Iceberg calving accounts for half of the mass discharge from the Greenland and Antarctic ice
sheets, which has increased dramatically over the last two decades. Through their …

Three long cores from Flemish Cap and Orphan Knoll, offshore southeastern Canada,
contain discrete units of detrital carbonates that are coeval with Hudson Strait Heinrich (HS …

Abstract In the North Atlantic, relatively coarse grained sediments can be found periodically
throughout sediment cores spanning the Last Glacial Period. These sediments were rafted …

While there are no ice sheets in the Northern Hemisphere outside of Greenland today, it is
uncertain whether this was also the case during most other Quaternary interglacials. We …

Recent high-resolution sediment records, such as Greenland ice cores and Chinese
stalagmites, have greatly enhanced our understanding of millennial-scale climate variability …

During Heinrich events, great armadas of icebergs episodically flooded the North Atlantic
Ocean and weakened overturning circulation. The ice discharges of these episodes …

Icebergs modulate the effective location of freshwater input from ice sheets into the ocean
and therefore play an important role for the climate, especially during times of increased ice …

Iceberg calving is currently responsible for half of the mass loss from Greenland's marine-
terminating glaciers and could increase well into the 21st century. While dynamically …

It is a scientifically accepted fact that the Earth's climate is presently undergoing significant
changes with the potential for immense negative impacts on human society. As evidence of …

Abstract The Atlantic Meridional Overturning Circulation (AMOC) is thought to exert
considerable influence over the climate via heat redistribution and carbon storage. Its …