The widely accepted" Milankovitch theory" explains insolation-induced waxing and waning
of the ice sheets and their effect on the global climate on orbital timescales. In the past half …

More than a decade ago, ice core records from Greenland revealed that the last glacial
period was characterized by abrupt climate changes that recurred on millennial time scales …

Climate projections suggest a weakening or collapse of the Atlantic Meridional Overturning
Circulation (AMOC) under global warming, with evidence that a slowdown is already …

During the last glacial period, the North Atlantic regionexperienced pronounced, millennial-
scale alternations between cold, stadial conditions and milder interstadial conditions …

Between~ 17,500 and 15,000 years ago, the Atlantic meridional overturning circulation
weakened substantially in response to meltwater discharges from disintegrating Northern …

Intermediate glacial states were characterized by large temperature changes in Greenland
and the North Atlantic, referred to as Dansgaard–Oeschger (D–O) variability, with some …

Abstract The Dansgaard‐Oeschger oscillations and Heinrich events described in North
Atlantic sediments and Greenland ice are expressed in the climate of the tropics, for …

Our understanding of climate dynamics during millennial-scale events is incomplete,
partially due to the lack of their precise phase analyses under various boundary conditions …

Deep water formation in the North Atlantic and Southern Ocean is widely thought to
influence deglacial CO2 rise and climate change; here we suggest that deep water …

Most studies of African dust and North Atlantic climate have been limited to the short time
period since the satellite era (1980 onward), precluding the examination of their relationship …