The global warming Deniers (and the rest of us) just can't catch a break: Vast areas of the Antarctic ice sheet -- which has 10 times as much ice as Greenland -- is losing mass much faster than anyone expected. And the rate of ice loss has quickened in the last decade. In fact, 2007's ice loss was 75% higher than 2006's.
Jeez, it's almost like ... I don't know ... the whole friggin' planet is melting, and we are to blame! If only we had a group of scientists who would, like, report regularly on the impending catastrophe and explain to us how to avoid it....
As the Washington Post reports:
"Without doubt, Antarctica as a whole is now losing ice yearly, and each year it's losing more," said Eric Rignot, lead author of a paper published online in the journal Nature Geoscience.
Here is the link to Nature's story on the article (note to Nature -- uhh, you folks could include a link to the actual study, too). And here, finally, is the link to the article, "Recent Antarctic ice mass loss from radar interferometry and regional climate modelling" by Eric Rignot et al. A subscription is required for the whole article, but the abstract is available:
Large uncertainties remain in the current and future contribution to sea level rise from Antarctica. Climate warming may increase snowfall in the continent's interior, but enhance glacier discharge at the coast where warmer air and ocean temperatures erode the buttressing ice shelves. Here, we use satellite interferometric synthetic-aperture radar observations from 1992 to 2006 covering 85% of Antarctica's coastline to estimate the total mass flux into the ocean. We compare the mass fluxes from large drainage basin units with interior snow accumulation calculated from a regional atmospheric climate model for 1980 to 2004. In East Antarctica, small glacier losses in Wilkes Land and glacier gains at the mouths of the Filchner and Ross ice shelves combine to a near-zero loss of 4 Gt yr-1. In West Antarctica, widespread losses along the Bellingshausen and Amundsen seas increased the ice sheet loss by 59% in 10 years to reach 132 Gt yr-1 in 2006. In the Peninsula, losses increased by 140% to reach 60 Gt yr-1 in 2006. Losses are concentrated along narrow channels occupied by outlet glaciers and are caused by ongoing and past glacier acceleration. Changes in glacier flow therefore have a significant, if not dominant impact on ice sheet mass balance.
The time to act is now. If not sooner.