Researchers led by Nicolás Young, a geologist at Columbia University's Lamont-Doherty Earth Observatory, have analyzed the Barnes Ice Cap on Baffin Island, the remnant of the Laurentide Ice Sheet that once buried most of Canada under two miles of ice and locked away about 80 meters of sea level.
The study shows that the Laurentide Ice Sheet reached its smallest size about 3,600 years ago, then began re-expanding roughly 2,000 years ago. The team interprets this as the opening move of the next glaciation. The natural ice growth continued until around 1960, when human-caused climate warming reversed the trend.
Barnes Ice Cap sits on the central plateau of Baffin Island in the Canadian Arctic. “Barnes is the last remaining piece of one of the domes of the Laurentide Ice Sheet,” Young said. As that enormous dome thinned through the Holocene, its margin withdrew onto Baffin Island. What remains today is the deflated core of what was once two miles thick.
The reason the ice cap can testify about its own history, Young explained, comes down to the temperature at its base. The ice preserved a record of its own expansion and contraction over millennia, allowing scientists to read the story of a natural ice age cycle that was already underway when modern warming intervened.
