Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland

On 29 April 2015, four beacons were deployed onto an ice island in the Strait of Belle Isle to record positional data. The ice island later broke up into many fragments, four of which were tracked by the beacons. The relative influences of wind drag, current drag, Coriolis force, sea surface height...

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Published in:Journal of Glaciology
Main Authors: Zeinali Torbati, R. (Reza), Turnbull, I.D. (Ian D.), Taylor, R.S. (Rocky S.), Mueller, D. (Derek)
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://ir.library.carleton.ca/pub/26174
https://doi.org/10.1017/jog.2019.96
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spelling ftcarletonunivir:oai:carleton.ca:26174 2023-05-15T16:57:10+02:00 Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland Zeinali Torbati, R. (Reza) Turnbull, I.D. (Ian D.) Taylor, R.S. (Rocky S.) Mueller, D. (Derek) 2019-01-01 application/pdf https://ir.library.carleton.ca/pub/26174 https://doi.org/10.1017/jog.2019.96 en eng https://ir.library.carleton.ca/pub/26174 doi:10.1017/jog.2019.96 info:eu-repo/semantics/openAccess Journal of Glaciology Atmospheric and oceanic forces basal ablation ice island deterioration ice island drift sea-ice force surface ablation info:eu-repo/semantics/article 2019 ftcarletonunivir https://doi.org/10.1017/jog.2019.96 2022-02-06T21:51:19Z On 29 April 2015, four beacons were deployed onto an ice island in the Strait of Belle Isle to record positional data. The ice island later broke up into many fragments, four of which were tracked by the beacons. The relative influences of wind drag, current drag, Coriolis force, sea surface height gradient and sea-ice force on the drift of the tracked ice island fragments were analyzed. Using atmospheric and oceanic model outputs, the sea-ice force was calculated as the residual of the fragments' net forces and the sum of all other forces. This was compared against the force obtained through ice concentration-dependent relationships when sea ice was present. The sea-ice forces calculated from the residual approach and concentration-dependent relationships were significant only when sea ice was present at medium-high concentrations in the vicinity of the ice island fragments. The forces from ocean currents and sea surface tilt contributed the most to the drift of the i Article in Journal/Newspaper Journal of Glaciology Newfoundland Sea ice Strait of Belle Isle Carleton University's Institutional Repository Belle Isle ENVELOPE(-55.357,-55.357,51.942,51.942) Strait of Belle Isle ENVELOPE(-57.115,-57.115,51.400,51.400) Journal of Glaciology 66 256 203 218
institution Open Polar
collection Carleton University's Institutional Repository
op_collection_id ftcarletonunivir
language English
topic Atmospheric and oceanic forces
basal ablation
ice island deterioration
ice island drift
sea-ice force
surface ablation
spellingShingle Atmospheric and oceanic forces
basal ablation
ice island deterioration
ice island drift
sea-ice force
surface ablation
Zeinali Torbati, R. (Reza)
Turnbull, I.D. (Ian D.)
Taylor, R.S. (Rocky S.)
Mueller, D. (Derek)
Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
topic_facet Atmospheric and oceanic forces
basal ablation
ice island deterioration
ice island drift
sea-ice force
surface ablation
description On 29 April 2015, four beacons were deployed onto an ice island in the Strait of Belle Isle to record positional data. The ice island later broke up into many fragments, four of which were tracked by the beacons. The relative influences of wind drag, current drag, Coriolis force, sea surface height gradient and sea-ice force on the drift of the tracked ice island fragments were analyzed. Using atmospheric and oceanic model outputs, the sea-ice force was calculated as the residual of the fragments' net forces and the sum of all other forces. This was compared against the force obtained through ice concentration-dependent relationships when sea ice was present. The sea-ice forces calculated from the residual approach and concentration-dependent relationships were significant only when sea ice was present at medium-high concentrations in the vicinity of the ice island fragments. The forces from ocean currents and sea surface tilt contributed the most to the drift of the i
format Article in Journal/Newspaper
author Zeinali Torbati, R. (Reza)
Turnbull, I.D. (Ian D.)
Taylor, R.S. (Rocky S.)
Mueller, D. (Derek)
author_facet Zeinali Torbati, R. (Reza)
Turnbull, I.D. (Ian D.)
Taylor, R.S. (Rocky S.)
Mueller, D. (Derek)
author_sort Zeinali Torbati, R. (Reza)
title Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
title_short Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
title_full Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
title_fullStr Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
title_full_unstemmed Evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore Newfoundland
title_sort evaluation of the relative contribution of meteorological and oceanic forces to the drift of ice islands offshore newfoundland
publishDate 2019
url https://ir.library.carleton.ca/pub/26174
https://doi.org/10.1017/jog.2019.96
long_lat ENVELOPE(-55.357,-55.357,51.942,51.942)
ENVELOPE(-57.115,-57.115,51.400,51.400)
geographic Belle Isle
Strait of Belle Isle
geographic_facet Belle Isle
Strait of Belle Isle
genre Journal of Glaciology
Newfoundland
Sea ice
Strait of Belle Isle
genre_facet Journal of Glaciology
Newfoundland
Sea ice
Strait of Belle Isle
op_source Journal of Glaciology
op_relation https://ir.library.carleton.ca/pub/26174
doi:10.1017/jog.2019.96
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1017/jog.2019.96
container_title Journal of Glaciology
container_volume 66
container_issue 256
container_start_page 203
op_container_end_page 218
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