Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre
The amount of cross‐isobath freshwater exchange within the North Atlantic subpolar gyre is estimated from numerical modelling simulations. A regional configuration of the Nucleus for European Modelling of the Ocean model is used to carry out three simulations with horizontal resolutions of 1/4°, 1/1...
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ftunivalberta:oai:era.library.ualberta.ca:cc3488d3-9ca2-48f0-9d1f-ed5d95493c9e 2024-06-23T07:53:18+00:00 Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre Pennelly, Clark Hu, Xianmin Myers, Paul G. 2019-01-01 https://era.library.ualberta.ca/items/cc3488d3-9ca2-48f0-9d1f-ed5d95493c9e https://doi.org/10.7939/r3-m2mk-3n64 English eng https://era.library.ualberta.ca/items/cc3488d3-9ca2-48f0-9d1f-ed5d95493c9e doi:10.7939/r3-m2mk-3n64 © 2019. American Geophysical Union. All Rights Reserved. Boundary currents Freshwater Labrador Sea Numerical modeling Stratification Article (Published) 2019 ftunivalberta https://doi.org/10.7939/r3-m2mk-3n64 2024-06-03T03:09:00Z The amount of cross‐isobath freshwater exchange within the North Atlantic subpolar gyre is estimated from numerical modelling simulations. A regional configuration of the Nucleus for European Modelling of the Ocean model is used to carry out three simulations with horizontal resolutions of 1/4°, 1/12°, and 1/4° with a 1/12° nested domain. Freshwater transport is calculated across five isobaths in six regions for three distinct water masses. Fresh Polar Water is only transported offshore from the western coast of Greenland and the southern coast of Labrador; other regions have onshore transport of freshwater or little offshore transport. The salty water masses of Irminger and Labrador Sea Water typically have onshore transport, acting to promote subsurface freshening of the Labrador Sea. The freshwater transport via the Polar Water mass experiences a large degree of seasonal variability, while the Irminger and Labrador Sea Water masses do not. Decomposing the freshwater transport into the mean and turbulent components indicates that most regions and water masses have stronger freshwater transport associated with the mean flow while the turbulent flow in often the opposite direction. The only water mass and region where the mean and turbulent freshwater transport act in the same direction is Polar Water along the western margin of Greenland. Model resolution plays an important role in determining cross‐isobath exchange as our results from an identically forced simulation at 1/4° has reduced seasonal cycles, reduced transport, and sometimes transport in the opposite direction when compared against the 1/12° resolution simulations. Article in Journal/Newspaper Greenland Labrador Sea North Atlantic University of Alberta: Era - Education and Research Archive Greenland |
institution |
Open Polar |
collection |
University of Alberta: Era - Education and Research Archive |
op_collection_id |
ftunivalberta |
language |
English |
topic |
Boundary currents Freshwater Labrador Sea Numerical modeling Stratification |
spellingShingle |
Boundary currents Freshwater Labrador Sea Numerical modeling Stratification Pennelly, Clark Hu, Xianmin Myers, Paul G. Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
topic_facet |
Boundary currents Freshwater Labrador Sea Numerical modeling Stratification |
description |
The amount of cross‐isobath freshwater exchange within the North Atlantic subpolar gyre is estimated from numerical modelling simulations. A regional configuration of the Nucleus for European Modelling of the Ocean model is used to carry out three simulations with horizontal resolutions of 1/4°, 1/12°, and 1/4° with a 1/12° nested domain. Freshwater transport is calculated across five isobaths in six regions for three distinct water masses. Fresh Polar Water is only transported offshore from the western coast of Greenland and the southern coast of Labrador; other regions have onshore transport of freshwater or little offshore transport. The salty water masses of Irminger and Labrador Sea Water typically have onshore transport, acting to promote subsurface freshening of the Labrador Sea. The freshwater transport via the Polar Water mass experiences a large degree of seasonal variability, while the Irminger and Labrador Sea Water masses do not. Decomposing the freshwater transport into the mean and turbulent components indicates that most regions and water masses have stronger freshwater transport associated with the mean flow while the turbulent flow in often the opposite direction. The only water mass and region where the mean and turbulent freshwater transport act in the same direction is Polar Water along the western margin of Greenland. Model resolution plays an important role in determining cross‐isobath exchange as our results from an identically forced simulation at 1/4° has reduced seasonal cycles, reduced transport, and sometimes transport in the opposite direction when compared against the 1/12° resolution simulations. |
format |
Article in Journal/Newspaper |
author |
Pennelly, Clark Hu, Xianmin Myers, Paul G. |
author_facet |
Pennelly, Clark Hu, Xianmin Myers, Paul G. |
author_sort |
Pennelly, Clark |
title |
Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
title_short |
Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
title_full |
Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
title_fullStr |
Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
title_full_unstemmed |
Cross-Isobath Freshwater Exchange Within the North Atlantic Subpolar Gyre |
title_sort |
cross-isobath freshwater exchange within the north atlantic subpolar gyre |
publishDate |
2019 |
url |
https://era.library.ualberta.ca/items/cc3488d3-9ca2-48f0-9d1f-ed5d95493c9e https://doi.org/10.7939/r3-m2mk-3n64 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Labrador Sea North Atlantic |
genre_facet |
Greenland Labrador Sea North Atlantic |
op_relation |
https://era.library.ualberta.ca/items/cc3488d3-9ca2-48f0-9d1f-ed5d95493c9e doi:10.7939/r3-m2mk-3n64 |
op_rights |
© 2019. American Geophysical Union. All Rights Reserved. |
op_doi |
https://doi.org/10.7939/r3-m2mk-3n64 |
_version_ |
1802644884513882112 |