Journal cover Journal topic
Ocean Science An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.289 IF 2.289
  • IF 5-year value: 2.756 IF 5-year 2.756
  • CiteScore value: 2.76 CiteScore 2.76
  • SNIP value: 1.050 SNIP 1.050
  • SJR value: 1.554 SJR 1.554
  • IPP value: 2.65 IPP 2.65
  • h5-index value: 30 h5-index 30
  • Scimago H index value: 41 Scimago H index 41
Volume 14, issue 5 | Copyright
Ocean Sci., 14, 1247-1264, 2018
https://doi.org/10.5194/os-14-1247-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 15 Oct 2018

Research article | 15 Oct 2018

Wind-driven transport of fresh shelf water into the upper 30 m of the Labrador Sea

Lena M. Schulze Chretien1 and Eleanor Frajka-Williams2 Lena M. Schulze Chretien and Eleanor Frajka-Williams
  • 1Marine Science Research Institute, Jacksonville University, FL, USA
  • 2University of Southampton, National Oceanography Center, Southampton, UK

Abstract. The Labrador Sea is one of a small number of deep convection sites in the North Atlantic that contribute to the meridional overturning circulation. Buoyancy is lost from surface waters during winter, allowing the formation of dense deep water. During the last few decades, mass loss from the Greenland ice sheet has accelerated, releasing freshwater into the high-latitude North Atlantic. This and the enhanced Arctic freshwater export in recent years have the potential to add buoyancy to surface waters, slowing or suppressing convection in the Labrador Sea. However, the impact of freshwater on convection is dependent on whether or not it can escape the shallow, topographically trapped boundary currents encircling the Labrador Sea. Previous studies have estimated the transport of freshwater into the central Labrador Sea by focusing on the role of eddies. Here, we use a Lagrangian approach by tracking particles in a global, eddy-permitting (1∕12°) ocean model to examine where and when freshwater in the surface 30m enters the Labrador Sea basin. We find that 60% of the total freshwater in the top 100m enters the basin in the top 30m along the eastern side. The year-to-year variability in freshwater transport from the shelves to the central Labrador Sea, as found by the model trajectories in the top 30m, is dominated by wind-driven Ekman transport rather than eddies transporting freshwater into the basin along the northeast.

Publications Copernicus
Download
Citation
Share