Here’s something about global warming that has left the world’s top scientists baffled. In a bizarre and unexpected twist to the global warming story, the amount of Antarctic ice has actually been increasing while the ice near the Arctic is melting! According to a report in New Scientist, in the southern hemisphere winter, when emperor penguins huddle together against the biting cold, ice on the sea around Antarctica has been increasing since the late 1970s, perhaps because climate change means shifts in winds, sea currents or snowfall.
At the other end of the planet, Arctic sea ice is now close to matching a September 2007 record low at the tail end of the northern summer, in a threat to the hunting lifestyles of indigenous peoples and creatures such as polar bears.
"The Antarctic wintertime ice extent increased at a rate of 0.6 per cent per decade from 1979 to 2006," said Donald Cavalieri, a senior research scientist at the NASA Goddard Space Flight Center in Maryland.
At 19 million square kilometers, it is still slightly below records from the early 1970s of 20 million. Since 1979 however, the average year-round ice extent has risen too.
Some climate skeptics point to the differing trends at the poles as a sign that worries about climate change are exaggerated, but experts say they can explain the development.
"What's happening is not unexpected. Climate modelers predicted a long time ago that the Arctic would warm fastest and the Antarctic would be stable for a long time," said Ted Maksym, a sea ice specialist at the British Antarctic Survey.
A key difference is that Arctic ice floats on an ocean and is warmed by shifting currents and winds from the south. By contrast, Antarctica is an isolated continent bigger than the US that creates its own deep freeze.
According to Cavalieri, some computer models indicate a reduction in the amount of heat coming up from the ocean around Antarctica as one possible explanation for growing ice.
Another theory was that warmer air absorbs more moisture and means more snow and rainfall.
That could mean more fresh water at the sea surface around Antarctica - fresh water freezes at a higher temperature than salt water.
In some places, stronger winds might blow ice out to sea to areas where ice would not naturally form.