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...

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Published in:Annals of Glaciology
Main Authors: Matsumura, Yoshimasa, Ohshima, Kay I.
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society (IGS)
Subjects:
Online Access:http://hdl.handle.net/2115/61139
https://doi.org/10.3189/2015AoG69A657
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author Matsumura, Yoshimasa
Ohshima, Kay I.
author_facet Matsumura, Yoshimasa
Ohshima, Kay I.
author_sort Matsumura, Yoshimasa
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
container_issue 69
container_start_page 373
container_title Annals of Glaciology
container_volume 56
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
genre Annals of Glaciology
Sea ice
genre_facet Annals of Glaciology
Sea ice
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/61139
institution Open Polar
language English
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op_container_end_page 382
op_doi https://doi.org/10.3189/2015AoG69A657
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
publisher International Glaciological Society (IGS)
record_format openpolar
spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/61139 2025-01-16T18:59:43+00:00 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
spellingShingle frazil ice
ice/ocean interactions
sea-ice modelling
Matsumura, Yoshimasa
Ohshima, Kay I.
Lagrangian modelling of frazil ice in the ocean
title 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_short Lagrangian modelling of frazil ice in the ocean
title_sort lagrangian modelling of frazil ice in the ocean
topic frazil ice
ice/ocean interactions
sea-ice modelling
topic_facet frazil ice
ice/ocean interactions
sea-ice modelling
url http://hdl.handle.net/2115/61139
https://doi.org/10.3189/2015AoG69A657