Lagrangian modelling of frazil ice in the ocean
A new modelling framework using Lagrangian particle tracking has been developed to assess dynamic and thermodynamic effects of underwater frazil ice. This frazil-ice model treats a Lagrangian particle as a bulk cluster of many frazil crystals, and calculates the thermodynamic growth of each particle...
Published in: | Annals of Glaciology |
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Language: | English |
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Online Access: | http://hdl.handle.net/2115/61139 https://doi.org/10.3189/2015AoG69A657 |
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fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/61139 2023-05-15T13:29:12+02:00 Lagrangian modelling of frazil ice in the ocean Matsumura, Yoshimasa Ohshima, Kay I. http://hdl.handle.net/2115/61139 https://doi.org/10.3189/2015AoG69A657 eng eng International Glaciological Society (IGS) http://www.igsoc.org/ http://hdl.handle.net/2115/61139 Annals of glaciology, 56(69): 373-382 http://dx.doi.org/10.3189/2015AoG69A657 © 2015 International Glaciological Society frazil ice ice/ocean interactions sea-ice modelling article fthokunivhus https://doi.org/10.3189/2015AoG69A657 2022-11-18T01:03:41Z A new modelling framework using Lagrangian particle tracking has been developed to assess dynamic and thermodynamic effects of underwater frazil ice. This frazil-ice model treats a Lagrangian particle as a bulk cluster of many frazil crystals, and calculates the thermodynamic growth of each particle and the corresponding budget of latent heat and fresh water. The effective density and viscosity of sea water depend on the mass fraction of underwater frazil ice, and hence affect ocean convection. An idealized experiment using our model successfully reproduces the formation of underwater frazil ice and its transition to grease ice at the surface. Because underwater frazil ice does not reduce the atmosphere/ocean heat exchange, surface heat flux and net sea-ice production in the experiment with frazil ice are relatively high compared with the experiment where surface cooling directly leads to columnar growth of a solid ice cover which effectively insulates the heat flux. These results suggest that large-scale sea-ice models which do not take account of the effects of frazil ice might underestimate atmosphere/ocean heat exchange, particularly at times of active new ice formation. Article in Journal/Newspaper Annals of Glaciology Sea ice Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Annals of Glaciology 56 69 373 382 |
institution |
Open Polar |
collection |
Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) |
op_collection_id |
fthokunivhus |
language |
English |
topic |
frazil ice ice/ocean interactions sea-ice modelling |
spellingShingle |
frazil ice ice/ocean interactions sea-ice modelling Matsumura, Yoshimasa Ohshima, Kay I. Lagrangian modelling of frazil ice in the ocean |
topic_facet |
frazil ice ice/ocean interactions sea-ice modelling |
description |
A new modelling framework using Lagrangian particle tracking has been developed to assess dynamic and thermodynamic effects of underwater frazil ice. This frazil-ice model treats a Lagrangian particle as a bulk cluster of many frazil crystals, and calculates the thermodynamic growth of each particle and the corresponding budget of latent heat and fresh water. The effective density and viscosity of sea water depend on the mass fraction of underwater frazil ice, and hence affect ocean convection. An idealized experiment using our model successfully reproduces the formation of underwater frazil ice and its transition to grease ice at the surface. Because underwater frazil ice does not reduce the atmosphere/ocean heat exchange, surface heat flux and net sea-ice production in the experiment with frazil ice are relatively high compared with the experiment where surface cooling directly leads to columnar growth of a solid ice cover which effectively insulates the heat flux. These results suggest that large-scale sea-ice models which do not take account of the effects of frazil ice might underestimate atmosphere/ocean heat exchange, particularly at times of active new ice formation. |
format |
Article in Journal/Newspaper |
author |
Matsumura, Yoshimasa Ohshima, Kay I. |
author_facet |
Matsumura, Yoshimasa Ohshima, Kay I. |
author_sort |
Matsumura, Yoshimasa |
title |
Lagrangian modelling of frazil ice in the ocean |
title_short |
Lagrangian modelling of frazil ice in the ocean |
title_full |
Lagrangian modelling of frazil ice in the ocean |
title_fullStr |
Lagrangian modelling of frazil ice in the ocean |
title_full_unstemmed |
Lagrangian modelling of frazil ice in the ocean |
title_sort |
lagrangian modelling of frazil ice in the ocean |
publisher |
International Glaciological Society (IGS) |
url |
http://hdl.handle.net/2115/61139 https://doi.org/10.3189/2015AoG69A657 |
genre |
Annals of Glaciology Sea ice |
genre_facet |
Annals of Glaciology Sea ice |
op_relation |
http://www.igsoc.org/ http://hdl.handle.net/2115/61139 Annals of glaciology, 56(69): 373-382 http://dx.doi.org/10.3189/2015AoG69A657 |
op_rights |
© 2015 International Glaciological Society |
op_doi |
https://doi.org/10.3189/2015AoG69A657 |
container_title |
Annals of Glaciology |
container_volume |
56 |
container_issue |
69 |
container_start_page |
373 |
op_container_end_page |
382 |
_version_ |
1765999213799276544 |