The 1992-2009 transport variability of the East Greenland-Irminger Current at 60°N
Author:
Affiliation:
1. Laboratoire de Physique des Océans, UMR 6523, Ifremer, CNRS, IRD; Université de Bretagne Occidentale; Brest France
2. Laboratoire de Physique des Océans, UMR 6523, Ifremer, CNRS, IRD; Université de Bretagne Occidentale; Plouzané France
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1107/2011GL046863/2011GL046863.pdf
Reference13 articles.
1. Circulation and transport at the south east tip of Greenland;Daniault;J. Phys. Oceanogr.,2011
2. Boundary circulation at the exit of the Labrador Sea;Fischer;J. Phys. Oceanogr.,2004
3. Shifting surface currents in the northern North Atlantic Ocean;Hakkinen;J. Geophys. Res.,2009
4. Decline and partial rebound of the Labrador Current 1993-2004: Monitoring ocean currents from altimetric and conductivity-temperature-depth data;Han;J. Geophys. Res.,2010
5. Retroflection of part of the east Greenland Current at Cape Farewell;Holliday;Geophys. Res. Lett.,2007
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