Antarctic sea ice recently reached its lowest concentration on record - falling below 2 million square kilometers (772,000 square miles) for the first time in 43 years of satellite observations.
"It's the first time on satellite record that we've had sea ice extent fall below 2 million square kilometers. It's a record and by quite a bit," said Ryan Fogt, a climate scientist and professor at Ohio University.
Sea ice builds and melts with the seasons. In Antarctica, sea ice typically reaches its maximum coverage at the end of the austral winter in mid- to late- September and melts to its minimum extent in February.
The 2021-2022 melt-and-freeze cycle has been a bit unusual, however. Antarctic sea ice reached its maximum extent on Sept. 1, 2021, almost a month earlier than normal peak. The sea ice maximum extent, measuring 18.75 million square kilometers (7.24 million square miles), was also well above average. But it didn't last long.
Sea ice retreated rapidly through austral spring and summer. In January and February, ice cleared out from the Ross, Amundsen and northwestern Weddell Sea regions. According to the National Snow and Ice Data Center (NSIDC), Antarctic sea ice reached its minimum extent of 1.92 million square kilometers on February 25. The previous low occurred in 2017 when sea ice extent reached 2.11 million square kilometers (815,000 square miles).
"It's a record low, but we see a lot of year-to-year variability. One year is a little bit higher, one year is a little bit lower," said Walt Meier, a research scientist at NSIDC. "There's really no trend."
Meier said the yearly fluctuations can be partly explained by geography. "The Antarctic is open to the ocean so it's very susceptible to changes and circulation changes in the ocean currents . . . The ice is thin, it moves around with the wind currents, it's very variable. Even subtle changes can make a pretty big difference," said Meier, based at the University of Colorado Boulder.
This year's low concentration was likely in part to a long, strong low-pressure system that formed in late 2021 near the inner peninsula area, which created winds and warm air that helped to quickly erode ice in those areas. For instance, strong winds pushed ice from the Ross Sea into warmer waters farther north. At the same time, some areas experienced slightly higher concentrations of ice, such as in the Pine Island Bay.