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See Greenland Current.
West Greenland Current, cool flow of water proceeding northward along the west coast of Greenland.
Along the east coast of Greenland is the southward-flowing cold East Greenland Current.
Other bergs pass through Fram Strait and into the East Greenland Current.
The Norwegian Gyral separates the Norway Current from a southeastward-flowing branch of the East Greenland Current.
The dashed arrows indicate the cold polar south-flowing waters such as the East Greenland Current, West Greenland Current and Labrador Current, which constitute the western branch of the subpolar gyre (SPG).
Similar(34)
One proceeds northward and then eastward around Iceland, and the other flows westward and then southwestward, merging with the East Greenland and, eventually, the West Greenland currents.
Interpretation of this trend is made difficult by AMO variability visible in Figure 2. In situ measurements during the Labrador Sea convection [e.g., Lilly et al., 1999] show large "spice" variation as atmospheric cooling penetrates the buoyancy barrier, originating from the low-salinity West Greenland boundary current and reaching the more saline Irminger Current water.
Sutherland, D. A. & Pickart, R. S. The East Greenland Coastal Current: Structure, variability, and forcing.
Greenland's current net ice loss is equivalent to an annual 0.008 inch sea level rise.
Greenland's current economic situation is considered vulnerable, with few sources of income and an increasing gap between expenditure and revenue.
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