In theory, more Antarctic snowfall would capture more of the moisture released by the melting, thereby limiting sea level rise.
The global sea level is currently rising at about 0.1 inch (2.8 millimeters) a year.
(Read "Greenland Ice Sheet Is Melting Faster, Study Says" [August 10, 2006].)
Global temperatures have risen, on average, about 1 degree Fahrenheit (0.6 degree Celsius) over the past century.
The Antarctic Peninsula, a 745-mile (1,200-kilometer) arm of land that juts north toward South America, has warmed by about 4.5 degrees Fahrenheit (2.5 degrees Celsius) since 1950.
(See an interactive Antarctica map, photos, video, and more.)
Chunks of ice the size of small U.S. states have disintegrated there in recent years.
(See video: "Huge Iceberg Crumbles Off Antarctica" [November 2005].)
But aside from the Antarctic Peninsula, the annual surface temperature over Antarctica as a whole has remained essentially the same for the past 50 years, Monaghan says.
Some studies suggest a slight cooling since the 1970s; others suggest a slight warming since the 1960s.
"But they are not statistically significant," he said. "You can't say the trend is different than zero."
The same goes for snowfall, he says.
In Science, Monaghan and colleagues write, "[t]here has been no significant change in snowfall since the 1950s."
Richard Alley is a glaciologist at Pennsylvania State University in University Park.
He explains that warmer air holds more moisture, which in the cold Antarctic should fall as snow, according to climate models.
"But the Antarctic is especially complex, in part because of the ozone hole," he said.
Previous research has found the ozone holea gap in or thinning of the upper atmosphere's ozone layerhas contributed to changes in atmospheric circulation over Antarctica.
The changes are causing the interior to cool and the Antarctic Peninsula to warm.
Monaghan likened the circulation pattern to a curtain around Antarctica, isolating the bulk of the continent from the rest of the global climate system.
As the ozone hole recovers, he adds, the study suggests that temperatures in Antarctica should come in line with the rest of the Southern Hemisphere.
"So it's important to figure out, if we see that, how snowfall changes and what impact it will have on sea level," he said.
Monaghan said he is confident that the 50-year snowfall record his team collected is scientifically robust.
Though the ice core and snow stake data are sparse, researchers were able to fill in the voids using a weather model like those used to create the forecasts on the evening news.
The scientists then performed a variety of statistical analyses on the data and recompiled the data in different ways.
"We kept getting the same answer over and over," Monaghan said. "We're pretty sure it's a good answer."
Jay Zwally, a glaciologist at the NASA Goddard Space Flight Center, says the result makes sense.
In an upcoming study on Antarctica's ice sheet, he and colleagues reach a similar conclusion.
"As we saw it, there has not been a significant increasing trend in Antarctic snowfall, except in the region of the Antarctic Peninsula," he said.
But when global temperature changes catch up in the rest of Antarctica, especially the East Antarctic ice sheet, he added, "we'll likely see an associated increase in precipitation."
According to Monaghan, the year-to-year and decade-to-decade change in Antarctic snowfall is so large that "unfortunately, it might take a while to figure out how Antarctica is fitting into the larger climate change picture."
Parkinson, also of NASA's Goddard Center, summed it up this way: "We've got a long way to go before we fully understand what's going on here."
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