Summary
The growth, drift and decay of the sea ice margins are closely related to the dynamics of the subpolar oceanic regions. This is especially true in the Greenland and Labrador Seas where warm northward currents (Norwegian and Irminger currents) encounter rapidly cooling atmospheric conditions and southward advancing sea ice and cold currents (East Greenland and Labrador currents). Location of the ice margin is partly due to the large oceanic heat flux from the deeper ocean which occurs primarily in winter when deep convection brings up warm water from below and prevents ice formation in early winter. After an historical data set analysis of Greenland and Labrador Seas hydrological characteristics, we are presenting some recent results about oceanic deep convection events and mesoscale dynamics close by an Ice edge which emphasized the role of the ocean in air — sea — ice interactions.
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Publications
GASCARD J.C (1981).- North Atlantic Subpolar circulation and Deep Water Formation in Labrador and Greenland seas. C.E.C. Contact Group. Contact Group “Climate Models”. Extended Abstracts of Presentations at the first meeting, Brussels, 26–27th May 1982.
HOUSSAIS M.N. and J.C. GASCARD (1982).- Quelques é1éments sur la validation des données appliquée à la mer du Groenland et à la mer du Labrador. C.E.C. Contact Group. Contact Group “Climate Models”. Abstracts of Presentations at the second meeting. Brussels, 11th May 1982.
GASCARD J.C. (1982).- Deep Convection in the Ocean and the general circulation. Summer School of Space Physics, Space Oceanography, Grasse (France), 1–28th July 1982.
CLARKE R.A. and J.C. GASCAR (1983).- The formation of Labrador sea Water. Part I: Large Scale Processes. J. Phys. Oceanogr., 13, 1764–1778.
GASCARD J.C. and R.A. CLARKE (1983).- The Formation of Labrador sea Water. Part II: Mesoscale and Smaller scale Processes. J. Phys. Oceanogr., 13, 1779–1797.
HOUSSAIS M.N. (1983).- Premiers résultats du traitement statistique des fichiers de données historiques de la mer de Norvège et de la mer du Labrador. (unpublished manuscript).
Communication
GASCARD J.C. (1981).- North Atlantic subpolar circulation and Deep Water formation in Labrador and Greenland seas. C.E.C. Contact Group. Contact Group “Climate Models”, Brussels 26–27th May 1981.
GASCARD J.C. (1981).- Open Ocean deep convection. NATO Advanced Research Institute on “Large Scale Transport of Heat and Matter in the Ocean”. Bonas (France) 22–30th September 1981.
HOUSSAIS M.N. and J.C. GASCARD (1982). Quelques éléments sur la validation des données appliquée à la mer du Groenland et à la mer du Labrador. C.E.C./Contact Group “Climate Models”, Brussels, 11th May 1982.
GASCARD J.C. (1982).- Deep Convection in the Labrador Sea. SCOR Working Group 58 on “Arctic Ocean Modelling Meeting”. Cambridge (G.B.) 2l–25th June 1982.
GASCARD J.C. (1982).- Deep Convection in the Ocean and the general circulation. Summer School of Space Physics: Space Oceanography, Grasse (France), 1–28th July 1982.
GASCARD J-C, (1983).- Labrador sea Water Formation. I.U.G.G. XVIII General Assembly, Hamburg, 15–27th August 1983.
GASCARD J.C. (1983).- Preliminary Results on the French MIZEX 83 Test Experiment, Lagrangian description of currents in the MIZ. MIZEX Science Group Meeting, Bremerhaven (RFA), 19–21th November 1983.
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© 1986 ECSC, EEC, EAEC, Brussels and Luxembourg
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Gascard, J.C. (1986). Subpolar Circulation, Deep Water Formation and Air — Sea — Ice Interactions in Labrador and Greenland Seas. In: Ghazi, A., Fantechi, R. (eds) Current Issues in Climate Research. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5494-6_19
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DOI: https://doi.org/10.1007/978-94-009-5494-6_19
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