Nov 3, 7:01 AM

How Humanity Canceled the Next Ice Age

Geochemical evidence from northern Canada reveals that global warming halted a 2,000-year planetary cooling trend in the 1960s.

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How Humanity Canceled the Next Ice Age

For decades, popular anxieties about global climate shifted between apocalyptic visions of a world frozen solid and one boiled alive. As it turns out, Earth was indeed quietly preparing its next long chill—until human industrial activity abruptly canceled the program.

On Baffin Island in northeastern Canada sits the Barnes Ice Cap, a 6,000-square-kilometer remnant of the ancient Laurentide Ice Sheet that once buried vast stretches of Canada and the northern United States. Geochemists at the Lamont-Doherty Earth Observatory of the Columbia Climate School, including Young and Joerg Schaefer, set out to determine whether this massive ice sheet had previously shrunk and re-expanded. By measuring carbon-14 isotopes in dead vegetation preserved along the glacier’s retreating margins, the researchers mapped the ice front's precise movement over millennia.

The data revealed a striking trajectory. The Laurentide Ice Sheet reached its smallest extent roughly 3,000 years ago before reversing course around 2,000 years ago. Temperatures dropped sufficiently for fresh ice to accumulate, initiating what researchers regard as the early structural phase of Earth's next cold period. The controversial claims made by some scientists in the 1970s regarding an imminent ice age were, from a geological perspective, surprisingly accurate.

That natural progression came to a sudden halt in 1961. Marked by an extraordinary summer heatwave comparable to the record temperatures of 2021, the early 1960s represented a sharp turning point. Canadian northern regions began warming roughly three times faster than the global average, with national summer temperatures rising about 2.1 degrees Celsius above baseline levels. The Barnes Ice Cap began losing more volume in the summer heat than winter snowfall could replenish.

Humanity effectively derailed a multi-millennial cooling trend in the span of a single generation. While the disappearance of ice affects smaller mountain glaciers—including those dwindling remnants in Germany—the complete loss of the Barnes Ice Cap carries systemic consequences. This massive ice body previously acted as a cooling engine, generating feedback loops that facilitated broader glaciation. Over the coming centuries, as this final fragment melts away entirely, the Earth will lose the primary physical catalyst that historically triggered future ice ages.

Written by Sandy van Dongen sandy.vandongen@alpineweekly.com