Abstract:

Post-glacial uplift and convection in the underlying mantle uplift in the Hudson Bay area (as reflected in changes of the area's gravity and magnetic intensity) are making significant contribution to the Davis Straits rate of flow, affecting composition of the Labrador current and further the Subpolar gyre's circulation, which is the engine of the heat transport across the North Atlantic Ocean and very relevant to the Atlantic basin climate.
Full article (pdf):  NORTH ATLANTIC TEMPERATURE ANOMALY

extract:

© m.a. vukcevic