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A. Kuijpers

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Open access Sep 2026

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...

A. Kuijpers, M. Seidenkrantz · 0 citations

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