Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study

This article presents a model study of the dynamics of icebergs and surface floats in the Labrador Sea. The model was forced with data on the wind above the ocean surface, surface waves, and ocean currents. These data were obtained from the reanalysis of near-surface characteristics of the ocean and...

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Published in:Journal of Marine Science and Engineering
Main Authors: Jamseena Parayil, Entcho Demirov, Yakov D. Afanasyev
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/jmse10091167
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spelling ftmdpi:oai:mdpi.com:/2077-1312/10/9/1167/ 2023-08-20T04:06:56+02:00 Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study Jamseena Parayil Entcho Demirov Yakov D. Afanasyev agris 2022-08-23 application/pdf https://doi.org/10.3390/jmse10091167 EN eng Multidisciplinary Digital Publishing Institute Physical Oceanography https://dx.doi.org/10.3390/jmse10091167 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 10; Issue 9; Pages: 1167 ocean icebergs surface floats ocean currents ocean modeling Text 2022 ftmdpi https://doi.org/10.3390/jmse10091167 2023-08-01T06:10:49Z This article presents a model study of the dynamics of icebergs and surface floats in the Labrador Sea. The model was forced with data on the wind above the ocean surface, surface waves, and ocean currents. These data were obtained from the reanalysis of near-surface characteristics of the ocean and atmosphere for the year 2008. Icebergs and floats launched in an area north of the Labrador coast and to the east of Greenland generally move southeastward until they reach a boundary current “highway”. After that, they are carried by ocean currents into the central part of the subpolar North Atlantic. Simulations demonstrated that, for smaller icebergs, the primary balance is between the air and water drag, while for larger icebergs, it is between three forces: the air and water drag and the combined Coriolis and pressure forces. Floats, on the other hand, are driven mostly by the Ekman component of the surface velocity, while the geostrophic and Stokes components are less important. The significant variability in the motion of icebergs and floats is due to storms passing over the Labrador Sea, since these high-wind events introduce time-dependent dynamics. Text Greenland Labrador Sea North Atlantic MDPI Open Access Publishing Greenland Journal of Marine Science and Engineering 10 9 1167
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ocean icebergs
surface floats
ocean currents
ocean modeling
spellingShingle ocean icebergs
surface floats
ocean currents
ocean modeling
Jamseena Parayil
Entcho Demirov
Yakov D. Afanasyev
Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
topic_facet ocean icebergs
surface floats
ocean currents
ocean modeling
description This article presents a model study of the dynamics of icebergs and surface floats in the Labrador Sea. The model was forced with data on the wind above the ocean surface, surface waves, and ocean currents. These data were obtained from the reanalysis of near-surface characteristics of the ocean and atmosphere for the year 2008. Icebergs and floats launched in an area north of the Labrador coast and to the east of Greenland generally move southeastward until they reach a boundary current “highway”. After that, they are carried by ocean currents into the central part of the subpolar North Atlantic. Simulations demonstrated that, for smaller icebergs, the primary balance is between the air and water drag, while for larger icebergs, it is between three forces: the air and water drag and the combined Coriolis and pressure forces. Floats, on the other hand, are driven mostly by the Ekman component of the surface velocity, while the geostrophic and Stokes components are less important. The significant variability in the motion of icebergs and floats is due to storms passing over the Labrador Sea, since these high-wind events introduce time-dependent dynamics.
format Text
author Jamseena Parayil
Entcho Demirov
Yakov D. Afanasyev
author_facet Jamseena Parayil
Entcho Demirov
Yakov D. Afanasyev
author_sort Jamseena Parayil
title Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
title_short Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
title_full Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
title_fullStr Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
title_full_unstemmed Effects of Wind, Waves, and Currents on Icebergs and Surface Floats in the Labrador Sea: A Modeling Study
title_sort effects of wind, waves, and currents on icebergs and surface floats in the labrador sea: a modeling study
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/jmse10091167
op_coverage agris
geographic Greenland
geographic_facet Greenland
genre Greenland
Labrador Sea
North Atlantic
genre_facet Greenland
Labrador Sea
North Atlantic
op_source Journal of Marine Science and Engineering; Volume 10; Issue 9; Pages: 1167
op_relation Physical Oceanography
https://dx.doi.org/10.3390/jmse10091167
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse10091167
container_title Journal of Marine Science and Engineering
container_volume 10
container_issue 9
container_start_page 1167
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