Glaciers are fighting back against climate change by cooling the air that touches their surfaces. But for how long? The Pellicciotti group at the Institute of Science and Technology Austria (ISTA) has compiled and re-analyzed an unprecedented dataset of on-glacier observations worldwide. Their findings, published today in Nature Climate Change, demonstrate that glaciers will likely reach the peak of their self-cooling power by the next decade before their near-surface temperatures spike up and melting accelerates.
Thomas Shaw keeps a vivid memory of this special summer day in August 2022. The postdoctoral researcher in Francesca Pellicciotti’s group at the Institute of Science and Technology Austria (ISTA) was in the Swiss Alps, with a blue sky and a pleasant temperature of 17 degrees Celsius. Except that he was on top of the Glacier de Corbassière, at an altitude of 2,600 meters, collecting data about the glacier’s health.
Are glaciers taking it too cool? While ambient temperatures have been increasing steadily worldwide, the near-surface temperatures of glaciers seem to be lagging behind. The massive Himalayan glaciers are even blowing cold winds down their slopes in an attempt to cool themselves and preserve their ecosystems. Yet, this strange effect is far from being an indicator of the glaciers’ long-term stability.
A new study led by Shaw demonstrates that this reaction of glaciers is likely to reach its peak in the 2030s. “The more the climate warms, the more it will trigger the glaciers to cool their own microclimate and local environments down-valley,” says Shaw. “But this effect will not last long, and a trend shift will ensue before the middle of the century.” From then on, the glaciers’ melting and fragmentation due to human-caused climate change will intensify, and their near-surface temperatures will rise more rapidly, hastening their decline.
Large glaciers and cold winds
It takes a tremendous effort to understand local climate effects in some of the world’s remotest areas and map their evolution on a global scale. Often, on-site data is simply lacking. This poses a challenge to the precision of computational models which simulate the climate’s detailed evolution. When Pellicciotti and her collaborators first saw the data collected at a 5000-meter-high climate station on the slopes of Mount Everest, they could hardly believe their eyes. “Upon examining the data thoroughly, we understood that the glaciers were reacting to the warming air in summer by intensifying their temperature exchange at the surface,” Pellicciotti says. Due to the sheer size of the Himalayan glaciers, this results in the cooling of large air masses in direct contact with the glacier surfaces. “These large, dense cold air masses then flow down the slopes with the effect of gravity in a phenomenon called ‘katabatic winds.’” Other large glaciers around the world behave similarly.
Scientists going out of their way
Now, Shaw sought to develop a robust global model that overcomes the limitations of data scarcity. He developed a new method to estimate how long glaciers would continue to absorb the climate shock worldwide. “We compiled data from past and recent projects across our research group, pooled them with all published data, and reached out to other researchers to request that they share with us their unpublished data,” says Shaw. “Using this unprecedented dataset, we reassessed the physical processes to find generalizable aspects and developed a statistical framework that can give us a glimpse into the evolution of glacier cooling worldwide.”
Peak cooling
Shaw and the team compiled an inventory of hourly data from 350 weather stations located on 62 glaciers worldwide, representing a total of 169 summer-long measurement campaigns. They specifically examined the ratio of near-surface temperature to ambient, non-glacier temperature right above each station and analyzed it over space and time. “We call the difference in temperature ‘decoupling,’ because it seems at odds with the warming of ambient temperatures,” says Shaw. They showed that, on average, the near-surface temperature on mountain glaciers worldwide warmed 0.83 degrees Celsius for every degree rise in ambient temperature.
They also investigated the glacier properties most likely to limit the decoupling effect, such as the presence of a debris mantle on the lower part of a glacier, and refined their model with this information. By modeling future projections, they demonstrated that this cooling effect will peak between the 2020s and 2040s, before the glaciers’ steady mass loss leads to their large-scale retreat, reversing the cooling trend. “By then, the worn-out and considerably degraded glaciers will ‘recouple’ to the steadily warming atmosphere, sealing their fate,” says Shaw.
Accepting the loss and coordinating future actions
While the projection paints a bleak future for the world’s majestic water towers, there are pragmatic consequences if the current trend continues. “Knowing that the glaciers’ self-cooling will continue a little longer could buy us some extra time to optimize our water management plans over the next decades,” says Shaw.
However, the team is fully aware that they can neither salvage nor recover the world’s mountain glaciers. “We must accept the committed ice loss and put our full efforts into limiting further climatic warming rather than into ineffective geo-engineering strategies such as seeding clouds and covering glaciers. These are like putting an expensive Band-Aid on a bullet wound. The coming decades are a time for reflection, effective water management, and action to change public consciousness about human-caused climate change.” The researchers further underline the need for coordinated global climate policies to drastically reduce emissions and safeguard human life on Earth from the unforeseeable effects of global warming. “Every bit of a degree counts,” says Shaw, echoing the words that scientists have been stressing for decades.
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