High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean
Hybrid finite element/finite volume based CaMEL shallow water flow solvers have been successfully extended to study wave effects on ice floes in a simplified 10 sq-km ocean domain. Our solver combines the merits of both the finite element and finite volume methods and is much more sophisticated, rob...
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ftdtic:AD1037351 2023-05-15T14:57:11+02:00 High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean Aliabadi,Shahrouz Jackson State University Jackson United States 2016-08-23 text/html http://www.dtic.mil/docs/citations/AD1037351 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1037351 en eng http://www.dtic.mil/docs/citations/AD1037351 Approved For Public Release; Computer Programming and Software Fluid Mechanics Snow Ice and Permafrost high performance computing MARGINAL ICE ZONES SHALLOW WATER FINITE ELEMENT ANALYSIS waves ARCTIC OCEAN computational fluid dynamics fluid flow sea ice dynamics finite volume MIZ (MARGINAL ICE ZONES) ice floes ice chunks cfd (computational fluid dynamics) CaMEL fluid flow solvers Tsunami type waves Circular waves Text 2016 ftdtic 2017-09-17T14:48:44Z Hybrid finite element/finite volume based CaMEL shallow water flow solvers have been successfully extended to study wave effects on ice floes in a simplified 10 sq-km ocean domain. Our solver combines the merits of both the finite element and finite volume methods and is much more sophisticated, robust, super convergent, and is the first of its kind approach extended for studying the dynamics and dispersion of ice chunks in ocean. Apart from studying the influence of waves on rigid, non-moving ice floes, We have also successfully implemented the automatic mesh moving techniques to study the ice kinematics. We have studied the wave-ice interactions using different artificial wave forcing mechanisms impacting, movable isolated ice floes, and also uniformly placed cluster of ice floes that are free to drift. Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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language |
English |
topic |
Computer Programming and Software Fluid Mechanics Snow Ice and Permafrost high performance computing MARGINAL ICE ZONES SHALLOW WATER FINITE ELEMENT ANALYSIS waves ARCTIC OCEAN computational fluid dynamics fluid flow sea ice dynamics finite volume MIZ (MARGINAL ICE ZONES) ice floes ice chunks cfd (computational fluid dynamics) CaMEL fluid flow solvers Tsunami type waves Circular waves |
spellingShingle |
Computer Programming and Software Fluid Mechanics Snow Ice and Permafrost high performance computing MARGINAL ICE ZONES SHALLOW WATER FINITE ELEMENT ANALYSIS waves ARCTIC OCEAN computational fluid dynamics fluid flow sea ice dynamics finite volume MIZ (MARGINAL ICE ZONES) ice floes ice chunks cfd (computational fluid dynamics) CaMEL fluid flow solvers Tsunami type waves Circular waves Aliabadi,Shahrouz High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
topic_facet |
Computer Programming and Software Fluid Mechanics Snow Ice and Permafrost high performance computing MARGINAL ICE ZONES SHALLOW WATER FINITE ELEMENT ANALYSIS waves ARCTIC OCEAN computational fluid dynamics fluid flow sea ice dynamics finite volume MIZ (MARGINAL ICE ZONES) ice floes ice chunks cfd (computational fluid dynamics) CaMEL fluid flow solvers Tsunami type waves Circular waves |
description |
Hybrid finite element/finite volume based CaMEL shallow water flow solvers have been successfully extended to study wave effects on ice floes in a simplified 10 sq-km ocean domain. Our solver combines the merits of both the finite element and finite volume methods and is much more sophisticated, robust, super convergent, and is the first of its kind approach extended for studying the dynamics and dispersion of ice chunks in ocean. Apart from studying the influence of waves on rigid, non-moving ice floes, We have also successfully implemented the automatic mesh moving techniques to study the ice kinematics. We have studied the wave-ice interactions using different artificial wave forcing mechanisms impacting, movable isolated ice floes, and also uniformly placed cluster of ice floes that are free to drift. |
author2 |
Jackson State University Jackson United States |
format |
Text |
author |
Aliabadi,Shahrouz |
author_facet |
Aliabadi,Shahrouz |
author_sort |
Aliabadi,Shahrouz |
title |
High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
title_short |
High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
title_full |
High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
title_fullStr |
High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
title_full_unstemmed |
High Performance Computing Technologies for Modeling the Dynamics and Dispersion of Ice Chunks in the Arctic Ocean |
title_sort |
high performance computing technologies for modeling the dynamics and dispersion of ice chunks in the arctic ocean |
publishDate |
2016 |
url |
http://www.dtic.mil/docs/citations/AD1037351 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1037351 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Ice permafrost Sea ice |
genre_facet |
Arctic Arctic Ocean Ice permafrost Sea ice |
op_relation |
http://www.dtic.mil/docs/citations/AD1037351 |
op_rights |
Approved For Public Release; |
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1766329273374736384 |