An Open Boundary Condition for Numerical Coastal Circulation Models
Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, an appropriate open boundary condition (OBC) is required so that outgoing waves freely pass to the exterior without creating reflections back into the interior of the computational domain. In this pap...
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Veröffentlicht in: | Journal of physical oceanography 2011-12, Vol.41 (12), p.2363-2380 |
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description | Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, an appropriate open boundary condition (OBC) is required so that outgoing waves freely pass to the exterior without creating reflections back into the interior of the computational domain. In this paper, the authors derive, based on the shallow-water equations including bottom friction and neglecting Coriolis effect and by means of nonlinear characteristic analysis, an OBC formulation with two predictive parameters, phase speed cr, and decay time Tf. Simple idealized tests are performed to demonstrate the proposed OBC’s excellent skills in elimination of unwanted reflections at OBs when the motion is periodic, as assumed in its theoretical derivation. It turns out that the formulas for the two OBC parameters become independent of period in the limit of small friction and/or short period. This feature is used to derive an OBC applicable when information about the typical period of the motion to be simulated is unavailable. Simple, idealized tests of this period independent OBC demonstrate its ability to afford excellent results, even when the limitations inherent in its derivation are exceeded. Finally, the OBC is applied in more realistic simulations, including Coriolis effects of 2D tidal flows, and is shown to yield excellent results, especially for residual flows. |
doi_str_mv | 10.1175/2011JPO4574.1 |
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At OBs, an appropriate open boundary condition (OBC) is required so that outgoing waves freely pass to the exterior without creating reflections back into the interior of the computational domain. In this paper, the authors derive, based on the shallow-water equations including bottom friction and neglecting Coriolis effect and by means of nonlinear characteristic analysis, an OBC formulation with two predictive parameters, phase speed cr, and decay time Tf. Simple idealized tests are performed to demonstrate the proposed OBC’s excellent skills in elimination of unwanted reflections at OBs when the motion is periodic, as assumed in its theoretical derivation. It turns out that the formulas for the two OBC parameters become independent of period in the limit of small friction and/or short period. This feature is used to derive an OBC applicable when information about the typical period of the motion to be simulated is unavailable. Simple, idealized tests of this period independent OBC demonstrate its ability to afford excellent results, even when the limitations inherent in its derivation are exceeded. Finally, the OBC is applied in more realistic simulations, including Coriolis effects of 2D tidal flows, and is shown to yield excellent results, especially for residual flows.</description><identifier>ISSN: 0022-3670</identifier><identifier>EISSN: 1520-0485</identifier><identifier>DOI: 10.1175/2011JPO4574.1</identifier><identifier>CODEN: JPYOBT</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Bottom friction ; Boundary conditions ; Coastal circulation ; Coastal circulation models ; Computer applications ; Coriolis effect ; Decay rate ; Derivation ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Friction ; Grain size ; Marine ; Ocean bottom seismometers ; Parameters ; Phase velocity ; Physics of the oceans ; Propagation ; Sediments ; Shallow water ; Shallow water equations ; Shear stress ; Simulation ; Studies ; Tidal flow ; Two dimensional flow ; Velocity</subject><ispartof>Journal of physical oceanography, 2011-12, Vol.41 (12), p.2363-2380</ispartof><rights>2015 INIST-CNRS</rights><rights>Copyright American Meteorological Society 2011</rights><rights>Copyright American Meteorological Society Dec 2011</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c393t-bde570caf8523fdc96fd7ce9bb85f8aa8b4d764cd955e176002e6f484295ede03</citedby><cites>FETCH-LOGICAL-c393t-bde570caf8523fdc96fd7ce9bb85f8aa8b4d764cd955e176002e6f484295ede03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,3681,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25335808$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>PEIFENG MA</creatorcontrib><creatorcontrib>MADSEN, Ole Secher</creatorcontrib><title>An Open Boundary Condition for Numerical Coastal Circulation Models</title><title>Journal of physical oceanography</title><description>Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, an appropriate open boundary condition (OBC) is required so that outgoing waves freely pass to the exterior without creating reflections back into the interior of the computational domain. In this paper, the authors derive, based on the shallow-water equations including bottom friction and neglecting Coriolis effect and by means of nonlinear characteristic analysis, an OBC formulation with two predictive parameters, phase speed cr, and decay time Tf. Simple idealized tests are performed to demonstrate the proposed OBC’s excellent skills in elimination of unwanted reflections at OBs when the motion is periodic, as assumed in its theoretical derivation. It turns out that the formulas for the two OBC parameters become independent of period in the limit of small friction and/or short period. This feature is used to derive an OBC applicable when information about the typical period of the motion to be simulated is unavailable. Simple, idealized tests of this period independent OBC demonstrate its ability to afford excellent results, even when the limitations inherent in its derivation are exceeded. Finally, the OBC is applied in more realistic simulations, including Coriolis effects of 2D tidal flows, and is shown to yield excellent results, especially for residual flows.</description><subject>Bottom friction</subject><subject>Boundary conditions</subject><subject>Coastal circulation</subject><subject>Coastal circulation models</subject><subject>Computer applications</subject><subject>Coriolis effect</subject><subject>Decay rate</subject><subject>Derivation</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Friction</subject><subject>Grain size</subject><subject>Marine</subject><subject>Ocean bottom seismometers</subject><subject>Parameters</subject><subject>Phase velocity</subject><subject>Physics of the oceans</subject><subject>Propagation</subject><subject>Sediments</subject><subject>Shallow water</subject><subject>Shallow water equations</subject><subject>Shear stress</subject><subject>Simulation</subject><subject>Studies</subject><subject>Tidal flow</subject><subject>Two dimensional flow</subject><subject>Velocity</subject><issn>0022-3670</issn><issn>1520-0485</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kEtLw0AUhQdRsFaX7oMirqJ3XsnMsgafVOtC12EyD0hJZ-pMsvDfm9oiIrg6cPnu4fAhdIrhCuOSXxPA-Ol1wXjJrvAemmBOIAcm-D6aABCS06KEQ3SU0hIACkzkBFUzny3W1mc3YfBGxc-sCt60fRt85kLMXoaVja1W3XhXqd9kG_XQqW_iORjbpWN04FSX7Mkup-j97vatesjni_vHajbPNZW0zxtjeQlaOcEJdUbLwplSW9k0gjuhlGiYKQumjeTc4rIYJ9vCMcGI5NZYoFN0ue1dx_Ax2NTXqzZp23XK2zCkWhKKpSzlhjz7Qy7DEP04rpaYUSYoIyN0_h9EBAAGTAQfqXxL6RhSitbV69iuRlE1hnqjvf6lvcYjf7FrVWnU5qLyuk0_T4RTygUI-gVhIIAO</recordid><startdate>20111201</startdate><enddate>20111201</enddate><creator>PEIFENG MA</creator><creator>MADSEN, Ole Secher</creator><general>American Meteorological Society</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>S0X</scope></search><sort><creationdate>20111201</creationdate><title>An Open Boundary Condition for Numerical Coastal Circulation Models</title><author>PEIFENG MA ; 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At OBs, an appropriate open boundary condition (OBC) is required so that outgoing waves freely pass to the exterior without creating reflections back into the interior of the computational domain. In this paper, the authors derive, based on the shallow-water equations including bottom friction and neglecting Coriolis effect and by means of nonlinear characteristic analysis, an OBC formulation with two predictive parameters, phase speed cr, and decay time Tf. Simple idealized tests are performed to demonstrate the proposed OBC’s excellent skills in elimination of unwanted reflections at OBs when the motion is periodic, as assumed in its theoretical derivation. It turns out that the formulas for the two OBC parameters become independent of period in the limit of small friction and/or short period. This feature is used to derive an OBC applicable when information about the typical period of the motion to be simulated is unavailable. Simple, idealized tests of this period independent OBC demonstrate its ability to afford excellent results, even when the limitations inherent in its derivation are exceeded. Finally, the OBC is applied in more realistic simulations, including Coriolis effects of 2D tidal flows, and is shown to yield excellent results, especially for residual flows.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/2011JPO4574.1</doi><tpages>18</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Bottom friction Boundary conditions Coastal circulation Coastal circulation models Computer applications Coriolis effect Decay rate Derivation Earth, ocean, space Exact sciences and technology External geophysics Friction Grain size Marine Ocean bottom seismometers Parameters Phase velocity Physics of the oceans Propagation Sediments Shallow water Shallow water equations Shear stress Simulation Studies Tidal flow Two dimensional flow Velocity |
title | An Open Boundary Condition for Numerical Coastal Circulation Models |
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