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...
Main Authors: | , |
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Format: | Text |
Language: | English |
Published: |
University of Alberta Library
2020
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Online Access: | https://dx.doi.org/10.7939/r3-kp1p-v989 https://ualberta.scholaris.ca/handle/123456789/16611 |
_version_ | 1835011559711047680 |
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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 |