Yellowstone Lake, North America’s largest high-elevation lake, freezes over completely in late December or early January and usually thaws in late May or early June. The period of ice cover has not changed in the last century, despite warming temperatures in the region. Credit: Lusha Tronstad, the duration for which Yellowstone Lake remains ice-covered each year has remained constant over the past century, even amidst rising regional temperatures.
The lack of long-term change in the duration of Yellowstone Lake’s ice cover was unexpected because the Yellowstone region has seen a warming climate, the researchers say. Since 1950, annual temperatures have increased by 1.8 degreesthroughout the greater Yellowstone ecosystem. The changes are particularly pronounced at the high elevation of Yellowstone Lake, where air temperatures increased by about 2.5 degrees Fahrenheit between 1980-2018.
That differs from the Upper Green River Basin to the south, where snowfall has declined or been relatively stable at high elevations. “Our results, paired with recent analyses of climate projections, suggest a ‘tipping point’ may be coming when ice phenology abruptly changes for Yellowstone Lake,” they wrote. “This tipping point will largely stem from the ongoing shift from snow- to rain-dominated precipitation regimes in the fall and spring.
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