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A note on linear dispersion and shoaling properties in extended Boussinesq equations
A set of optimum parameter α is obtained to evaluate the linear dispersion and shoaling properties in the extended Boussinesq equations of Madsen and Sørensen (1992), Nwogu (1993), and Chen and Liu (1995). Optimum α values are determined to produce minimal errors in each wave property of phase veloc...
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Published in: | Ocean engineering 2003-10, Vol.30 (14), p.1849-1867 |
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container_end_page | 1867 |
container_issue | 14 |
container_start_page | 1849 |
container_title | Ocean engineering |
container_volume | 30 |
creator | Lee, C. Cho, Y.-S. Yoon, S.B. |
description | A set of optimum parameter
α is obtained to evaluate the linear dispersion and shoaling properties in the extended Boussinesq equations of
Madsen and Sørensen (1992), Nwogu (1993), and
Chen and Liu (1995). Optimum
α values are determined to produce minimal errors in each wave property of phase velocity, group velocity, or shoaling coefficient relative to the analytical one given by the Stokes wave theory. Comparisons are made of the percent errors in phase velocity, group velocity, and shoaling coefficient produced by the Boussinesq equations with a different set of optimum
α values. The case with a fixed value of
α = −0.4 is also presented in the comparison. The comparisons reveal that the optimum
α value tuned for a particular wave property gives in general poor results for other properties. Considering all the properties simultaneously, the fixed value of
α = −0.4 may give overall accuracies in phase velocity and shoaling coefficient for all the types of Boussinesq equations selected in this study. |
doi_str_mv | 10.1016/S0029-8018(03)00015-5 |
format | article |
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α is obtained to evaluate the linear dispersion and shoaling properties in the extended Boussinesq equations of
Madsen and Sørensen (1992), Nwogu (1993), and
Chen and Liu (1995). Optimum
α values are determined to produce minimal errors in each wave property of phase velocity, group velocity, or shoaling coefficient relative to the analytical one given by the Stokes wave theory. Comparisons are made of the percent errors in phase velocity, group velocity, and shoaling coefficient produced by the Boussinesq equations with a different set of optimum
α values. The case with a fixed value of
α = −0.4 is also presented in the comparison. The comparisons reveal that the optimum
α value tuned for a particular wave property gives in general poor results for other properties. Considering all the properties simultaneously, the fixed value of
α = −0.4 may give overall accuracies in phase velocity and shoaling coefficient for all the types of Boussinesq equations selected in this study.</description><identifier>ISSN: 0029-8018</identifier><identifier>EISSN: 1873-5258</identifier><identifier>DOI: 10.1016/S0029-8018(03)00015-5</identifier><identifier>CODEN: OCENBQ</identifier><language>eng</language><publisher>Amsterdam: Elsevier Ltd</publisher><subject>Dynamics of the ocean (upper and deep oceans) ; Earth, ocean, space ; Exact sciences and technology ; Extended Boussinesq equations ; External geophysics ; Linear dispersion ; Marine ; Numerical test ; Physics of the oceans ; Shoaling coefficient ; Surface waves, tides and sea level. Seiches</subject><ispartof>Ocean engineering, 2003-10, Vol.30 (14), p.1849-1867</ispartof><rights>2003 Elsevier Science Ltd</rights><rights>2003 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23</citedby><cites>FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14984673$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Lee, C.</creatorcontrib><creatorcontrib>Cho, Y.-S.</creatorcontrib><creatorcontrib>Yoon, S.B.</creatorcontrib><title>A note on linear dispersion and shoaling properties in extended Boussinesq equations</title><title>Ocean engineering</title><description>A set of optimum parameter
α is obtained to evaluate the linear dispersion and shoaling properties in the extended Boussinesq equations of
Madsen and Sørensen (1992), Nwogu (1993), and
Chen and Liu (1995). Optimum
α values are determined to produce minimal errors in each wave property of phase velocity, group velocity, or shoaling coefficient relative to the analytical one given by the Stokes wave theory. Comparisons are made of the percent errors in phase velocity, group velocity, and shoaling coefficient produced by the Boussinesq equations with a different set of optimum
α values. The case with a fixed value of
α = −0.4 is also presented in the comparison. The comparisons reveal that the optimum
α value tuned for a particular wave property gives in general poor results for other properties. Considering all the properties simultaneously, the fixed value of
α = −0.4 may give overall accuracies in phase velocity and shoaling coefficient for all the types of Boussinesq equations selected in this study.</description><subject>Dynamics of the ocean (upper and deep oceans)</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Extended Boussinesq equations</subject><subject>External geophysics</subject><subject>Linear dispersion</subject><subject>Marine</subject><subject>Numerical test</subject><subject>Physics of the oceans</subject><subject>Shoaling coefficient</subject><subject>Surface waves, tides and sea level. Seiches</subject><issn>0029-8018</issn><issn>1873-5258</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNqFkE9PHDEMxaMKpC60H6FSLq3gMOAkk5nMqQJU_khIPZSeozRxINWQ2Y1nK_j2ze4iOHKyZP-e_fwY-yLgRIDoTn8ByKExIMwRqGMAELrRH9hCmF41WmqzxxavyEd2QPS3Ql0HasHuznieZuRT5mPK6AoPiZZYKNWOy4HTw-Tq5J4vy1T7c0LiKXN8mjEHDPx8WhNVJa04rtZurjr6xPajGwk_v9RD9vvyx93FdXP78-rm4uy28aozc2Nip4ULRnod216B_tOb2MtOVZvRdNiboZU4mBgUKKV9AKkVBC-hDQGjVIfs225v9bZaI832MZHHcXQZqy0rDMi2HVQF9Q70ZSIqGO2ypEdXnq0Au8nQbjO0m4AsKLvN0Oqq-_pywJF3Yywu-0Rv4nYwbddv9n_fcVi__ZewWPIJs8eQCvrZhim9c-k_i0mFtw</recordid><startdate>20031001</startdate><enddate>20031001</enddate><creator>Lee, C.</creator><creator>Cho, Y.-S.</creator><creator>Yoon, S.B.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20031001</creationdate><title>A note on linear dispersion and shoaling properties in extended Boussinesq equations</title><author>Lee, C. ; Cho, Y.-S. ; Yoon, S.B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Dynamics of the ocean (upper and deep oceans)</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Extended Boussinesq equations</topic><topic>External geophysics</topic><topic>Linear dispersion</topic><topic>Marine</topic><topic>Numerical test</topic><topic>Physics of the oceans</topic><topic>Shoaling coefficient</topic><topic>Surface waves, tides and sea level. Seiches</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lee, C.</creatorcontrib><creatorcontrib>Cho, Y.-S.</creatorcontrib><creatorcontrib>Yoon, S.B.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Ocean engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lee, C.</au><au>Cho, Y.-S.</au><au>Yoon, S.B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A note on linear dispersion and shoaling properties in extended Boussinesq equations</atitle><jtitle>Ocean engineering</jtitle><date>2003-10-01</date><risdate>2003</risdate><volume>30</volume><issue>14</issue><spage>1849</spage><epage>1867</epage><pages>1849-1867</pages><issn>0029-8018</issn><eissn>1873-5258</eissn><coden>OCENBQ</coden><abstract>A set of optimum parameter
α is obtained to evaluate the linear dispersion and shoaling properties in the extended Boussinesq equations of
Madsen and Sørensen (1992), Nwogu (1993), and
Chen and Liu (1995). Optimum
α values are determined to produce minimal errors in each wave property of phase velocity, group velocity, or shoaling coefficient relative to the analytical one given by the Stokes wave theory. Comparisons are made of the percent errors in phase velocity, group velocity, and shoaling coefficient produced by the Boussinesq equations with a different set of optimum
α values. The case with a fixed value of
α = −0.4 is also presented in the comparison. The comparisons reveal that the optimum
α value tuned for a particular wave property gives in general poor results for other properties. Considering all the properties simultaneously, the fixed value of
α = −0.4 may give overall accuracies in phase velocity and shoaling coefficient for all the types of Boussinesq equations selected in this study.</abstract><cop>Amsterdam</cop><pub>Elsevier Ltd</pub><doi>10.1016/S0029-8018(03)00015-5</doi><tpages>19</tpages></addata></record> |
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source | ScienceDirect Freedom Collection |
subjects | Dynamics of the ocean (upper and deep oceans) Earth, ocean, space Exact sciences and technology Extended Boussinesq equations External geophysics Linear dispersion Marine Numerical test Physics of the oceans Shoaling coefficient Surface waves, tides and sea level. Seiches |
title | A note on linear dispersion and shoaling properties in extended Boussinesq equations |
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