This image and the ice covered one below depict the differences between Antarctica's ice sheet with its underlying topography. (Vertical scale has been magnified by a factor of 17 to make terrain features such as mountains and valleys more visible.) The topography map, called Bedmap2, was compiled by the British Antarctic Survey and incorporates millions of new measurements.
courtesy NASA's Goddard Space Flight Center, SOURCE
Antarctica's ice sheet (see Bedmap2 caption).
courtesy NASA's Goddard Space Flight Center, SOURCE
The original Bedmap topography
courtesy NASA's Goddard Space Flight Center, SOURCE
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.
courtesy NASA's Goddard Space Flight Center, SOURCE
This VIDEO strips away Antarctic ice to reveal a new, and much more detailed map of the bedrock below. This map, called Bedmap2, was compiled by the British Antarctic Survey and incorporates millions of new measurements, including substantial data sets from NASA's ICESat satellite and an airborne mission called Operation IceBridge.
courtesy NASA Goddard's Scientific Visualization Studio, SOURCE
New ice-free map of Antarctica

Posted: Jun 10, 2013 02:29 pm EDT

(By Correne Coetzer) After studying decades of data, scientists of the British Antarctic Survey (BAS) and NASA released a virtual map of Antarctica showing the White Continent without snow and ice.  The new dataset, called Bedmap2, is a new suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60°S.

 

Bedmap2

 

BAS 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.

 

A new dataset called Bedmap2 gives a clearer picture of Antarctica from the ice surface down to the bedrock below. The previous collection of Antarctic data, known as Bedmap, was produced in 2001. 

 

Bedmap2, like the original Bedmap, is a collection of three datasets—surface elevation, ice thickness and bedrock topography. Over the past decade there have been many Antarctic surveys, which vastly increased the amount of available data. Researchers used data from satellites, aircraft and surface-based surveys to build a data product with higher resolution, greater coverage and improved precision.

 

The extensive use of GPS data in more recent surveys improved the precision in resolution, coverage and precision that will lead to more accurate calculations of ice volume and potential contribution to sea level rise. 

Total ice volume and sea level contribution remain similar to calculations using the original Bedmap, but Antarctica's average bedrock depth, deepest point and ice thickness estimates have all increased.

 

Key statistics

 

Several features of the bed have been revealed for the first time including a new deepest point. The bed under the Byrd Glacier in Victoria Land is 2,870 metres below sea level making it the lowest point on any of the Earth’s continental plates.

 

Key stats:

 

The volume of ice in Antarctica is 4.6% greater than previously thought.

 

The mean bed depth of Antarctica, at 95 metres, is 60 m lower than estimated.

 

The volume of ice that is grounded with a bed below sea level is 23% greater than originally thought meaning there is a larger volume of ice that is susceptible to rapid melting. The ice that rests just below sea level is vulnerable to warming from ocean currents.

 

The total potential contribution to global sea level rise from Antarctica is 58 metres, similar to previous estimates but a much more accurate measurement.

 

The new deepest point, under Byrd Glacier, is around 400 metres deeper than the previously identified deepest point.

 

Previous/Related

 

A detailed explanation of Bedmap2 is published in the Journal of Cryosphere.

 

The Research Paper

 

AGAP Antarctica findings: Gamburtsev's ghost mountains lived twice

 

Dark, hot, lost world discovered on the seafloor near Antarctica

 

NASA's IceBridge 2012 Antarctic Campaign

 

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