As it does in the Arctic, the surface of the ocean around Antarctica freezes over in the winter and melts back each summer. Antarctic sea ice usually reaches its annual maximum extent in mid- to late September, and reaches its annual minimum in late February or early March.
In 2022, Antarctic sea ice reached its annual peak on September 16. The 2022 winter maximum extent was 18.19 million square kilometers (7.02 million square miles). In 2023, Antarctic sea ice reached its annual minimum on February 21. At 1.79 million square kilometers (691,000 square miles), it was the lowest extent on record. This low value punctuated a series of below-average extents, including multiple record lows. Whether this was due to natural variability or the start of a climate-change signal was not clear as of February 2023. Making such a determination could require several more years.
The timing of the seasonal cycles isn’t the only way that Antarctic sea ice differs from the Arctic. One key difference is the larger range between austral winter maximum extent and summer minimum extent. Historically, Antarctic sea ice has extended to about 19 million square kilometers (7 million square miles) in winter and retreated to about 3 million square kilometers (1 million square miles) in summer. That’s a bigger winter-summer difference than in the Arctic, where the range is about 15 million square kilometers (6 million square miles) in winter and 6 million square kilometers (2 million square miles) in summer.
The differences in seasonal extremes are largely due to basic geography. The Arctic is an ocean basin largely surrounded by land. Sea ice is always present over the North Pole and central Arctic, and it expands southward every autumn, but its expansion is checked by Eurasia, North America, and Greenland. The Antarctic is a continent surrounded by a vast ocean. Sea ice can expand freely across the Southern Ocean in winter, but it can get no closer to the South Pole than the Antarctic coastline will allow. This barrier means that sea ice can't form over the very coldest parts of the Southern Hemisphere.
Because a substantial amount of Antarctic sea ice forms at lower, warmer latitudes, less ice survives the summer. On average, about 40 percent of the Arctic Ocean’s winter ice cover remains at the summer minimum, whereas in the Southern Ocean only about 15 percent does. Because so little Antarctic ice persists through the summer, the majority of Antarctica’s sea ice is only one winter old. As a result, Antarctic sea ice is relatively thin, often 1 meter (about 3 feet) or less. (In the Arctic, multiyear ice that survives at least one summer is generally 3–4 meters (10–12 feet) thick, and even seasonal ice that formed since the previous summer can often reach about 2 meters (roughly 6 feet) in thickness.)
So overall, average Antarctic ice thickness is much lower than Arctic sea ice. However, snowfall often thickens Antarctic sea ice. The heavy snow burden can depress ice floes, and seawater can subsequently flood the snow layer. This saturated snow can freeze, forming “snow ice,” an important component of southern sea ice. Although this can occur in the Arctic as well, it is less common.
Variability and long-term change
Sea ice waxes and wanes with the seasons, and minimum and maximum summer and winter extents vary. Compared to the Arctic, Antarctic sea ice shows lower variability in summer, and higher variability in winter. These changes largely result from the geographic differences mentioned above, namely Antarctic sea ice’s distance from the pole (sea ice can melt back only as far as the coast in summer, making for less year-to-year variability) and unconstrained growth potential in winter. Weather events often drive variability, but have different effects in the Northern and Southern Hemispheres. Weather exerts a greater influence on the Arctic minimum, and the Antarctic maximum.
The sea ice satellite record dates back to October 25, 1978. Unlike the Arctic, where sea ice extent is declining in all areas in all seasons, Antarctic trends are less apparent. From 1979–2017, Antarctic-wide sea ice extent showed a slightly positive trend overall, although some regions experienced declines. Those exceptions have primarily occurred around the Antarctic Peninsula. The region south and west of the Antarctic Peninsula has shown a persistent decline, but this downward trend is small compared to the high variability of Antarctic sea ice overall. Another region near the northern tip of the Peninsula, in the Weddell Sea, showed strong sea ice declines until 2006, but the ice in that region rebounded in the 2010s; most recently it has declined slightly again. The eastern Ross Sea region has shown a modest increase in ice extent over the same period.
Overall, the long-term trend in Antarctic sea ice is nearly flat. (in contrast, the glaciers and ice sheets over land in Antarctica are losing mass.) The satellite record spans more than four decades, and although the ice has shown increasing and decreasing trends over portions of that record, few of those trends have been statistically significant. Year-to-year variability has dominated, especially over the last decade. Since the year 2013, Antarctic sea ice has exhibited its highest and lowest extents in the entire record—the highest-ever winter maximum occurred in September 2014, and the lowest-ever summer minimum was in February 2023. But the overall trend, as of early 2023, is close to zero.
According to the National Snow and Ice Data Center’s Sea Ice Index, from the start of the satellite record in November 1978 through February 2023, Antarctic sea ice showed a slightly positive long-term trend in most months, with the exceptions of January, February, November, and December, which showed slightly negative trends. None of the trends are statistically significant.
A study published in 2022 reconstructed Antarctic sea ice back to 1905 using a combination of several climate models. The study found that, prior to the continuous satellite record, Antarctic sea ice experienced declining trends over much of the early and mid-twentieth century.
Impacts of change
Land-sea configurations affect sea ice extents not only by limiting where ice can form, but also by introducing their own effects. In the Arctic, landmasses surround and influence the sea ice in the Arctic Ocean. Ice and (especially) snow are highly reflective, bouncing much of the Sun’s energy back into space. As Northern Hemisphere spring and summer snow cover declines, the underlying land surface absorbs more energy and warms. Warmer conditions on land affect the nearby ocean, and more sea ice melts as a result. As sea ice melts, more of the ocean warms. The melt-warmth-melt feedback cycle means that the Arctic is warming faster than the rest of the globe.
No such polar amplification effect has occurred on a large scale in the Southern Hemisphere, however. Antarctica is surrounded by ocean, not a land surface that is losing its reflective snow and ice cover in the spring and summer. It was already normal, historically, for summertime sea ice to melt back nearly to the Antarctic coastline, leaving large expanses of the Southern Ocean exposed to heating from the summer sun. By contrast, the loss of reflective snow and ice in high northern latitudes surrounding the Arctic Basin represents a profound change from what was historically normal.
The Southern Ocean is vast, a fact often underplayed in map projections focused on the Northern Hemisphere. Natural cycles in the Southern Ocean can have pronounced effects on Antarctic sea ice. Atmospheric patterns, partly influenced by greenhouse gas emissions, are also at work.
The Southern Annular Mode (SAM) is a pattern of westerly winds circling Antarctica. The SAM is influenced by El Niño-Southern Oscillation (ENSO) conditions, so it is partly driven by natural oscillations. At the same time, research has found that human-caused global warming tips the SAM into its positive mode more frequently, and the resulting wind effects generally tend to increase Antarctic sea ice extent. The SAM also affects the Amundsen Sea Low, which in turn affects sea ice transport and weather conditions over a broad area from the western Antarctic Peninsula to the eastern Ross Sea.
Several consecutive years of below-average Antarctic sea ice extent, however, have captured growing attention from researchers. At the time of the record-low extent observed in February 2023, Ted Scambos, senior research scientist at the University of Colorado, Boulder, said, “If lower-than-average Antarctic sea ice extent continues, despite a shift in ENSO or with a range of SAM index values, it would be a strong indication that we're seeing a climate signal emerging from the high variability of the Antarctic system.”
Long story short: Climate change has a discernible influence on Arctic sea ice, but it has a complicated, messy influence on Antarctic sea ice. (Meanwhile, the Antarctic Ice Sheet is losing mass.)
Where sea ice does melt away completely in the Antarctic summer, the ice’s absence can have cascading effects. For example, sea ice retreat in the Weddell Sea along the northern tip of the Antarctic Peninsula probably contributed to Larsen Ice Shelf losses. Ice shelves—thick slabs of floating ice attached to coastlines and usually fed by glaciers—fringe the frozen continent. Intact sea ice in front of an ice shelf buffers the shelf from ocean swells. When the ice is gone, ocean waves can flex the shelf and make it more vulnerable to disintegration. Depending on how much an ice shelf disintegrates, the glacier feeding it may accelerate into the ocean. Another potential impact of reduced sea ice cover is greater accumulation on the continent, as winds from the open ocean reach the ice sheet without first flowing over an extensive sea ice fringe. This possibility, if it occurs, would tend to reduce the impact of sea level rise from the ice sheet.
Antarctica is colder than the Arctic, but it’s still losing ice. (2019, March 12). Climate.gov.
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