But what about the polar vortex?

One reason the world grew more aware of the poles in 2014 is that infamous vortex. Add to that icy onslaught Buffalo’s November mega-blizzard and it all seems pretty dissonant with the climate records for the year—for instance, that the northern hemisphere’s 2014 snow cover came in well below average for the 10th year in a row, while hitting its lowest level in Eurasia since 1967.

Here’s what scientists think is happening: As snow cover and sea-ice melts, sunlight that it normally would have reflected is instead absorbed by the land and ocean. For instance, Greenland ice sheet’s albedo—the amount of sunlight it reflects—hit a record monthly low in Aug. 2014.

Warmer seas eat away at ice sheets. And to refreeze come winter, this extra heat must first be released into the air, warming the atmosphere even more—a cycle called “Arctic Amplification.”

Arctic Amplification may be weakening the jet stream—the eastward-blowing air currents that whip around the globe, which is now 14% slower than it was in the 1990s—allowing icy Arctic air to flow further and further south, according to a hypothesis put forth in 2012 (pdf).

Surface air temperatures over the Barents and Kara seas during winter, compared to the 1979-2013 average. Blue dots dots indicate unusually cold winters; red dots indicate unusually warm winters.
Surface air temperatures over the Barents and Kara seas during winter, compared to the 1979-2013 average. Blue dots dots indicate unusually cold winters; red dots indicate unusually warm winters.
Image: "Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades," Mori et al. 2014

This cycle could be the culprit behind the recent spate of cold snaps in Europe, Asia, and the US. The link isn’t conclusive—weather patterns are highly chaotic—and many scientists are still skeptical. However, a paper published in October (paywall) lends still more support to this theory.

Walruses, penguins and polar bears—oh my!

arctic global warming climate change rising temperatures ice In this aerial photo taken on Sept. 23, 2014 and released by NOAA, some 1500 walrus are gather on the northwest coast of Alaska. Pacific walrus looking for places to rest in the absence of sea ice are coming to shore in record numbers, according to NOAA. (AP Photo/NOAA, Corey Accardo This June 2014 released by the U.S. Fish and Wildlife Service shows Pacific walruses in the Chukchi Sea off the coast of Alaska. Researchers are trying to get a better handle on the size of the Pacific walrus population ahead of an expected decision by the U.S. Fish and Wildlife Service on whether the animals need special protections. (AP Photo/U.S. Fish and Wildlife Service
Ditching slushy seas for Alaska.
Image: AP Photo/U.S. Fish and Wildlife Service

This year, the plight of animals of the polar north and south attracted unusual attention. After snowy owls invaded the northern US, some 35,000 walruses thronged northwest Alaska, as shrinking sea ice drove them further south. That problem is also driving down polar bear numbers in western Hudson Bay—reversing a recent stabilization of their populations—making it more likely that they’ll start interbreeding with brown bears.

And on the opposite pole, Antarctica’s emperor penguins, which breed on sea ice, face falling populations too.

House-sized waves and Titanic-sinking icebergs

A scanned copy of the photographic print of the iceberg with which the RMS Titanic supposedly collided on April 14, 1912 at latitude 41-46N, longitude 50-14W. This print was in possession of Captain De Carteret, the Captain of the Minia, who reportedly stated that this was the only iceberg near the scene of the collision. The Minia was one of the first ships to reach the scene following the disaster.
A scanned copy of the photographic print of the iceberg with which the RMS Titanic supposedly collided on April 14, 1912 at latitude 41-46N, longitude 50-14W. This print was in possession of Captain De Carteret, the Captain of the Minia, who reportedly stated that this was the only iceberg near the scene of the collision. The Minia was one of the first ships to reach the scene following the disaster.
Image: US Coast Guard

Those effects are perhaps to be expected. But as 2014 revealed, there are a good many other effects of melting polar ice sheets that few are watching out for.

Waves, for one. Usually, the Arctic’s blanket of sea ice prevents the wind from whipping up much chop. However, the peel-back of Arctic ice means the creation of an entirely new swath of ocean—and of “house-sized waves,” according to Jim Thomson, a University of Washington physicist who reported the phenomenon (pdf). In related research, scientists researching historical iceberg data (pdf) found that Titanic-esque iceberg hazards have climbed since 1990, thanks to melting polar ice sheets.

These unexpected changes aren’t isolated to the sea, though. For instance, earlier this year, scientists in Siberia’s Yamal Peninsula found methane in concentration 50,000 times higher than the atmospheric average seeping from a crater that had been covered by a now-collapsed sheet of permafrost, as we recently highlighted.

Of course, this wasn’t the first year that alarming developments at the Earth’s ends seized the world’s attention. But thanks to several big scientific breakthroughs, 2014 will likely go down as the year that melting polar ice caps graduated from being a geographic abstraction to a symbol of the irreversible ways we’ve warped the planet.

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