Based on a more than 500-foot-long ice core extracted from the thick sheet and containing a snowfall record dating back 2,000 years, the researchers found snow accumulation levels had been rising since around 1900. And the increase is most marked in recent decades, up through the year 2010. It’s a finding that aligns with the notion that climate change, by increasing the atmosphere’s retention of water vapor, is increasing precipitation.
“We know very robustly that the present day is not anything like we’ve seen in the past essentially 2,000 years” for snowfall, said Brooke Medley, a NASA research scientist who was the lead author of the study in the journal Geophysical Research Letters. “It’s receiving much more precipitation.”
Medley conducted the research with colleagues at institutions in the United States, the Netherlands, Switzerland and Germany.
The work, she said, casts light on the large-scale dynamics of how water moves onto, and through, the Antarctic ice sheet to the sea — a process of addition and subtraction whose overall sums determine how the ice sheet is affecting the level of the planet’s oceans. Antarctica contains about 200 feet of potential sea level rise.
A huge amount of snow falls there every year — the equivalent of 5 to 7 millimeters of sea level rise annually, the study states. But at the same time, Medley explained, that snowfall is usually balanced by the loss of ice around the periphery of the ice sheet, where it melts in contact with ocean waters or slides out into sea and eventually floats away in large chunks.
Any tweak to either side of this equation — more snowfall, or more ice loss — would change Antarctica’s contribution to sea level rise. We already know Antarctic ice loss has been increasing, particularly in the vulnerable West Antarctic region, which has drawn massive media attention as several large glaciers have markedly retreated.
“It’s ‘what goes in’ versus ‘what goes out,’ ” Medley said. “Most studies aren’t interested in the ‘what goes in’ part, but they’re equally important.”
Sure enough, the study found that snowfall atop western Queen Maud Land is 25 percent larger than snowfall in the preindustrial era, before the late 19th century. Meanwhile, this has happened even as temperatures have risen by a sharp 1 degree Celsius (1.8 degrees Fahrenheit) per decade at Kohnen Station, a weather outpost in the region that has been recording temperatures over the last 19 years.
To provide a significant counterweight to Antarctica’s expected long-term ice loss, however, the increased snow accumulation would have to continue in coming decades and also occur elsewhere across the continent — areas the study did not cover. The researchers surmised that overall, this trend of growing precipitation that they documented is probably occurring over a vast area of Antarctica — about 7 to 10 percent of the ice sheet.
Meanwhile, when the scientists compared the results to the findings of a group of global climate models, they found that temperature rises and snowfall accumulation were outstripping the pace of model predictions, even in an extreme global warming scenario.
Indeed, the study notes that models predict an increase in snowfall accumulation atop Antarctica by the end of the century that is equivalent to 1.5 millimeters of sea level annually. Such a large amount, if not offset by increased ice losses at the periphery of Antarctica, would counter about half of current sea level rise.
However, while snowfall increases across Antarctica are expected, the current research only addresses the western part of Queen Maud Land. Further research would have to show whether anything like this amount of change is happening elsewhere — and to what extent it may be offsetting ice loss from West Antarctica and other places.
Still, several experts consulted by The Post agreed the new research could have significant implications.
“The notion that increased accumulation in East Antarctica will at least partly offset increased ice outflow has long been discussed,” said Ted Scambos, an Antarctic expert at the National Snow and Ice Data Center in Boulder, Colo., by email. “The problem is that in the long term, if the Earth warms, the ice sheets shrink. The compensation effect does not last.”
“For human planning, however, delaying the [sea level rise] by a few centuries is a bit like saying, ‘no need to worry — never mind,'” Scambos continued. “If true, it could have a huge impact on the eventual pace of [sea level rise].”
Andrew Shepherd, an Antarctic expert at the University of Leeds, said the gap between climate models and observations in this case requires further research.
“It’s important to find out whether this discrepancy is widespread across the continent, and present in other climate models, so that climate projections can be revised to take increased snowfall into account, as this could offset a proportion of expected future sea level rise,” he said by email.
The current result is different, however. Medley stressed in an interview that while snowfall accumulation could be partially mitigating ice loss in West Antarctica, she is not asserting that Antarctica is gaining ice — just that losses may be offset somewhat.
“If you take the net, we’re still looking at ice loss,” Medley said.
At the same time, the findings in a sense presume the reality of human-caused climate change — after all, temperatures are rising rapidly in Queen Maud Land (albeit with only a short thermometer record of 19 years so far), and an increase in precipitation is what would be expected to occur in response to climate change.
So while there’s nothing here that refutes climate change, the research may point to a silver lining — especially if verified in further research.