In the Arctic and Antarctica, PSCs appear anywhere between 15 and 25 kilometers (9.3 and 15.5 miles) in the sky during cold winter conditions. They’re most often invisible, but they can be sighted when the sun is angled just right. In these cases, they’re known as mother-of-pearl clouds, on account of their wild coloration: swirls of purple, teal, and yellow. Just like high clouds do elsewhere, they form an insulating layer over the poles, which prevents rapid temperature drops.
In the Eocene, the formation of these clouds was enhanced by the positions of the Earth’s continents and mountains. For instance, the Himalayas hadn’t fully formed yet, and the lack of miles-thick ice in Greenland meant lower land elevations. That led to the proliferation of waves of pressure in the atmosphere, which deflected more energy toward the tropics. Less energy reached the Arctic stratosphere, so it cooled, forming a blanket of PSCs. Things on land got … balmy.
Luckily, continental shift in the past 50 million years has changed the topography and atmospheric circulation in a way that thins this blanket. While PSCs still form and trap heat, they aren’t as abundant as they were before. But things can heat back up: If humanity continues to spew methane into the atmosphere, that could provide the stratospheric water vapor needed to form more of these invisible clouds. “I need to be very clear: The magnitude of PSCs won’t be as high as the Eocene,” says Dutta. “And that’s probably the good news for us.”
Better understanding clouds will be supremely important as the poles continue to rapidly transform. “The intensity of the feedbacks involving clouds remains those with the greatest uncertainties,” says atmospheric chemist Sophie Szopa, who has studied the Eocene climate at France’s Laboratory for the Sciences of the Climate and Environment, but wasn’t involved in the new paper. “It is therefore necessary to compare the results of different climate models, including polar stratospheric clouds, in order to understand the importance of this feedback on polar amplification for the coming century.”
Learning how the Eocene stratosphere influenced the climate will help scientists get a better handle on what to expect next. “Basically, these past climates provide us a testbed to check our models,” says Dutta. Polar scientists can then tease apart the potential warming from natural fluctuations in Earth’s climate versus the contribution of our civilization’s gas emissions.
Improved models can also help predict how the Arctic’s ecosystems will continue to transform. The region is greening, for instance, as higher temperatures allow plant species to spread north. That, in turn, changes how the landscape absorbs or reflects the sun’s energy: If more shrubs grow, they trap a layer of snow, preventing chilly wintertime air from penetrating the ground. That could accelerate the thawing of Arctic permafrost, releasing both carbon dioxide and methane—yet another climate-warming feedback loop.
Like the rest of the world this summer, the Arctic was extremely hot. At her research site, Myers-Smith recalls temperatures reaching 77 degrees Fahrenheit. “I hadn’t ever experienced that at the site,” she says. It’s yet more evidence that the region is undergoing monumental change, and that scientists need models that can precisely track it. “Even when you work in these systems, and think you have a pretty good understanding of how things go,” she says, “you can still get surprised.”
