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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Bibliographic Details
Main Author: Aliabadi,Shahrouz
Other Authors: Jackson State University Jackson United States
Format: Text
Language:English
Published: 2016
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD1037351
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1037351
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spelling 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
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
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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