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Wednesday, June 26, 2013

Antarctica - What Lies Beneath

Information from an article originally published by NASA on Jun 4, 2013

http://www.nasa.gov/topics/earth/feat...

The world's understanding of what lies beneath the world's biggest ice sheet has taken another leap forward. In the video below NASA strips away the Antarctic ice sheets to reveal a new, and much more detailed map of the bedrock below. This map called Bedmap2, gives a clearer picture of Antarctica from the ice surface down to the bedrock below. Bedmap2 is a significant improvement on the previous collection of Antarctic data—known as Bedmap—that was produced more than 10 years ago. The product was a result of work led by the British Antarctic Survey, where researchers compiled decades worth of geophysical measurements, such as surface elevation measurements from NASA's Ice, Cloud and Land Elevation Satellite, known as ICESat, and ice thickness data collected by Operation IceBridge.

This video is public domain and can be downloaded at: http://svs.gsfc.nasa.gov/goto?4060







The following images depict the differences between Antarctica's ice sheet with its underlying topography. Note that the vertical scale has been magnified by a factor of 17 to make terrain features such as mountains and valleys more visible.)
Credit: NASA's Goddard Space Flight Center






With effects ranging from influencing ocean currents to raising sea level, Antarctica plays a large role in the global climate system. Researchers are using a variety of methods to understand how Antarctica will react to a changing climate, but limited information on ice thickness and what lies beneath the ice makes this work challenging. Now, thanks to work led by the British Antarctic Survey published recently in the journal The Cryosphere, scientists will have a new detailed map of the frozen continent.

The Model

Ice sheet modeling is an area that will likely make heavy use of Bedmap2 data. Ice sheets are thick, dome-shaped formations of ice that cover large areas of land. There are two major ice sheets on Earth, one covering Greenland and one over Antarctica. Ice sheets are formed as snow accumulates and is compacted into ice over many years. "Ice sheets grow because of snow, and like honey poured on a plate, spread outward and thin due to their own weight," said Sophie Nowicki, an ice sheet scientist at NASA's Goddard Space Flight Center in Greenbelt, Md.

Ice sheet researchers use computer models to simulate how ice sheets will respond to changes in ocean and air temperatures. An advantage of these simulations is that they allow testing of many different climate scenarios, but the models are limited by how accurate the data on ice volume and sub-ice terrain are. "In order to accurately simulate the dynamic response of ice sheets to changing environmental conditions, such as temperature and snow accumulation, we need to know the shape and structure of the bedrock below the ice sheets in great detail," said Michael Studinger, IceBridge project scientist at NASA Goddard.

Knowing what the bedrock looks like is important for ice sheet modeling because features in the bed control the ice's shape and affect how it moves. Ice will flow faster on a downhill slope, while an uphill slope or bumpy terrain can slow an ice sheet down or even hold it in place temporarily. "The shape of the bed is the most important unknown, and affect how ice can flow," said Nowicki. "You can influence how honey spreads on your plate, by simply varying how you hold your plate." The vastly improved bedrock data included in Bedmap2 should provide the level of detail needed for models to be realistic.

NASA's Operation IceBridge

 
graphical representation of Antarctica with survey flight paths superimposed
A significant portion of the data in Bedmap2 was collected by NASA's Operation IceBridge. Flight paths from the 2009, 2010 and 2011 Antarctic campaigns are shown here as dark green lines. NASA DC-8 flights originated from Punta Arenas, Chile, on the left side of the image. Flight lines in East Antarctica represent surveys flown by the Institute for Geophysics at the University of Texas at Austin, one of IceBridge's partnering organizations.
Credit: NASA Goddard's Scientific Visualization Studio

IceBridge data also played a big role by providing data on parts of Antarctica where there have been few to no measurements before. One such area is the Recovery Ice Stream, which IceBridge essentially put on the map with data from its 2011 Antarctic campaign. Both NASA and the U.S. National Science Foundation have invested a great deal of time and money in radars like MCoRDS and airborne campaigns like IceBridge over the years.

NASA's contributions go beyond merely collecting this data. By making its data freely available to researchers, NASA is leading a positive trend with researchers. "We hope that other partners will also go down this road," said Fretwell. Collecting radar sounding data over Antarctica is an expensive effort, which has led some researchers to be understandably protective. This could change, however, as more researchers make use of freely available data.

"More and more people in the research community realize the tremendous value of making data freely available," said Studinger.

For more information on NASA's Operation Ice Bridge, visit:


George Hale
NASA's Goddard Space Flight Center, Greenbelt, Md.

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