Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...

A high-resolution coupled ocean–sea ice model is set up within the Labrador Sea. With a horizontal resolution of 1/60◦ , this simulation is capable of resolving the multitude of eddies that transport heat and freshwater into the interior of the Labrador Sea. These fluxes strongly govern the overall...

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Bibliographic Details
Main Authors: Pennelly, Clark, Myers, Paul G.
Format: Text
Language:English
Published: University of Alberta Library 2020
Subjects:
Online Access:https://dx.doi.org/10.7939/r3-kp1p-v989
https://ualberta.scholaris.ca/handle/123456789/16611
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author Pennelly, Clark
Myers, Paul G.
author_facet Pennelly, Clark
Myers, Paul G.
author_sort Pennelly, Clark
collection Unknown
description A high-resolution coupled ocean–sea ice model is set up within the Labrador Sea. With a horizontal resolution of 1/60◦ , this simulation is capable of resolving the multitude of eddies that transport heat and freshwater into the interior of the Labrador Sea. These fluxes strongly govern the overall stratification, deep convection, restratification, and production of Labrador Sea Water. Our regional configuration spans the full North Atlantic and Arctic; however, high resolution is only applied in smaller nested domains within the North Atlantic and Labrador Sea. Using nesting reduces computational costs and allows for a long simulation from 2002 to the near present. Three passive tracers are also included: Greenland runoff, Labrador Sea Water produced during convection, and Irminger Water that enters the Labrador Sea along Greenland. We describe the configuration setup and compare it against similarly forced lower-resolution simulations to better describe how horizontal resolution impacts the representation ...
format Text
genre Arctic
Greenland
Labrador Sea
North Atlantic
Sea ice
genre_facet Arctic
Greenland
Labrador Sea
North Atlantic
Sea ice
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
id ftdatacite:10.7939/r3-kp1p-v989
institution Open Polar
language English
op_collection_id ftdatacite
op_doi https://doi.org/10.7939/r3-kp1p-v989
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
publishDate 2020
publisher University of Alberta Library
record_format openpolar
spelling ftdatacite:10.7939/r3-kp1p-v989 2025-06-15T14:21:28+00:00 Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ... Pennelly, Clark Myers, Paul G. 2020 https://dx.doi.org/10.7939/r3-kp1p-v989 https://ualberta.scholaris.ca/handle/123456789/16611 en eng University of Alberta Library Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Fresh-water transport Deep convection Mesoscale eddies Impact Circulation Heat model Variability Sensitivity Resolution Text Journal Article (Published) article-journal ScholarlyArticle 2020 ftdatacite https://doi.org/10.7939/r3-kp1p-v989 2025-06-02T13:03:05Z A high-resolution coupled ocean–sea ice model is set up within the Labrador Sea. With a horizontal resolution of 1/60◦ , this simulation is capable of resolving the multitude of eddies that transport heat and freshwater into the interior of the Labrador Sea. These fluxes strongly govern the overall stratification, deep convection, restratification, and production of Labrador Sea Water. Our regional configuration spans the full North Atlantic and Arctic; however, high resolution is only applied in smaller nested domains within the North Atlantic and Labrador Sea. Using nesting reduces computational costs and allows for a long simulation from 2002 to the near present. Three passive tracers are also included: Greenland runoff, Labrador Sea Water produced during convection, and Irminger Water that enters the Labrador Sea along Greenland. We describe the configuration setup and compare it against similarly forced lower-resolution simulations to better describe how horizontal resolution impacts the representation ... Text Arctic Greenland Labrador Sea North Atlantic Sea ice Unknown Arctic Greenland
spellingShingle Fresh-water transport
Deep convection
Mesoscale eddies
Impact
Circulation
Heat model
Variability
Sensitivity
Resolution
Pennelly, Clark
Myers, Paul G.
Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title_full Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title_fullStr Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title_full_unstemmed Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title_short Introducing LAB60: A 1/60 degree NEMO 3.6 numerical simulation of the Labrador Sea ...
title_sort introducing lab60: a 1/60 degree nemo 3.6 numerical simulation of the labrador sea ...
topic Fresh-water transport
Deep convection
Mesoscale eddies
Impact
Circulation
Heat model
Variability
Sensitivity
Resolution
topic_facet Fresh-water transport
Deep convection
Mesoscale eddies
Impact
Circulation
Heat model
Variability
Sensitivity
Resolution
url https://dx.doi.org/10.7939/r3-kp1p-v989
https://ualberta.scholaris.ca/handle/123456789/16611