Using satellite imagery from 2010 to 2017 and 2018 to 2021, a team studied how elevations and landscapes changed on the peninsula and found evidence of what they call “thaw slumps” — landslides that occur as ice slowly melts, leading to horseshoe-shaped collapses in the hillside.

Between 2010 and 2017, researchers noted 82 slumps. But between 2018 and 2021, that number climbed to 1,404 slumps, with a 43-fold increase in the volume of affected material.

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As they thawed and collapsed, the hillsides released carbon once trapped beneath the ice. Researchers estimate that carbon release increased 28-fold in the study period; much of that was linked to 2020, when the region recorded temperatures that were much warmer than average.

The climate models used to quantify and predict climate change don’t account for that carbon release.

That should change, the researchers write. They contend the hillsides are a “major but largely neglected component of the Arctic carbon cycle.”

It’s unclear what happens to that carbon and how it contributes to global warming and climate change. Scientists say it will take more research, including remote sensing via satellite, to understand more about the sliding hillsides and their long-term consequences for both the Arctic landscape and the planet.