for realistic jonswap sea-states, irrespective of the spectral bandwidth and steepness. However, for kpd<1.363, the bound-wave contributions increase the largest crest heights, while the near-resonant interactions reduce them. The tail of the crest-height distributions is therefore defined by two competing nonlinear processes. The present results have important implications for both the interpretation of laboratory data describing crest-height distributions and the appropriateness of second-order models for practical engineering calculations.
•Numerical simulation of crest height statistics in broad-banded random seas.•Largest crests dependent on high-order bound waves and near-resonant interactions.•In deep water bound and near-resonant terms increase crest heights above second-order.In shallower water near-resonant defocusing reduces crests, but bound waves dominate.•Transition from resonant focusing/de-focusing independent of steepness and bandwidth.•Spatial/temporal evolution of near-resonant effects key to understanding laboratory data.</description><subject>Near-resonant interactions</subject><subject>Nonlinear defocusing</subject><subject>Nonlinear focusing</subject><subject>Nonlinear waves</subject><subject>Wave crest statistics</subject><issn>0029-8018</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNqFkM1OwzAQhH0AiVJ4BeQXSFjbihNzAlX8SZXgUM6W42waV8GubBfE25MSOHPa0WpnNPsRcsWgZMDk9a4MFo1Hvy05cFEyJoVUJ2QBwFXRAGvOyHlKOwCQEsSCHFYRUy4GdNsh05RNdik7m6jztHfeZaSfJmOkHe7zUNJXEzNlN3QzII1hRBp6miftgx-dRxMn43RubHbB_6QcvCs6F_FnY0aa0KQLctqbMeHl71ySt4f7zeqpWL88Pq_u1oUVUOeiAlWzqT_rgVvFAQU3qhJcYs072Va2RmFs17RStkqoehJN1VojkdcdQiOWRM65NoaUIvZ6H927iV-agT4C0zv9B0wfgekZ2GS8nY04tftwGHWyDr3F-RPdBfdfxDeCzHrQ</recordid><startdate>20231201</startdate><enddate>20231201</enddate><creator>Zve, E.S.</creator><creator>Swan, C.</creator><creator>Hughes, G.O.</creator><general>Elsevier Ltd</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><orcidid>https://orcid.org/0000-0003-4925-8822</orcidid><orcidid>https://orcid.org/0000-0001-6487-0230</orcidid></search><sort><creationdate>20231201</creationdate><title>Crest-height statistics in finite water depth. Part 1: The role of the nonlinear interactions in uni-directional seas</title><author>Zve, E.S. ; Swan, C. ; Hughes, G.O.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c307t-509713691f02c920e32a95326e72d6b5c7e3acd8b66b93978b685bca6e27de083</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Near-resonant interactions</topic><topic>Nonlinear defocusing</topic><topic>Nonlinear focusing</topic><topic>Nonlinear waves</topic><topic>Wave crest statistics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zve, E.S.</creatorcontrib><creatorcontrib>Swan, C.</creatorcontrib><creatorcontrib>Hughes, G.O.</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><jtitle>Ocean engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zve, E.S.</au><au>Swan, C.</au><au>Hughes, G.O.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Crest-height statistics in finite water depth. Part 1: The role of the nonlinear interactions in uni-directional seas</atitle><jtitle>Ocean engineering</jtitle><date>2023-12-01</date><risdate>2023</risdate><volume>289</volume><spage>116369</spage><pages>116369-</pages><artnum>116369</artnum><issn>0029-8018</issn><abstract>This paper explores the competing nonlinear processes that define the largest crest heights in uni-directional random seas. In deep water, the third-order near-resonant interactions produce a focusing of the free-wave energy and hence larger crest elevations. However, as the effective water depth reduces, theoretical considerations, based upon the assumption that the frequency spectrum is narrow-banded, suggest that this process weakens and below kpd=1.363 (kp being the wavenumber of the spectral peak frequency and d the water depth) energy defocusing occurs. This paper first explores how the near-resonant interactions affect the crest heights arising in broad-banded, non-breaking, uni-directional seas in a wide range of effective water depths. It also quantifies the role of the bound-wave interactions. The numerical calculations conclude that kpd=1.363 indeed defines the boundary between energy focusing and defocusing for realistic jonswap sea-states, irrespective of the spectral bandwidth and steepness. However, for kpd<1.363, the bound-wave contributions increase the largest crest heights, while the near-resonant interactions reduce them. The tail of the crest-height distributions is therefore defined by two competing nonlinear processes. The present results have important implications for both the interpretation of laboratory data describing crest-height distributions and the appropriateness of second-order models for practical engineering calculations.
•Numerical simulation of crest height statistics in broad-banded random seas.•Largest crests dependent on high-order bound waves and near-resonant interactions.•In deep water bound and near-resonant terms increase crest heights above second-order.In shallower water near-resonant defocusing reduces crests, but bound waves dominate.•Transition from resonant focusing/de-focusing independent of steepness and bandwidth.•Spatial/temporal evolution of near-resonant effects key to understanding laboratory data.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.oceaneng.2023.116369</doi><orcidid>https://orcid.org/0000-0003-4925-8822</orcidid><orcidid>https://orcid.org/0000-0001-6487-0230</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Near-resonant interactions Nonlinear defocusing Nonlinear focusing Nonlinear waves Wave crest statistics |
title | Crest-height statistics in finite water depth. Part 1: The role of the nonlinear interactions in uni-directional seas |
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