Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME
Author Posting. © American Meteorological Society, 2016. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 46 (2016): 1717-1734, doi:10.1175/JPO-D-15-0124.1....
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/8059 2023-05-15T16:30:16+02:00 Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME de Jong, Marieke F. Bower, Amy S. Furey, Heather H. 2016-05-23 https://hdl.handle.net/1912/8059 en_US eng American Meteorological Society https://doi.org/10.1175/JPO-D-15-0124.1 Journal of Physical Oceanography 46 (2016): 1717-1734 https://hdl.handle.net/1912/8059 doi:10.1175/JPO-D-15-0124.1 Journal of Physical Oceanography 46 (2016): 1717-1734 doi:10.1175/JPO-D-15-0124.1 Geographic location/entity North Atlantic Ocean Circulation/ Dynamics Anticyclones Boundary currents Convection Eddies Fluxes Article 2016 ftwhoas https://doi.org/10.1175/JPO-D-15-0124.1 2022-05-28T22:59:36Z Author Posting. © American Meteorological Society, 2016. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 46 (2016): 1717-1734, doi:10.1175/JPO-D-15-0124.1. The contribution of warm-core anticyclones shed by the Irminger Current off West Greenland, known as Irminger rings, to the restratification of the upper layers of the Labrador Sea is investigated in the 1/12° Family of Linked Atlantic Models Experiment (FLAME) model. The model output, covering the 1990–2004 period, shows strong similarities to observations of the Irminger Current as well as ring observations at a mooring located offshore of the eddy formation region in 2007–09. An analysis of fluxes in the model shows that while the majority of heat exchange with the interior indeed occurs at the site of the Irminger Current instability, the contribution of the coherent Irminger rings is modest (18%). Heat is provided to the convective region mainly through noncoherent anomalies and enhanced local mixing by the rings facilitating further exchange between the boundary and interior. The time variability of the eddy kinetic energy and the boundary to interior heat flux in the model are strongly correlated to the density gradient between the dense convective region and the more buoyant boundary current. In FLAME, the density variations of the boundary current are larger than those of the convective region, thereby largely controlling changes in lateral fluxes. Synchronous long-term trends in temperature in the boundary and the interior over the 15-yr simulation suggest that the heat flux relative to the temperature of the interior is largely steady on these time scales. The authors were supported in this work by the U.S. National Science Foundation. Article in Journal/Newspaper Greenland Labrador Sea North Atlantic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Greenland Journal of Physical Oceanography 46 6 1717 1734 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Geographic location/entity North Atlantic Ocean Circulation/ Dynamics Anticyclones Boundary currents Convection Eddies Fluxes |
spellingShingle |
Geographic location/entity North Atlantic Ocean Circulation/ Dynamics Anticyclones Boundary currents Convection Eddies Fluxes de Jong, Marieke F. Bower, Amy S. Furey, Heather H. Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
topic_facet |
Geographic location/entity North Atlantic Ocean Circulation/ Dynamics Anticyclones Boundary currents Convection Eddies Fluxes |
description |
Author Posting. © American Meteorological Society, 2016. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 46 (2016): 1717-1734, doi:10.1175/JPO-D-15-0124.1. The contribution of warm-core anticyclones shed by the Irminger Current off West Greenland, known as Irminger rings, to the restratification of the upper layers of the Labrador Sea is investigated in the 1/12° Family of Linked Atlantic Models Experiment (FLAME) model. The model output, covering the 1990–2004 period, shows strong similarities to observations of the Irminger Current as well as ring observations at a mooring located offshore of the eddy formation region in 2007–09. An analysis of fluxes in the model shows that while the majority of heat exchange with the interior indeed occurs at the site of the Irminger Current instability, the contribution of the coherent Irminger rings is modest (18%). Heat is provided to the convective region mainly through noncoherent anomalies and enhanced local mixing by the rings facilitating further exchange between the boundary and interior. The time variability of the eddy kinetic energy and the boundary to interior heat flux in the model are strongly correlated to the density gradient between the dense convective region and the more buoyant boundary current. In FLAME, the density variations of the boundary current are larger than those of the convective region, thereby largely controlling changes in lateral fluxes. Synchronous long-term trends in temperature in the boundary and the interior over the 15-yr simulation suggest that the heat flux relative to the temperature of the interior is largely steady on these time scales. The authors were supported in this work by the U.S. National Science Foundation. |
format |
Article in Journal/Newspaper |
author |
de Jong, Marieke F. Bower, Amy S. Furey, Heather H. |
author_facet |
de Jong, Marieke F. Bower, Amy S. Furey, Heather H. |
author_sort |
de Jong, Marieke F. |
title |
Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
title_short |
Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
title_full |
Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
title_fullStr |
Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
title_full_unstemmed |
Seasonal and interannual variations of Irminger ring formation and boundary–interior heat exchange in FLAME |
title_sort |
seasonal and interannual variations of irminger ring formation and boundary–interior heat exchange in flame |
publisher |
American Meteorological Society |
publishDate |
2016 |
url |
https://hdl.handle.net/1912/8059 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Labrador Sea North Atlantic |
genre_facet |
Greenland Labrador Sea North Atlantic |
op_source |
Journal of Physical Oceanography 46 (2016): 1717-1734 doi:10.1175/JPO-D-15-0124.1 |
op_relation |
https://doi.org/10.1175/JPO-D-15-0124.1 Journal of Physical Oceanography 46 (2016): 1717-1734 https://hdl.handle.net/1912/8059 doi:10.1175/JPO-D-15-0124.1 |
op_doi |
https://doi.org/10.1175/JPO-D-15-0124.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
46 |
container_issue |
6 |
container_start_page |
1717 |
op_container_end_page |
1734 |
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1766019987495976960 |