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Two men hunch over a cylinder of ice.
Photo Credit: Tommy Cox/Wais Divde
Nicolai Mortensen and Patrick Casssidy work on the sonde electronics of the DISC Drill during the 2009-10 WAIS Divide ice-coring field season in West Antarctica. The drill is the most advanced of its kind on the planet.
 

New methodologies

Schoenenmann, a tall, lean man with a fondness for rock climbing, is interested in developing a new methodology for measuring the stable isotope oxygen-17. The work will provide new information on the sea surface humidity during the Last Glacial Maximum (LGM), when the last glacial period peaked about 20,000 years ago.

Previous research indicated conditions were dry, but other data suggest the humidity may have been higher, accompanied by more precipitation, according to Schoenenmann. He hopes the O17 record will shed more light on the issue.

“It’s really an exciting new measurement,” he said. “The WAIS Divide record will be the first one to have an O17 record.”

Thomas Bauska External Non-U.S. government site is another PhD student who has worked in the Middle of Nowhere, West Antarctica, on the ice-coring project. He was at WAIS Divide during the most recent field season, when the drill reached a bottom depth of 2,560 meters.

Carts loaded with ice cores.
Photo Credit: Chad Naughton
Ice core storage room at WAIS Divide.

Like Schoenenmann, he has developed a new methodology to analyze stable isotopes in the gases trapped in the ice — in this case, carbon-12 and carbon-13 — working in the laboratory with WAIS Divide PI Ed Brook at Oregon State University External Non-U.S. government site.

The gas measurements are perhaps some of the most exciting because they will address a central question regarding the relationship between carbon dioxide and temperature.

Current ice core records show that in the past temperature increased, followed several centuries later by an increase in carbon dioxide — but there is still a large uncertainty in the timing of this sequence.

Most scientists believe past climate warming was caused by variations in the Earth’s orbit, called Milankovitch cycles, which changed how sunlight was distributed on the surface of the planet. But the orbital changes alone are probably not enough to end an ice age, just to initiate environmental changes that allow more carbon dioxide into the atmosphere to create the greenhouse effect.

“Humans are now increasing the level of CO2 in the atmosphere to levels higher than at any time in the last 800,000 years,” Taylor explained. “The effect will be similar to what happened when changes in the Earth’s orbit caused the oceans to release CO2: No change for while, then lots of warming and changes in rainfall on a scale that humans have never experienced.”

By studying ice cores, which record how this process worked in the past, scientists will be able to predict more accurately how human releases of CO2 will affect climate. Specifically, the analysis of the ancient ice by Bauska and others will identify the sources of CO2 and help figure out why it varies naturally.

“You need the large amount of samples that WAIS Divide can give us to make these measurements,” Bauska noted.

Ice time

Results from the work by young scientists like Schoenenmann, Koffman, Fudge, Bauska and the many PIs are still well down the road, according to Taylor. Only about 600 meters of ice has been processed previously, containing the most recent 2,000 years of climate history.

Long room with people working on ice.
Photo Credit: Chad Naughton
The core-handling room at WAIS Divide, which is kept at minus 25 centigrade.

“That’s the annoying thing with these ice cores. You drill them, and it can be like two years before the ice gets to the lab. It’s another year or two of measurements. And then another couple of years to figure out what it [means],” Taylor mused.

The brittle ice being processed this summer was originally cored from the ice sheet during the brief 2008-09 field season. It had to spend a year on site before it could be moved to allow the ice to “relax” so it would not become brittle and get damaged during transport to the United States.

The delay is partly due to the need for conducting the CPL and the different analyses back in the United States. That’s in contrast to projects like GISP-2, Greenland Ice Sheet Project 2 External Non-U.S. government site, or the recently completed North Greenland Eemian Ice Drilling project External Non-U.S. government site, which hit bedrock last month.

In Greenland, the scientists make many measurements in a snow trench carved out for that purpose. However, it’s too expensive to bring all of the equipment and people needed for such an operation to West Antarctica, where the field camp is reached by a ski-equipped military aircraft when the weather is good enough to fly.

“Going to Greenland is like a vacation compared to a place like WAIS Divide, where it takes at least three weeks just to come and join us for lunch,” Taylor said.

By the time the CPL crew reaches about 2,000 meters in mid-August, the climate record will reach back about 8,000 years. The first 40,000 years are expected to be thick enough for the annual layers to be counted before the ice flow makes the layers too thin to resolve.

Taylor said he is hopeful that the drilling team will reach its final target depth of 3,330 meters during the 2010-11 season, bringing back another 1,400 meters of ice for next summer’s CPL.

“We’re really looking forward to pushing that last piece of ice through the drill,” Taylor said.

NSF-funded research in this story: Kendrick Taylor, Desert Research Institute, Award Nos. 0944191, 0440817, 0440819, 0944348, 0739780 and 0230396 External U.S. government site. For a complete list of all funded projects related to the project, see the WAIS Divide webpage of funded projects at http://waisdivide.unh.edu External Non-U.S. government site.Back   1 2 3

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Curator: Peter Rejcek, Antarctic Support Contract | NSF Official: Winifred Reuning, Division of Polar Programs