A mechanism for reconciling the synchronisation of Heinrich events and Dansgaard-Oeschger cycles
Abstract The evolution of the northern hemispheric climate during the last glacial period was beset by quasi-episodic iceberg discharge events from the Laurentide ice sheet, known as Heinrich events (HEs).The paleo record places most HEs into the Wide Fireplace Insert cold stadial of the Dansgaard-Oeschger cycle.However, not every Dansgaard-Oeschge