MODELLING OF REFROZEN CRACKS IN SEA ICE

Refrozen cracks in sea ice provide the conditions that allow the investigation of refreez-ing saltwater ice under heat transfer in two dimensions. In this study we investigate the refreezing process of cracks with a numerical model based on the finite volume method with mushy layer treatment after D...

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Main Authors: Chris Petrich, Pat J. Langhorne, Tim G. Haskell
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.5333
http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.501.5333 2023-05-15T18:16:42+02:00 MODELLING OF REFROZEN CRACKS IN SEA ICE Chris Petrich Pat J. Langhorne Tim G. Haskell The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.5333 http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.5333 http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf text ftciteseerx 2016-01-08T09:09:36Z Refrozen cracks in sea ice provide the conditions that allow the investigation of refreez-ing saltwater ice under heat transfer in two dimensions. In this study we investigate the refreezing process of cracks with a numerical model based on the finite volume method with mushy layer treatment after Darcy. The model results are compared to our field data on refrozen cracks 10 to 40 cm wide. We find that numerical sea ice growth modelling is still handicapped by the absence of appropriate permeability parameterizations of the crystal structure. However, we are able to obtain qualitative agreement between model and reality. Text Sea ice Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Refrozen cracks in sea ice provide the conditions that allow the investigation of refreez-ing saltwater ice under heat transfer in two dimensions. In this study we investigate the refreezing process of cracks with a numerical model based on the finite volume method with mushy layer treatment after Darcy. The model results are compared to our field data on refrozen cracks 10 to 40 cm wide. We find that numerical sea ice growth modelling is still handicapped by the absence of appropriate permeability parameterizations of the crystal structure. However, we are able to obtain qualitative agreement between model and reality.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Chris Petrich
Pat J. Langhorne
Tim G. Haskell
spellingShingle Chris Petrich
Pat J. Langhorne
Tim G. Haskell
MODELLING OF REFROZEN CRACKS IN SEA ICE
author_facet Chris Petrich
Pat J. Langhorne
Tim G. Haskell
author_sort Chris Petrich
title MODELLING OF REFROZEN CRACKS IN SEA ICE
title_short MODELLING OF REFROZEN CRACKS IN SEA ICE
title_full MODELLING OF REFROZEN CRACKS IN SEA ICE
title_fullStr MODELLING OF REFROZEN CRACKS IN SEA ICE
title_full_unstemmed MODELLING OF REFROZEN CRACKS IN SEA ICE
title_sort modelling of refrozen cracks in sea ice
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.5333
http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf
genre Sea ice
genre_facet Sea ice
op_source http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.5333
http://www.physics.otago.ac.nz/research/ice/publications/Petrich_IAHR2002.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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