Loading…

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...

Full description

Saved in:
Bibliographic Details
Published in:Ocean engineering 2003-10, Vol.30 (14), p.1849-1867
Main Authors: Lee, C., Cho, Y.-S., Yoon, S.B.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23
cites cdi_FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23
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
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_18024493</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0029801803000155</els_id><sourcerecordid>18024493</sourcerecordid><originalsourceid>FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23</originalsourceid><addsrcrecordid>eNqFkE9PHDEMxaMKpC60H6FSLq3gMOAkk5nMqQJU_khIPZSeozRxINWQ2Y1nK_j2ze4iOHKyZP-e_fwY-yLgRIDoTn8ByKExIMwRqGMAELrRH9hCmF41WmqzxxavyEd2QPS3Ql0HasHuznieZuRT5mPK6AoPiZZYKNWOy4HTw-Tq5J4vy1T7c0LiKXN8mjEHDPx8WhNVJa04rtZurjr6xPajGwk_v9RD9vvyx93FdXP78-rm4uy28aozc2Nip4ULRnod216B_tOb2MtOVZvRdNiboZU4mBgUKKV9AKkVBC-hDQGjVIfs225v9bZaI832MZHHcXQZqy0rDMi2HVQF9Q70ZSIqGO2ypEdXnq0Au8nQbjO0m4AsKLvN0Oqq-_pywJF3Yywu-0Rv4nYwbddv9n_fcVi__ZewWPIJs8eQCvrZhim9c-k_i0mFtw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18024493</pqid></control><display><type>article</type><title>A note on linear dispersion and shoaling properties in extended Boussinesq equations</title><source>ScienceDirect Freedom Collection</source><creator>Lee, C. ; Cho, Y.-S. ; Yoon, S.B.</creator><creatorcontrib>Lee, C. ; Cho, Y.-S. ; Yoon, S.B.</creatorcontrib><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><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&amp;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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; 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>
fulltext fulltext
identifier ISSN: 0029-8018
ispartof Ocean engineering, 2003-10, Vol.30 (14), p.1849-1867
issn 0029-8018
1873-5258
language eng
recordid cdi_proquest_miscellaneous_18024493
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
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-24T14%3A26%3A01IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20note%20on%20linear%20dispersion%20and%20shoaling%20properties%20in%20extended%20Boussinesq%20equations&rft.jtitle=Ocean%20engineering&rft.au=Lee,%20C.&rft.date=2003-10-01&rft.volume=30&rft.issue=14&rft.spage=1849&rft.epage=1867&rft.pages=1849-1867&rft.issn=0029-8018&rft.eissn=1873-5258&rft.coden=OCENBQ&rft_id=info:doi/10.1016/S0029-8018(03)00015-5&rft_dat=%3Cproquest_cross%3E18024493%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c368t-8f651ad82c5f47305b78f7263018f86e78942e98fd30335cd02530dc204ddef23%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=18024493&rft_id=info:pmid/&rfr_iscdi=true