Ice/Ocean Interactions

This is a simulation of a body of warm salty water placed next to an ice face (left). The warm ocean melts the ice, which decreases the temperature and salinity of water close to the ice/ocean interface. This more buoyant fluid rises creating a turbulent plume, which entrains more warm and salty wat...

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Main Authors: Gahounzo, Yao, Kopera, Michal
Format: Text
Language:unknown
Published: ScholarWorks 2023
Subjects:
Online Access:https://scholarworks.boisestate.edu/rcd_2023/2
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spelling ftboisestateu:oai:scholarworks.boisestate.edu:rcd_2023-1001 2023-10-29T02:36:43+01:00 Ice/Ocean Interactions Gahounzo, Yao Kopera, Michal 2023-03-28T07:00:00Z video/mp4 https://scholarworks.boisestate.edu/rcd_2023/2 unknown ScholarWorks https://scholarworks.boisestate.edu/rcd_2023/2 Research Computing Days 2023 text 2023 ftboisestateu 2023-09-29T15:04:11Z This is a simulation of a body of warm salty water placed next to an ice face (left). The warm ocean melts the ice, which decreases the temperature and salinity of water close to the ice/ocean interface. This more buoyant fluid rises creating a turbulent plume, which entrains more warm and salty water and creates a circulation in the initially static system. The simulation was done using Non-hydrostatic Unified Model of the Ocean (NUMO). The model is using advanced numerical methods (discontinuous and continuous Galerkin) and ice/ocean boundary conditions developed by Yao Gahounzo for his PhD in Computing thesis. This simulation is one of the benchmarks for the model aiming to simulate the interaction of ice and ocean in Greenland fjords. Text Greenland Boise State University: Scholar Works
institution Open Polar
collection Boise State University: Scholar Works
op_collection_id ftboisestateu
language unknown
description This is a simulation of a body of warm salty water placed next to an ice face (left). The warm ocean melts the ice, which decreases the temperature and salinity of water close to the ice/ocean interface. This more buoyant fluid rises creating a turbulent plume, which entrains more warm and salty water and creates a circulation in the initially static system. The simulation was done using Non-hydrostatic Unified Model of the Ocean (NUMO). The model is using advanced numerical methods (discontinuous and continuous Galerkin) and ice/ocean boundary conditions developed by Yao Gahounzo for his PhD in Computing thesis. This simulation is one of the benchmarks for the model aiming to simulate the interaction of ice and ocean in Greenland fjords.
format Text
author Gahounzo, Yao
Kopera, Michal
spellingShingle Gahounzo, Yao
Kopera, Michal
Ice/Ocean Interactions
author_facet Gahounzo, Yao
Kopera, Michal
author_sort Gahounzo, Yao
title Ice/Ocean Interactions
title_short Ice/Ocean Interactions
title_full Ice/Ocean Interactions
title_fullStr Ice/Ocean Interactions
title_full_unstemmed Ice/Ocean Interactions
title_sort ice/ocean interactions
publisher ScholarWorks
publishDate 2023
url https://scholarworks.boisestate.edu/rcd_2023/2
genre Greenland
genre_facet Greenland
op_source Research Computing Days 2023
op_relation https://scholarworks.boisestate.edu/rcd_2023/2
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