Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013
The LAB60 simulation is a coupled ocean sea-ice model (NEMO) that uses grid refinement to achieve high resolution (1/60 of a degree) within the Labrador Sea. This simulation starts in 2002 and will cover a period of over 10 years. This video shows the stratification strength (convective energy) from...
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fttriple:oai:gotriple.eu:10670/1.05lri6 2023-05-15T17:06:06+02:00 Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 Clark Pennelly, Paul G. Myers 2020-04-16 https://doi.org/10.7939/r3-nen0-g831 https://era.library.ualberta.ca/items/550b03e2-6b57-43e7-b8e7-ad03116b26e2 en eng doi:10.7939/r3-nen0-g831 10670/1.05lri6 https://era.library.ualberta.ca/items/550b03e2-6b57-43e7-b8e7-ad03116b26e2 lic_creative-commons ERA : Education and Research Archive geo envir Other https://vocabularies.coar-repositories.org/resource_types/c_1843/ 2020 fttriple https://doi.org/10.7939/r3-nen0-g831 2023-01-22T17:19:26Z The LAB60 simulation is a coupled ocean sea-ice model (NEMO) that uses grid refinement to achieve high resolution (1/60 of a degree) within the Labrador Sea. This simulation starts in 2002 and will cover a period of over 10 years. This video shows the stratification strength (convective energy) from the surface down to 2000m (J m-3) from 2004 through the end of 2013. Higher values indicate stronger stratification and more resistance to convection. This is video 2 in a set of 6 that shows the results of our LAB60 simulation. A few frames are missing due to file problems. Other/Unknown Material Labrador Sea Sea ice Unknown |
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geo envir Clark Pennelly, Paul G. Myers Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
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geo envir |
description |
The LAB60 simulation is a coupled ocean sea-ice model (NEMO) that uses grid refinement to achieve high resolution (1/60 of a degree) within the Labrador Sea. This simulation starts in 2002 and will cover a period of over 10 years. This video shows the stratification strength (convective energy) from the surface down to 2000m (J m-3) from 2004 through the end of 2013. Higher values indicate stronger stratification and more resistance to convection. This is video 2 in a set of 6 that shows the results of our LAB60 simulation. A few frames are missing due to file problems. |
format |
Other/Unknown Material |
author |
Clark Pennelly, Paul G. Myers |
author_facet |
Clark Pennelly, Paul G. Myers |
author_sort |
Clark Pennelly, |
title |
Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
title_short |
Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
title_full |
Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
title_fullStr |
Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
title_full_unstemmed |
Stratification strength of the LAB60 ocean sea-ice simulation: 2004-2013 |
title_sort |
stratification strength of the lab60 ocean sea-ice simulation: 2004-2013 |
publishDate |
2020 |
url |
https://doi.org/10.7939/r3-nen0-g831 https://era.library.ualberta.ca/items/550b03e2-6b57-43e7-b8e7-ad03116b26e2 |
genre |
Labrador Sea Sea ice |
genre_facet |
Labrador Sea Sea ice |
op_source |
ERA : Education and Research Archive |
op_relation |
doi:10.7939/r3-nen0-g831 10670/1.05lri6 https://era.library.ualberta.ca/items/550b03e2-6b57-43e7-b8e7-ad03116b26e2 |
op_rights |
lic_creative-commons |
op_doi |
https://doi.org/10.7939/r3-nen0-g831 |
_version_ |
1766061090300493824 |