Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific

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In this work, we consider the primitive equations of an ocean circulation model for the southern pacific, which consists of the time-dependent Navier-Stokes equations in the β-plane coupled with the temperature transport equation. Specifically, the full three-dimensional equations are adopt...

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Detalles Bibliográficos
Autores: Hartmann, Thomas, Stephan, Ernst P., Wick, Thomas
Formato: artículo
Fecha de Publicación:2025
Institución:Universidad Nacional de Trujillo
Repositorio:Revistas - Universidad Nacional de Trujillo
Lenguaje:inglés
OAI Identifier:oai:ojs.revistas.unitru.edu.pe:article/7082
Enlace del recurso:https://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082
Nivel de acceso:acceso abierto
Materia:Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
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spelling Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern PacificNumerical Modeling and Simulations for an Ocean Circulation Model of the Southern PacificHartmann, ThomasStephan, Ernst P.Wick, ThomasNavier-Stokes equationsTemperature modelMonolithic approachGalerkin finite elementsEl NiñoNavier-Stokes equationsTemperature modelMonolithic approachGalerkin finite elementsEl NiñoIn this work, we consider the primitive equations of an ocean circulation model for the southern pacific, which consists of the time-dependent Navier-Stokes equations in the β-plane coupled with the temperature transport equation. Specifically, the full three-dimensional equations are adopted and formulated as a monolithic system of nonstationary, nonlinear, coupled partial differential equations. The El Nino phenomenon is simulated by the action of given wind stresses on the ocean surface. We present an approximation scheme with Crank-Nicolson finite differences in time, and in space we take inf-sup stable Galerkin finite elements for the Navier-Stokes part and bilinear elements for the temperature. We solve the resulting, nonlinear monolithic discrete system by Newton's method. Numerical experiments with realistic geometry and material data are conducted, which show the practicability of our approach.In this work, we consider the primitive equations of an ocean circulation model for the southern pacific, which consists of the time-dependent Navier-Stokes equations in the β-plane coupled with the temperature transport equation. Specifically, the full three-dimensional equations are adopted and formulated as a monolithic system of nonstationary, nonlinear, coupled partial differential equations. The El Nino phenomenon is simulated by the action of given wind stresses on the ocean surface. We present an approximation scheme with Crank-Nicolson finite differences in time, and in space we take inf-sup stable Galerkin finite elements for the Navier-Stokes part and bilinear elements for the temperature. We solve the resulting, nonlinear monolithic discrete system by Newton's method. Numerical experiments with realistic geometry and material data are conducted, which show the practicability of our approach.National University of Trujillo - Academic Department of Mathematics2025-12-27info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082Selecciones Matemáticas; Vol. 12 No. 02 (2025): August - December; 261 - 272Selecciones Matemáticas; Vol. 12 Núm. 02 (2025): Agosto - Diciembre; 261 - 272Selecciones Matemáticas; v. 12 n. 02 (2025): Agosto - Dezembro; 261 - 2722411-1783reponame:Revistas - Universidad Nacional de Trujilloinstname:Universidad Nacional de Trujilloinstacron:UNITRUenghttps://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082/7104https://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessoai:ojs.revistas.unitru.edu.pe:article/70822025-12-27T01:09:48Z
dc.title.none.fl_str_mv Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
title Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
spellingShingle Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
Hartmann, Thomas
Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
title_short Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
title_full Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
title_fullStr Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
title_full_unstemmed Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
title_sort Numerical Modeling and Simulations for an Ocean Circulation Model of the Southern Pacific
dc.creator.none.fl_str_mv Hartmann, Thomas
Stephan, Ernst P.
Wick, Thomas
author Hartmann, Thomas
author_facet Hartmann, Thomas
Stephan, Ernst P.
Wick, Thomas
author_role author
author2 Stephan, Ernst P.
Wick, Thomas
author2_role author
author
dc.subject.none.fl_str_mv Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
topic Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
Navier-Stokes equations
Temperature model
Monolithic approach
Galerkin finite elements
El Niño
description In this work, we consider the primitive equations of an ocean circulation model for the southern pacific, which consists of the time-dependent Navier-Stokes equations in the β-plane coupled with the temperature transport equation. Specifically, the full three-dimensional equations are adopted and formulated as a monolithic system of nonstationary, nonlinear, coupled partial differential equations. The El Nino phenomenon is simulated by the action of given wind stresses on the ocean surface. We present an approximation scheme with Crank-Nicolson finite differences in time, and in space we take inf-sup stable Galerkin finite elements for the Navier-Stokes part and bilinear elements for the temperature. We solve the resulting, nonlinear monolithic discrete system by Newton's method. Numerical experiments with realistic geometry and material data are conducted, which show the practicability of our approach.
publishDate 2025
dc.date.none.fl_str_mv 2025-12-27
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082
url https://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.unitru.edu.pe/index.php/SSMM/article/view/7082/7104
dc.rights.none.fl_str_mv https://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv National University of Trujillo - Academic Department of Mathematics
publisher.none.fl_str_mv National University of Trujillo - Academic Department of Mathematics
dc.source.none.fl_str_mv Selecciones Matemáticas; Vol. 12 No. 02 (2025): August - December; 261 - 272
Selecciones Matemáticas; Vol. 12 Núm. 02 (2025): Agosto - Diciembre; 261 - 272
Selecciones Matemáticas; v. 12 n. 02 (2025): Agosto - Dezembro; 261 - 272
2411-1783
reponame:Revistas - Universidad Nacional de Trujillo
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instacron:UNITRU
instname_str Universidad Nacional de Trujillo
instacron_str UNITRU
institution UNITRU
reponame_str Revistas - Universidad Nacional de Trujillo
collection Revistas - Universidad Nacional de Trujillo
repository.name.fl_str_mv
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