Seasonal variability of the warm Atlantic water layer in the vicinity of the Greenland shelf break

Abstract The warmest water reaching the east and west coast of Greenland is found between 200 and 600m. While important for melting Greenland’s outlet glaciers, limited winter observations of this layer prohibit determination of its seasonality. To address this, temperature data from Argo profiling...

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Bibliographic Details
Main Authors: Jeremy P. Grist, Simon A. Josey, Lars Boehme, Michael P. Meredith, Kristin L. Laidre, Garry B. Stenson, Mike O. Hammill, Robert Marsh, Andrew C. Coward
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.670.9525
http://eprints.soton.ac.uk/371748/1/grl52347.pdf