Excessive Southwest Greenland Ice Sheet Melting Between 4.4 and 3.2 ka BP Documented by Fjord Sediments: Implications for N-Atlantic Ocean Circulation and AMOC
Greenland Ice Sheet (GrIS) melting occurred during the later part of the Holocene Thermal Maximum (HTM) with a well-documented significant GrIS retreat between 7 and 3 ka. However, less is known about the immediate melt water impact on Greenland fjord hydrography and more distant ocean circulation. A compilation of pub...