Research team uses innovative techniques to map water beneath Antarctic ice shelf

Feb 20, 2013 by Anne Danahy

(Phys.org)—Antarctica's recent summer season was a success for the Penn State researchers who camped out on the ice for nearly two months. Their efforts are part of a National Science Foundation-funded project to better understand melting that is happening on the Pine Island Glacier ice shelf, an extension of the Antarctic ice sheet. The Penn State team is in charge of mapping the ocean cavity beneath the ice shelf.

The weather cooperated in December and early January, giving Penn State graduate student Kiya Riverman and research associate Leo Peters the opportunity to use several methods to generate the images needed to create an of the ocean circulation. "We were able to collect more than enough data to produce a meaningful map of the ocean cavity and thickness variations," Riverman said.

Riverman and Peters are working with Professor of Geosciences Sridhar Anandakrishnan, a lead researcher on the Pine Island Glacier project, which is an international effort that also receives support from NASA and includes researchers from the Naval Postgraduate School, the , University of Alaska and New York University.

Water circulates under the Pine Island shelf, which is a floating extension of the . The Penn State team's part of the project is developing a map of that cavity beneath the 37-mile-long shelf. The images of will be used to fine tune models of future melting behavior and understand the role of rising that are believed to be contributing to the melting of the ice shelf.

An aerial view of the Pine Island Glacier camp. Credit: Kiya Riverman

"Changes in the size of this ice shelf are a direct control on the speed of the glacier, which in turn is able to draw ice from a large portion of ," Riverman said. "This means that changes on the Pine Island Ice Shelf have ramifications for much of Western Antarctica."

The site of the work is 1,200 miles from McMurdo Station on Antarctica and can be reached only by special planes that can land on ice. Riverman and Peters used reflection seismology to generate an image of the seafloor and ice-penetrating radar to map changes in ice thickness.

This video is not supported by your browser at this time.
Sridhar Anandakrishnan has completed many seasons of Antarctic research. In December 2006, as he describes in this audio diary he and his team traveled to Ross Island to search for a body of water that some scientists say lies deep below the surface of the South Pole. By lowering explosives into deep holes, the team recorded rebound sounds through geophones to estimate the distance to the bottom of the ice. The resulting seismic data was used to create cross-section maps of the ice sheets. Anandakrishnan hopes the data will help predict future changes in sea-level and possibly unveil new microscopic organisms.

For the first of these techniques, the team pounded sledgehammers against steel plates and set off explosives to create energy on the surface of the ice.

"This energy travels through the ice and seawater and bounces off the seafloor," Riverman explained. "Using instruments called geophones, we record vibrations in the ice at the surface and the amount of time it takes for that energy to bounce off the seafloor. This tells us the seafloor depth. By repeating explosions or hammer blows at different locations, we can start to develop a map of the seafloor."

For the second technique, the team dragged a low-frequency radar unit behind a snowmobile to map changes in the thickness of the ice.

The NSF recently singled out the project is one of three Antarctic science initiatives that have achieved technological milestones with innovative approaches to drilling.

"Although additional challenges doubtless lie ahead for these projects in the harsh Antarctic environment, these successes are a testament to both scientific and engineering ingenuity and the logistical support needed to mount such ambitious and scientifically promising programs," said Scott Borg, who heads Antarctic Sciences in NSF's Office of Polar Programs.

Explore further: Climate researchers measure the concentration of greenhouse gases above the Atlantic

add to favorites email to friend print save as pdf

Related Stories

Ocean currents speed melting of Antarctic ice

Jun 26, 2011

Stronger ocean currents beneath West Antarctica's Pine Island Glacier Ice Shelf are eroding the ice from below, speeding the melting of the glacier as a whole, according to a new study in Nature Geoscience. A grow ...

Antarctic rift subject of international attention

Oct 16, 2012

As NASA's Operation IceBridge resumed Antarctic science flights on Oct. 12, 2012, researchers worldwide had their eyes on Antarctica's Pine Island Glacier ice shelf, the site of a large rift measured during ...

Recommended for you

New discovery helps solve mystery source of African lava

1 hour ago

Floods of molten lava may sound like the stuff of apocalyptic theorists, but history is littered with evidence of such past events where vast lava outpourings originating deep in the Earth accompany the breakup ...

Climate change likely to make Everest even riskier

2 hours ago

Climbing to the roof of the world is becoming less predictable and possibly more dangerous, scientists say, as climate change brings warmer temperatures that may eat through the ice and snow on Mount Everest.

NASA gets two last looks at Tropical Cyclone Jack

22 hours ago

Tropical Cyclone Jack lost its credentials today, April 22, as it no longer qualified as a tropical cyclone. However, before it weakened, NASA's TRMM satellite took a "second look" at the storm yesterday.

User comments : 0

More news stories

Climate change likely to make Everest even riskier

Climbing to the roof of the world is becoming less predictable and possibly more dangerous, scientists say, as climate change brings warmer temperatures that may eat through the ice and snow on Mount Everest.