Even extra gorgeous, it was solely within the mid-2010s that Antarctic sea ice was at report highs—a minimum of highs since satellite tv for pc observations started—having elevated barely however steadily within the years since 1979.

That current progress of Antarctic sea ice has been in stark distinction with that of the Arctic, a area that’s now warming up to four times faster than the remainder of the planet and has been steadily dropping ice for many years. That’s as a result of a phenomenon called Arctic amplification: Melting ice exposes darker ocean water or land, which absorbs extra of the solar’s power than white ice, which in flip results in extra warming. 

The Antarctic is a unique beast: It’s a frozen continent surrounded by open ocean, whereas the Arctic is an ocean of floating ice enclosed by land, like Russia, Alaska, and northern Canada. Antarctica’s ice is insulated, in a way, by robust, chilly ocean currents that swirl across the continent. Plus, Antarctica’s elevation is sort of excessive, offering extra cooling.

Antarctica’s sea ice—which types when seawater freezes—is distinct from the continent’s ice sheets and cabinets. An ice sheet rests on the land, and may be hundreds of toes thick. It turns into an ice shelf when it begins floating on coastal waters. While Antarctica’s ice sheets and cabinets have certainly been deteriorating as the planet warms, the continent’s sea ice is way more seasonal, waxing and waning dramatically between winter and summer season. 

Losing that sea ice received’t add to sea ranges, simply as melting ice cubes floating in a glass of water received’t trigger the glass to overflow. (The ice is already displacing the water.) But sea ice performs a important position in defending Antarctica’s colossal ice cabinets from deteriorating, and people may dramatically increase ocean ranges in the event that they break aside. If it totally melts, the Thwaites Glacier, aka the Doomsday Glacier, may add 10 toes to sea ranges. Sea ice protects Thwaites and different glaciers as a result of it acts like a buffer, absorbing the power of winds and waves that might in any other case erode them. It additionally cools the air passing over coastal waters, additional stopping the melting of ice cabinets.

This yr, the coast of West Antarctica has been significantly devoid of sea ice. “It’s the area where climate scientists are most concerned about potential massive contributions from the ice sheet to global sea level rise,” says Maksym. “This year, we see absolutely no sea ice at all in that area, which is, I think, pretty much the first time that has happened. Then there are some previous studies that showed that if you remove sea ice, you lose the sort of buttressing effects, and that can accelerate the breakup of the ice shelf.”

But that’s not the one world impact the lack of sea ice could have: When seawater freezes into ice, the denser brine that’s left over sinks to the seafloor, creating deep currents that rush away from Antarctica. The much less sea ice, the weaker these currents. “This will affect the efficiency with which the oceans will distribute energy, and ultimately affect the global climate,” says geographer Marilyn Raphael at UCLA, who research the area. “What happens in Antarctica doesn’t stay in Antarctica.”