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Person examines ice core.
Photo Credit: Don Voigt/WAIS Divide
Scientist Don Voigt logs the last meter of WAIS Divide ice core from a depth of 3,404 meters. The research team deepened the borehole by more than 70 meters over last year, when project personnel had completed major coring operations after five years of drilling. The project represents the deepest core ever drilled by the U.S. ice-coring community.

The last core

WAIS Divide deepens borehole for research into climate change

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A different sort of countdown was under way on New Year’s Eve at a remote field camp in West Antarctica.

In this case, the count literally went down to near the bottom of the West Antarctic Ice Sheet (WAIS), where drillers extracted about 72 more meters of ice cores in five days, reaching a final depth of 3,405 meters for the multiyear WAIS Divide Ice Core project.

Last year, project personnel had completed major coring operations after five years of drilling, stopping at about 3,331 meters, representing the deepest core ever drilled by the U.S. ice-coring community. [See previous article — Deep core complete: WAIS Divide project finishes five-year effort to retrieve 3,331 meters of ice.] Russians have the record for the deepest ice core, which they drilled in the 1990s at Vostok Station in East Antarctica, to a depth of 3,701 meters.

“The core quality has been beyond excellent; the warm ice surprisingly presented no obstacle at all, and the speed with which the drilling was completed was astounding,” wrote Jeff Severinghaus External Non-U.S. government site, chief scientist at the WAIS Divide field camp and a professor of geosciences at Scripps Institution of Oceanography External Non-U.S. government site.

Ice in a drill bit.
Photo Credit: Kristina Dahnert/WAIS Divide
Final core from the WAIS Divide borehole.

“All this suggests to me that the engineering for warm-ice drilling that went into DISC has really paid off,” he added, referring to the high-tech drill that was developed by engineers with the Ice Drilling Design and Operations (IDDO) External Non-U.S. government site group at the University of Wisconsin-Madison External Non-U.S. government site.

The ice core represents a window back in time on the Earth’s climate. Scientists can analyze bubbles of various gases trapped in the ice — particularly the important greenhouse gas carbon dioxide — to get a sample of the ancient atmosphere. Dust and chemicals found in the ice can also provide details about past climate.

Scientists like Kendrick Taylor External Non-U.S. government site are eager to start seeing results after years of planning and organizing the massive project, which began in earnest in 2000. Chief scientist for the WAIS Divide Ice Core project External Non-U.S. government site from the Desert Research Institute External Non-U.S. government site in Nevada, Taylor said it would take researchers about two years to finish their measurements on the ice, and another year to interpret and publish the data.

“I am really thankful for Julie Palais, our program manager at NSF, for pushing this project along all these years,” Taylor said. “Besides improving the ability to predict how human activity will change climate, the best part of the project is working with my science and support colleagues, many of whom have become great friends during the project.”

Researchers had expected to recover ice as old as 100,000 years, but preliminary indications from processing the ice last year at the National Ice Core Laboratory External U.S. government site in Lakewood, Colo., suggest it is may be about 62,000 years old at the bottom of the ice sheet.

People stand around WAIS drill.
Photo Credit: Don Voigt/WAIS Divide
The drill and core handling crew in front of the DISC Drill.
[See previous article — Getting to the bottom: NICL team processes deepest ice from WAIS Divide project.]

While some ice-core records reach back more than 800,000 years into the past, the WAIS Divide ice core will boast the most high-resolution record to date, thanks to the high snow accumulation in the region that produces thick annual layers throughout much of the core.

Taylor and his graduate student, T.J. Fudge External Non-U.S. government site from the University of Washington External Non-U.S. government site, have used seasonal changes in the chemistry of the ice to determine the age of the ice at different depth. So far, they have counted 30,366 annual layers, like counting tree rings.

“Additional measurements might push the annual dating back further, but it is already the most detailed record from Antarctica of the changes that occurred during the transition from the last ice age to the current warm period,” Taylor said.

That sort of detail will help provide for an unprecedented reconstruction of carbon dioxide concentrations in the atmosphere over that time.1 2   Next

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