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

The warmest water reaching the east and west coast of Greenland is found between 200 m and 600 m. Whilst 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 floats, a range of sources within the World Ocean Database and unprecedented coverage from marine-mammal borne sensors have been analysed for the period 2002-2011. A significant seasonal range in temperature (~1-2 °C) is found in the warm layer, in contrast to most of the surrounding ocean. The phase of the seasonal cycle exhibits considerable spatial variability, with the warmest water found near the eastern and southwestern shelf-break towards the end of the calendar year. High-resolution ocean model trajectory analysis suggest the timing of the arrival of the year's warmest water is a function of advection time from the subduction site in the Irminger Basin.


Publication status:
Authors: Grist, Jeremy P. ORCIDORCID record for Jeremy P. Grist, Josey, Simon A. ORCIDORCID record for Simon A. Josey, Boehme, Lars, Meredith, Michael P. ORCIDORCID record for Michael P. Meredith, Laidre, Kristin L., Heide-Jorgensen, Mads Peter, Kovacs, Kit M., Lydersen, Christian, Davidson, Fraser J.M., Stenson, Garry B., Hammill, Mike O., Marsh, Robert, Coward, Andrew C. ORCIDORCID record for Andrew C. Coward

On this site: Michael Meredith
16 December, 2014
Geophysical Research Letters / 41
Link to published article: