Arctic melt versus Antarctic freeze: Is Antarctica warming or not?

Photograph of a large tabular iceberg and sea ice near Antarctica

During the short austral summer, much of the sea ice surrounding Antarctica melts, often leaving only the large, tabular icebergs. Credit: NSIDC courtesy Andi Pfaffling

September 2012 was a record-setting month for both of Earth’s poles, but for different reasons: sea ice in the Arctic fell to a record low minimum extent after a summer of melting, while Antarctic sea ice froze to a record high extent during the South Pole winter. Is record Antarctic sea ice canceling out the losses in Arctic ice? And does the record in the south mean that Antarctica is not warming?

Warming at the South Pole

Polar scientists say no on both counts. Ted Scambos, lead scientist at NSIDC, said, “These systems are not directly connected, and they certainly don’t offset each other. The climate and ocean processes that control summer Arctic ice extent are completely different from the ones that drive the Antarctic.” Data records indicate warming at both poles, but Antarctica’s geography is forcing warming to show in different ways than it does in the Arctic. “Antarctica’s trend is not nearly as large or as clear as the Arctic’s,” Scambos said.

Antarctica is a vast and largely ice-bound landmass, and the effects of warming are more complicated for scientists to sort out. The East Antarctic Ice Sheet has remained fairly stable, but air temperatures over the Antarctic Peninsula and the West Antarctic Ice Sheet are rising. Along the Peninsula, warmer air has increased surface melting, and several large ice shelves along the Peninsula have disintegrated dramatically after particularly warm summer periods.

Data image illustrating warming across Antarctica

Although Antarctica remains a cold place, this data image illustrates warming across the continent. Red represents areas where temperatures, measured in degrees Celsius per decade, have increased the most during the last 50 years, while dark blue represents areas with a lesser degree of warming. West Antarctica and the Antarctic Peninsula, the craggy finger of land jutting out from the continent, have experienced the most warming. Credit: NASA/GSFC Scientific Visualization Studio

In spite of warmer air, the climate of rest of the West Antarctic Ice Sheet remains colder than the Peninsula, so the rise in temperatures has not led to much summertime melting. There, the main culprit is warmer ocean currents. New ocean circulation patterns are bringing much warmer water to the ice edges along the coast. This is rapidly thinning the thickest glaciers at their base, and causing them to speed up. Consequently, glaciers in West Antarctica are also losing ice, in much larger amounts than glaciers along the Peninsula.

Wind, weather, and ozone

Yet warming is only part of the story. Changes in Antarctica’s winter sea ice are due more to changes in the winds that encircle the continent and, strangely enough, in the ozone layer above it. “The winds that blow around the continent have gotten stronger,” Scambos said. “And an added effect is the ozone hole, which also changes winds in the far south.” This seasonal hole forms over Antarctica each winter. Normally, ozone absorbs sunlight and warms the atmosphere. The current lack of ozone leaves a much colder air mass above Antarctica. While this may sound ideal for ice formation, it can sometimes have the opposite effect on sea ice. When warmer air from the north mixes with stubbornly cold air over Antarctica, the resulting turbulence generates stronger winds. During winter, stronger winds often blow the ice northward, away from the continent, creating a larger overall extent. These winds shifts are also behind the new patterns of ocean circulation that is warming glaciers at the edges of the West Antarctic Ice Sheet

For now, however, most of Antarctica remains a very cold place, and it has not yet reached the critical threshold beyond which melting further amplifies changes. “Both the Arctic and Antarctic systems are being driven in new directions by human-caused changes. At this point, the side effects for the Antarctic are outweighing the effect of warming,” Scambos said.

For more information on see the differences between Arctic and Antarctic sea ice, see this previous Icelights post: Sea ice down under: Antarctic ice and climate

For a more in-depth explanation of this year’s polar ice conditions, see Poles apart: A record-breaking summer and winter.

To view maps of Arctic and Antarctic sea ice derived from satellite data, see the NSIDC Sea Ice Index.

Industry and ice

As the Arctic Ocean becomes increasingly ice-free, many countries are eager to tap into previously inaccessible northern resources. Energy companies seek drilling permits for oil and natural gas, and shipping companies hope to ply newly opened sea routes. Given the unpredictable nature of Arctic sea ice, some wonder if operating in the already inhospitable north will be an economically viable effort. Others believe that even if drilling or shipping is not currently viable, the Arctic is changing fast enough that industry in the Arctic is here to stay. Continue reading

Is stored heat causing Arctic sea ice to freeze later each year?

Graph showing Arctic sea ice minimum dates from 1979 through 2012, derived from satelite records

This graph shows the yearly trend toward later Arctic sea ice minimum dates, but also illustrates the wide variability from year to year. Credit: NSIDC

A reader recently asked if the date of the annual Arctic sea ice minimum is shifting later each year. And if so, is that shift a sign of heat being stored in the Arctic region?

According to the satellite record, Arctic sea ice generally melts to its minimum annual extent between the first and third week of September, after which ice begins freezing again. In recent decades, the Arctic has been gaining heat: Air, land, and ocean temperatures in the region have been slowly rising, and scientists have noted dramatic reductions in summer sea ice extent, as this heat causes more ice to melt away. But is this heat causing sea ice to form later each fall? Continue reading

Do satellites sometimes see ice where there isn’t any?

Readers often ask us, “Why does your sea ice map show sea ice where there is none?” Sometimes our Daily Sea Ice Extent images show sea ice in a particular area, but when readers who live in those areas look out their windows, they see open water—or they even may see ice where our maps show open water. This occurs most frequently along rivers or near coasts. Why does this happen?

Ups and downs of passive microwave

Photograph of Qaanaaq, a small town on the Greenland coast

The rugged coast near Qaanaaq, Greenland, illustrates the challenge to satellite sensors, which must distinguish between land and ocean signals within the same image. Credit: Andy Mahoney|{a href=http://nsidc.org/icelights/files/2012/07/Qaanaaq_coast.jpg}High Resolution Image{/a}

These discrepancies are most often caused by the resolution of the satellite sensor. NSIDC relies on passive microwave sensors to compile daily sea ice maps. These sensors have the advantage of being able to see through the Arctic’s cloudy weather and capture surface data even during long, dark winters, making them ideal for tracking sea ice. The disadvantage, however, is that passive microwave sensors often have low spatial resolution. The sensors collect data in “footprints” that are up to 50 to 70 kilometers (31 to 44 miles) in diameter. Continue reading

What does seeping methane mean for the thawing Arctic?

Photograph of bubbling methane melting a hole through lake ice

Bubbling methane melted a hole in the ice of this otherwise frozen lake in the Brooks Range, Alaska, in April 2011. Credit: Katey Walter Anthony

As people watch the decline of Arctic sea ice, the most obvious sign of climate warming in that region, scientists are noting other signs of change, like methane seeping out of the ground as permafrost thaws and glaciers melt across the Arctic. Scientists suspected these methane seeps existed, but no one had measured how much methane was escaping—until recently. Continue reading