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 cold stadial of the Dansgaard-Oeschger cycle. However. https://www.jmannino.com/special-deal-A-Magazine-Curated-By-Sacai-quick-pick/