Summit County Citizens Voice

Patagonian ice fields and glaciers are melting quickly and contributing to sea level rise.

Southernmost ice fields thinning by about six feet per year

By Summit Voice

SUMMIT COUNTY — The largest ice fields in the southern hemisphere outside of Antarctica are melting faster than ever — at a rate that has increased by 50 percent in the past dozen years compared to the 30 years before 2ooo. On average, the southern Patagonia ice fields are thinning by about six feet per year.

Scientists have been monitoring cycles in southern glaciers of the Andes for at least four decades, and have detected an overall loss of ice as the climate warms. Now the region is becoming a poster child for climate change, said Michael Willis, lead author of the study and a research associate at Cornell University in Ithaca, New York.

“We are characterizing a region that is supplying water to sea level at a big rate, compared to its size,” said Willis.

The Southern Patagonian Icefield together with its smaller northern neighbor, the Northern Patagonian Icefield, are the largest icefields in the southern hemisphere — excluding Antarctica. The new study shows that the icefields are losing ice faster since the turn of the century and contributing more to sea level rise than ever before.

Earlier studies determined that between the 1970’s and 2000 both icefields, which feed into surrounding oceans as they melt, together raised global sea levels by an average of .042 millimeters each year. Since 2000, Willis and his colleagues found that number increased to 0.067 mm of sea level rise on average per year – about two percent of total annual sea level rise since 1998.

The Southern Icefield, which Willis and his colleagues focused on, loses around 20 billion tons of ice each year, the scientists calculated —  9,000 times the volume of water stored by Hoover Dam annually. Cumulatively, the Southern Patagonian Icefield has lost enough water over the last 12 years to cover the entire United States with 2.7 centimeters (about 1 inch) of water. Include melting of both icefields, and that amount increases to 3.3 centimeters (1.2 inches), the scientists report.

To map the changing Southern Patagonian Icefield, Willis used 156 satellite images taken over the 12-year period by NASA’s Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument, and data from the Shuttle Radar Topography Mission.

That enabled the researchers to accurately measure how the Southern Patagonian Icefield changed in height and overall size between February 2000 and March 2012.

The team compared its findings with a different set of observations from twin satellites known as the Gravity Recovery and Climate Experiment (GRACE).

“Using ASTER, we think that we have a good idea of where things are changing. But with GRACE we get a good idea of when things are changing. So we have this powerful hybrid,” Willis said. From their new map, the scientists identified individual glaciers and how much each has thinned — i.e. shrunk in height — since 2000. On average, the Southern Patagonian Icefield glaciers have thinned by about 1.8 meters (5.9 feet) per year.

“We find some glaciers are stagnant and even that some have advanced slightly but on the whole, retreat and thinning is prevalent,” Willis said. “Interestingly, we see thinning occurring up to the highest elevations, where presumably it is coldest.”

Warming air temperatures contribute to the thinning at the highest and coldest regions of the ice field, Willis said. Warmer temperatures mean greater chances that rain, as opposed to snow, will fall on and around the glaciers.

This double threat of warming and more rain may, in turn, change the amount of water beneath the glaciers. More water means less friction, so the glaciers start to move faster as they thin, moving even more ice in to the oceans. Rising lakes at the front of the glaciers may also play a part as they eat away at the icy edges faster, causing the glaciers to retreat even further.

“Precipitation is a huge component and likely causes large changes in mass input, and therefore net balance,” said Alex Gardner, an assistant professor at Clark University in Worcester, Massachusetts, who was not involved with the study but studies glaciers and ice sheets. “[This new research] shows very high rates of mass loss and it would be great to see a follow up study on how lakes modify these rates of loss.”

Even though scientists have yet to understand exactly how warming temperatures will continue to influence these South American icefields, this new study provides valuable information for future predictions, Gardner said.

“A study like this really provides a strong data set to validate and calibrate glacial models that we could then use to simulate future changes in glaciers,” he said. “Modeling is really the only tool we have to provide future predictions.”

The collaborative study between scientists from Cornell University and the Center for Scientific Studies (CECs) in Valdivia, Chile, is set to be published 5 September in Geophysical Research Letters, a journal of the American Geophysical Union.

Filed under: climate and weather, Environment, global warming Tagged: | climate, Cornell University, glacial melting, global warming, Michael Willis, Patagonia, sea level rise