On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea

In this study, an idealized eddy-resolving model is employed to examine the interplay between the downwelling, ocean convection and mesoscale eddies in the Labrador Sea and the spreading of dense water masses. The model output demonstrates a good agreement with observations with regard to the eddy f...

Full description

Bibliographic Details
Published in:Ocean Modelling
Main Authors: Georgiou, Sotiria, van der Boog, Carine G., Brüggemann, Nils, Ypma, Stefanie L., Pietrzak, Julie D., Katsman, Caroline A.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2019
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/46133/
https://oceanrep.geomar.de/id/eprint/46133/1/Geogiou.pdf
https://doi.org/10.1016/j.ocemod.2019.02.004
_version_ 1821529421076496384
author Georgiou, Sotiria
van der Boog, Carine G.
Brüggemann, Nils
Ypma, Stefanie L.
Pietrzak, Julie D.
Katsman, Caroline A.
author_facet Georgiou, Sotiria
van der Boog, Carine G.
Brüggemann, Nils
Ypma, Stefanie L.
Pietrzak, Julie D.
Katsman, Caroline A.
author_sort Georgiou, Sotiria
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
container_start_page 56
container_title Ocean Modelling
container_volume 135
description In this study, an idealized eddy-resolving model is employed to examine the interplay between the downwelling, ocean convection and mesoscale eddies in the Labrador Sea and the spreading of dense water masses. The model output demonstrates a good agreement with observations with regard to the eddy field and convection characteristics. It also displays a basin mean net downwelling of 3.0 Sv. Our analysis confirms that the downwelling occurs near the west Greenland coast and that the eddies spawned from the boundary current play a major role in controlling the dynamics of the downwelling. The magnitude of the downwelling is positively correlated to the magnitude of the applied surface heat loss. However, we argue that this connection is indirect: the heat fluxes affect the convection properties as well as the eddy field, while the latter governs the Eulerian downwelling. With a passive tracer analysis we show that dense water is transported from the interior towards the boundary, predominantly towards the Labrador coast in shallow layers and towards the Greenland coast in deeper layers. The latter transport is steered by the presence of the eddy field. The outcome that the characteristics of the downwelling in a marginal sea like the Labrador Sea depend crucially on the properties of the eddy field emphasizes that it is essential to resolve the eddies to properly represent the downwelling and overturning in the North Atlantic Ocean, and its response to changing environmental conditions.
format Article in Journal/Newspaper
genre Greenland
Labrador Sea
North Atlantic
genre_facet Greenland
Labrador Sea
North Atlantic
geographic Greenland
geographic_facet Greenland
id ftoceanrep:oai:oceanrep.geomar.de:46133
institution Open Polar
language English
op_collection_id ftoceanrep
op_container_end_page 70
op_doi https://doi.org/10.1016/j.ocemod.2019.02.004
op_relation https://oceanrep.geomar.de/id/eprint/46133/1/Geogiou.pdf
Georgiou, S., van der Boog, C. G., Brüggemann, N., Ypma, S. L., Pietrzak, J. D. and Katsman, C. A. (2019) On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea. Ocean Modelling, 135 . pp. 56-70. DOI 10.1016/j.ocemod.2019.02.004 <https://doi.org/10.1016/j.ocemod.2019.02.004>.
doi:10.1016/j.ocemod.2019.02.004
op_rights info:eu-repo/semantics/restrictedAccess
publishDate 2019
publisher Elsevier
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:46133 2025-01-16T22:10:59+00:00 On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea Georgiou, Sotiria van der Boog, Carine G. Brüggemann, Nils Ypma, Stefanie L. Pietrzak, Julie D. Katsman, Caroline A. 2019 text https://oceanrep.geomar.de/id/eprint/46133/ https://oceanrep.geomar.de/id/eprint/46133/1/Geogiou.pdf https://doi.org/10.1016/j.ocemod.2019.02.004 en eng Elsevier https://oceanrep.geomar.de/id/eprint/46133/1/Geogiou.pdf Georgiou, S., van der Boog, C. G., Brüggemann, N., Ypma, S. L., Pietrzak, J. D. and Katsman, C. A. (2019) On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea. Ocean Modelling, 135 . pp. 56-70. DOI 10.1016/j.ocemod.2019.02.004 <https://doi.org/10.1016/j.ocemod.2019.02.004>. doi:10.1016/j.ocemod.2019.02.004 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2019 ftoceanrep https://doi.org/10.1016/j.ocemod.2019.02.004 2023-04-07T15:44:22Z In this study, an idealized eddy-resolving model is employed to examine the interplay between the downwelling, ocean convection and mesoscale eddies in the Labrador Sea and the spreading of dense water masses. The model output demonstrates a good agreement with observations with regard to the eddy field and convection characteristics. It also displays a basin mean net downwelling of 3.0 Sv. Our analysis confirms that the downwelling occurs near the west Greenland coast and that the eddies spawned from the boundary current play a major role in controlling the dynamics of the downwelling. The magnitude of the downwelling is positively correlated to the magnitude of the applied surface heat loss. However, we argue that this connection is indirect: the heat fluxes affect the convection properties as well as the eddy field, while the latter governs the Eulerian downwelling. With a passive tracer analysis we show that dense water is transported from the interior towards the boundary, predominantly towards the Labrador coast in shallow layers and towards the Greenland coast in deeper layers. The latter transport is steered by the presence of the eddy field. The outcome that the characteristics of the downwelling in a marginal sea like the Labrador Sea depend crucially on the properties of the eddy field emphasizes that it is essential to resolve the eddies to properly represent the downwelling and overturning in the North Atlantic Ocean, and its response to changing environmental conditions. Article in Journal/Newspaper Greenland Labrador Sea North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland Ocean Modelling 135 56 70
spellingShingle Georgiou, Sotiria
van der Boog, Carine G.
Brüggemann, Nils
Ypma, Stefanie L.
Pietrzak, Julie D.
Katsman, Caroline A.
On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title_full On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title_fullStr On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title_full_unstemmed On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title_short On the interplay between downwelling, deep convection and mesoscale eddies in the Labrador Sea
title_sort on the interplay between downwelling, deep convection and mesoscale eddies in the labrador sea
url https://oceanrep.geomar.de/id/eprint/46133/
https://oceanrep.geomar.de/id/eprint/46133/1/Geogiou.pdf
https://doi.org/10.1016/j.ocemod.2019.02.004