A coupled finite and boundary spectral element method for linear water-wave propagation problems
•A coupled finite and boundary spectral element method for linear water-wave propagation problems is proposed.•Boundary spectral element method (BSEM) is a new technique that combines the advantages of the spectral approach and the BEM.•BSEM has been applied to the mild-slope equation with variable...
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Veröffentlicht in: | Applied Mathematical Modelling 2017-08, Vol.48, p.1-20 |
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description | •A coupled finite and boundary spectral element method for linear water-wave propagation problems is proposed.•Boundary spectral element method (BSEM) is a new technique that combines the advantages of the spectral approach and the BEM.•BSEM has been applied to the mild-slope equation with variable bathymetry in one direction.•A convergence study has been made for the BSEM alone and coupled with finite spectral elements.•The proposed formulation has been validated by solving classical water-wave propagation problems.
A coupled boundary spectral element method (BSEM) and spectral element method (SEM) formulation for the propagation of small-amplitude water waves over variable bathymetries is presented in this work. The wave model is based on the mild-slope equation (MSE), which provides a good approximation of the propagation of water waves over irregular bottom surfaces with slopes up to 1:3. In unbounded domains or infinite regions, space can be divided into two different areas: a central region of interest, where an irregular bathymetry is included, and an exterior infinite region with straight and parallel bathymetric lines. The SEM allows us to model the central region, where any variation of the bathymetry can be considered, while the exterior infinite region is modelled by the BSEM which, combined with the fundamental solution presented by Cerrato et al. [A. Cerrato, J. A. González, L. Rodríguez-Tembleque, Boundary element formulation of the mild-slope equation for harmonic water waves propagating over unidirectional variable bathymetries, Eng. Anal. Boundary Elem. 62 (2016) 22–34.] can include bathymetries with straight and parallel contour lines. This coupled model combines important advantages of both methods; it benefits from the flexibility of the SEM for the interior region and, at the same time, includes the fulfilment of the Sommerfeld’s radiation condition for the exterior problem, that is provided by the BSEM. The solution approximation inside the elements is constructed by high order Legendre polynomials associated with Legendre–Gauss–Lobatto quadrature points, providing a spectral convergence for both methods. The proposed formulation has been validated in three different benchmark cases with different shapes of the bottom surface. The solutions exhibit the typical p-convergence of spectral methods. |
doi_str_mv | 10.1016/j.apm.2017.03.061 |
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A coupled boundary spectral element method (BSEM) and spectral element method (SEM) formulation for the propagation of small-amplitude water waves over variable bathymetries is presented in this work. The wave model is based on the mild-slope equation (MSE), which provides a good approximation of the propagation of water waves over irregular bottom surfaces with slopes up to 1:3. In unbounded domains or infinite regions, space can be divided into two different areas: a central region of interest, where an irregular bathymetry is included, and an exterior infinite region with straight and parallel bathymetric lines. The SEM allows us to model the central region, where any variation of the bathymetry can be considered, while the exterior infinite region is modelled by the BSEM which, combined with the fundamental solution presented by Cerrato et al. [A. Cerrato, J. A. González, L. Rodríguez-Tembleque, Boundary element formulation of the mild-slope equation for harmonic water waves propagating over unidirectional variable bathymetries, Eng. Anal. Boundary Elem. 62 (2016) 22–34.] can include bathymetries with straight and parallel contour lines. This coupled model combines important advantages of both methods; it benefits from the flexibility of the SEM for the interior region and, at the same time, includes the fulfilment of the Sommerfeld’s radiation condition for the exterior problem, that is provided by the BSEM. The solution approximation inside the elements is constructed by high order Legendre polynomials associated with Legendre–Gauss–Lobatto quadrature points, providing a spectral convergence for both methods. The proposed formulation has been validated in three different benchmark cases with different shapes of the bottom surface. The solutions exhibit the typical p-convergence of spectral methods.</description><identifier>ISSN: 0307-904X</identifier><identifier>ISSN: 1088-8691</identifier><identifier>EISSN: 0307-904X</identifier><identifier>DOI: 10.1016/j.apm.2017.03.061</identifier><language>eng</language><publisher>New York: Elsevier Inc</publisher><subject>Approximation ; Bathymetry ; BEM–FEM coupling ; Boundary element method ; Convergence ; Finite element analysis ; Mild-slope equation ; Propagation ; Spectral element method ; Spectral element methods ; Spectral methods ; Studies ; Water waves ; Wave propagation</subject><ispartof>Applied Mathematical Modelling, 2017-08, Vol.48, p.1-20</ispartof><rights>2017 Elsevier Inc.</rights><rights>Copyright Elsevier BV Aug 2017</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c368t-149a52473429adc51e7db40a44aef45e736a97eac89ff28e70bca2038d739b4e3</citedby><cites>FETCH-LOGICAL-c368t-149a52473429adc51e7db40a44aef45e736a97eac89ff28e70bca2038d739b4e3</cites><orcidid>0000-0003-2993-8361</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.apm.2017.03.061$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3548,27922,27923,45993</link.rule.ids></links><search><creatorcontrib>Cerrato, Antonio</creatorcontrib><creatorcontrib>Rodríguez-Tembleque, Luis</creatorcontrib><creatorcontrib>González, José A.</creatorcontrib><creatorcontrib>Ferri Aliabadi, M.H.</creatorcontrib><title>A coupled finite and boundary spectral element method for linear water-wave propagation problems</title><title>Applied Mathematical Modelling</title><description>•A coupled finite and boundary spectral element method for linear water-wave propagation problems is proposed.•Boundary spectral element method (BSEM) is a new technique that combines the advantages of the spectral approach and the BEM.•BSEM has been applied to the mild-slope equation with variable bathymetry in one direction.•A convergence study has been made for the BSEM alone and coupled with finite spectral elements.•The proposed formulation has been validated by solving classical water-wave propagation problems.
A coupled boundary spectral element method (BSEM) and spectral element method (SEM) formulation for the propagation of small-amplitude water waves over variable bathymetries is presented in this work. The wave model is based on the mild-slope equation (MSE), which provides a good approximation of the propagation of water waves over irregular bottom surfaces with slopes up to 1:3. In unbounded domains or infinite regions, space can be divided into two different areas: a central region of interest, where an irregular bathymetry is included, and an exterior infinite region with straight and parallel bathymetric lines. The SEM allows us to model the central region, where any variation of the bathymetry can be considered, while the exterior infinite region is modelled by the BSEM which, combined with the fundamental solution presented by Cerrato et al. [A. Cerrato, J. A. González, L. Rodríguez-Tembleque, Boundary element formulation of the mild-slope equation for harmonic water waves propagating over unidirectional variable bathymetries, Eng. Anal. Boundary Elem. 62 (2016) 22–34.] can include bathymetries with straight and parallel contour lines. This coupled model combines important advantages of both methods; it benefits from the flexibility of the SEM for the interior region and, at the same time, includes the fulfilment of the Sommerfeld’s radiation condition for the exterior problem, that is provided by the BSEM. The solution approximation inside the elements is constructed by high order Legendre polynomials associated with Legendre–Gauss–Lobatto quadrature points, providing a spectral convergence for both methods. The proposed formulation has been validated in three different benchmark cases with different shapes of the bottom surface. The solutions exhibit the typical p-convergence of spectral methods.</description><subject>Approximation</subject><subject>Bathymetry</subject><subject>BEM–FEM coupling</subject><subject>Boundary element method</subject><subject>Convergence</subject><subject>Finite element analysis</subject><subject>Mild-slope equation</subject><subject>Propagation</subject><subject>Spectral element method</subject><subject>Spectral element methods</subject><subject>Spectral methods</subject><subject>Studies</subject><subject>Water waves</subject><subject>Wave propagation</subject><issn>0307-904X</issn><issn>1088-8691</issn><issn>0307-904X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LxDAQhosouK7-AG8Bz62TJm03eFoWv0DwouAtTtOppnSbmnR38d-bZT148jTvwPvOx5MklxwyDry87jIc11kOvMpAZFDyo2QGAqpUgXw7_qNPk7MQOgAoYjdL3pfMuM3YU8NaO9iJGA4Nq91maNB_szCSmTz2jHpa0zCxNU2fLnqdZ70dCD3b4UQ-3eGW2OjdiB84WTfsdR0z4Tw5abEPdPFb58nr3e3L6iF9er5_XC2fUiPKxZRyqbDIZSVkrrAxBaeqqSWglEitLKgSJaqK0CxU2-YLqqA2mINYNJVQtSQxT64Oc-Pirw2FSXdu44e4UnMlcq5ASRld_OAy3oXgqdWjt-v4qeag9yB1pyNIvQepQegIMmZuDhmK528teR2MpcFQY32koxtn_0n_AOe7fME</recordid><startdate>201708</startdate><enddate>201708</enddate><creator>Cerrato, Antonio</creator><creator>Rodríguez-Tembleque, Luis</creator><creator>González, José A.</creator><creator>Ferri Aliabadi, M.H.</creator><general>Elsevier Inc</general><general>Elsevier BV</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SC</scope><scope>8FD</scope><scope>JQ2</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope><orcidid>https://orcid.org/0000-0003-2993-8361</orcidid></search><sort><creationdate>201708</creationdate><title>A coupled finite and boundary spectral element method for linear water-wave propagation problems</title><author>Cerrato, Antonio ; Rodríguez-Tembleque, Luis ; González, José A. ; Ferri Aliabadi, M.H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c368t-149a52473429adc51e7db40a44aef45e736a97eac89ff28e70bca2038d739b4e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Approximation</topic><topic>Bathymetry</topic><topic>BEM–FEM coupling</topic><topic>Boundary element method</topic><topic>Convergence</topic><topic>Finite element analysis</topic><topic>Mild-slope equation</topic><topic>Propagation</topic><topic>Spectral element method</topic><topic>Spectral element methods</topic><topic>Spectral methods</topic><topic>Studies</topic><topic>Water waves</topic><topic>Wave propagation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cerrato, Antonio</creatorcontrib><creatorcontrib>Rodríguez-Tembleque, Luis</creatorcontrib><creatorcontrib>González, José A.</creatorcontrib><creatorcontrib>Ferri Aliabadi, M.H.</creatorcontrib><collection>CrossRef</collection><collection>Computer and Information Systems Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Computer and Information Systems Abstracts Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><jtitle>Applied Mathematical Modelling</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cerrato, Antonio</au><au>Rodríguez-Tembleque, Luis</au><au>González, José A.</au><au>Ferri Aliabadi, M.H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A coupled finite and boundary spectral element method for linear water-wave propagation problems</atitle><jtitle>Applied Mathematical Modelling</jtitle><date>2017-08</date><risdate>2017</risdate><volume>48</volume><spage>1</spage><epage>20</epage><pages>1-20</pages><issn>0307-904X</issn><issn>1088-8691</issn><eissn>0307-904X</eissn><abstract>•A coupled finite and boundary spectral element method for linear water-wave propagation problems is proposed.•Boundary spectral element method (BSEM) is a new technique that combines the advantages of the spectral approach and the BEM.•BSEM has been applied to the mild-slope equation with variable bathymetry in one direction.•A convergence study has been made for the BSEM alone and coupled with finite spectral elements.•The proposed formulation has been validated by solving classical water-wave propagation problems.
A coupled boundary spectral element method (BSEM) and spectral element method (SEM) formulation for the propagation of small-amplitude water waves over variable bathymetries is presented in this work. The wave model is based on the mild-slope equation (MSE), which provides a good approximation of the propagation of water waves over irregular bottom surfaces with slopes up to 1:3. In unbounded domains or infinite regions, space can be divided into two different areas: a central region of interest, where an irregular bathymetry is included, and an exterior infinite region with straight and parallel bathymetric lines. The SEM allows us to model the central region, where any variation of the bathymetry can be considered, while the exterior infinite region is modelled by the BSEM which, combined with the fundamental solution presented by Cerrato et al. [A. Cerrato, J. A. González, L. Rodríguez-Tembleque, Boundary element formulation of the mild-slope equation for harmonic water waves propagating over unidirectional variable bathymetries, Eng. Anal. Boundary Elem. 62 (2016) 22–34.] can include bathymetries with straight and parallel contour lines. This coupled model combines important advantages of both methods; it benefits from the flexibility of the SEM for the interior region and, at the same time, includes the fulfilment of the Sommerfeld’s radiation condition for the exterior problem, that is provided by the BSEM. The solution approximation inside the elements is constructed by high order Legendre polynomials associated with Legendre–Gauss–Lobatto quadrature points, providing a spectral convergence for both methods. The proposed formulation has been validated in three different benchmark cases with different shapes of the bottom surface. The solutions exhibit the typical p-convergence of spectral methods.</abstract><cop>New York</cop><pub>Elsevier Inc</pub><doi>10.1016/j.apm.2017.03.061</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0003-2993-8361</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Approximation Bathymetry BEM–FEM coupling Boundary element method Convergence Finite element analysis Mild-slope equation Propagation Spectral element method Spectral element methods Spectral methods Studies Water waves Wave propagation |
title | A coupled finite and boundary spectral element method for linear water-wave propagation problems |
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