Little Ice Age (c. 1300–1900)
A centuries-long cooling of the Northern Hemisphere, strongest in the Arctic, that expanded glaciers worldwide. On Baffin Island, ice caps covered more than 11,000 square kilometers at the 1780–1880 peak — over a hundred times the area glaciated today.
Glaciers advanced and cold summers persisted for centuries across the North Atlantic region.
Cooling after about 1880 reversed as industrial greenhouse gas emissions rose, ending the Little Ice Age.
The Little Ice Age is the recent peak of the same late-Holocene cooling trend the study says was driving the Laurentide remnant's reexpansion into a new glacial period.
