Links: Please click on the links below to learn more about the Labrador current. Example Plots are below the Links.
- Labrador Sea surface circulation and the fate of the Irminger Sea Water
- Labrador Sea surface circulation and the fate of the Irminger Sea Water (Labrador Sea Circulations from drifters and hydrography)
- Labrador Sea surface circulation and the fate of the Irminger Sea Water (Labrador current velocity map)
- Mid-depth recirculation observed in the interior Labrador and Irminger seas by direct velocity measurements - Letters to Nature (Mid-depth circulation of Labrador current)
- Cold Ocean: Newfoundland and Labrador Heritage (Popular account of Labrador Current)
- How do the Labrador and Gulf Stream currents affect icebergs in the North Atlantic Ocean ? (Iceberg drift trajectories in the Labrador Current)
- Changes in Labrador Sea properties from 1998 to 1999 (Water properties) (Adobe PDF file)
- Newfoundland and Labrador Shelves: A subarctic shelf system (Biology)
- Mid-Depth Ventilation Along the Western Boundary of the Sub-Polar Gyre (Labrador Current study near the Flemish Cap)
- The Labrador Sea Convection Experiment LDOE
- Labrador Sea Water tracked by profling floats - from the boundary current into the open North Atlantic - by Jurgen Fischer, Friedrich Schott, (Abstract of profiling flots in the Deep Labrador Current)
- Glossary of Physical Oceanography Glossary: La-Lm
- Spatial and Temporal Variability of Ocean Temperature over the Labrador Shelf (Temperature over the Labrador Shelf) (Adobe PDF file)
- Atmospheres: Icebergs - by Kevin Chambers November 1, 2000, The Weather Channel. (Iceberg Alley)
- Currents and Transports in the Labrador Sea (Average velocity transect of Labrador Current at 53°N) (Adobe PDF file)
- Large Marine Ecosystems of the World LME #9: Newfoundland-Labrador Shelf
Example Plots: Clicking on a thumbnail image loads a larger image, clicking on the figure number downloads a PostScript image.
Figure 1. The Labrador current as represented by the Mariano Global Surface Velocity Analysis (MGSVA). The Labrador Current is the "southward" flowing component of the N. Atlantic subpolar gyre. It transports cold waters into the warmer Gulf Stream ring and meander region. Click here for example plots of seasonal averages. Figure 2. The average drifting buoy derived surface velocity. Click here for example plots of seasonal averages. Figure 3. Figure 4. Figure 5. Figure 6. Trajectories of buoys, ID 23508 (red) and 23534 (blue), exhibit the well-know counter-clockwise subpolar gyre circulation of the East Greenland Current, the West Greenland Current, and the Labrador Current. Buoy 23508 was in the Labrador Current twice; during the summer and fall of 1996 and in the fall and winter of 1998-99. It completed nearly one and three-quarters of a loop around the North Atlantic subpolar gyre (Also see the text of Irminger Current Figure 6.). Buoy 23534 was initially in the local recirculation in the north-east corner of the subpolar gyre before being advected by the East Greenland, West Greenland, and Labrador Currents. Figure 7. AVRRR image of the sea-surface temperature (SST). Figure 8. Geography of the region. Figure 9. Topography/Bathymetry of the region.