Recent changes in the Greenland–Scotland overflow-derived water transport inferred from hydrographic observations in the southern Irminger Sea.

International audience Recent decadal changes (1955–2007) in the baroclinic transport (TBC) of the Deep Western Boundary Current (DWBC) carrying the Greenland–Scotland overflow-derived waters along the East Greenland slope are quantified from a set of hydrographic sections in vicinity of Cape Farewe...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Sarafanov, Artem, Falina, Anastasia, Mercier, Herlé, Lherminier, Pascale, Sokov, Alexey
Other Authors: P.P. Shirshov Institute of Oceanology (SIO), Russian Academy of Sciences Moscow (RAS), Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00406698
https://doi.org/10.1029/2009GL038385