The last glacial termination was characterised by millennial-scale episodes of warming and
cooling that appear offset between the hemispheres. It has been proposed that this bi-polar …

Climatic fluctuations recorded in Antarctica and Greenland during the last deglaciation (18–
10 ka) differ markedly in their timing. It remains controversial whether local climate …

During each of the dramatic global warmings that ended the Pleistocene ice ages, the
Atlantic Meridional Overturning Circulation (AMOC) was disrupted. It is not clear whether this …

The last glacial period was punctuated by abrupt climate changes that are widely
considered to result from millennial-scale variability of the Atlantic meridional overturning …

The millennial-scale variability of the Atlantic Meridional Overturning Circulation (AMOC) is
well documented for the last glacial termination and beyond. Despite its importance for the …

The interhemispheric temperature response to a meltwater-induced weakening of the
Atlantic Meridional Overturning Circulation (AMOC) is characterized by a Northern …

Paleoclimate proxy data suggest that the Atlantic Meridional Overturning Circulation (AMOC)
was shallower at the Last Glacial Maximum (LGM) than its preindustrial (PI) depth. Previous …

Paleo proxy data and previous modeling studies both indicate that the massive discharge of
icebergs into the North Atlantic may have led to a (nearly) collapsed Atlantic meridional …

The Pacific meridional overturning circulation (PMOC) is not well known compared to the
Atlantic meridional overturning circulation (AMOC), due to its absence today. However …

During the last glacial period and deglaciation, climate shifts in the Northern and Southern
Hemispheres occurred asynchronously, cooling in one coinciding with warming in the …