In today’s warming climate, the persistent North Atlantic cooling anomaly off the southeast coast of Greenland is thought to be caused by the accelerating input of meltwater from the Greenland Ice Sheet (GrIS) and considered an indicator of a big change, as in a major weakening of the Atlantic Meridional Overturning Circulation (AMOC). New research shows, Greenland ice mass loss during the Younger Dryas driven by Atlantic Meridional Overturning Circulation feedbacks… Read complete article.
Greenland ice mass loss driven by Atlantic Meridional Overturning Circulation feedbacks
Attribution: Samrat Bharadwaj