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4074 viewsTed pretends to surf on a sastrugi, a snow formation caused by strong winds.
Image Credit: Ted Scambos, NSIDC
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1406 viewsTed Scambos smiles from the driver's seat of one of the traverse vehicles.
Image Credit: Ted Scambos, NSIDC
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Allan Hills1506 viewsThe Allan Hills are located on the flanks of the TransAntarctic Mountains. Ice upwells onto the hills where combinations of winds and solar insolation cause the ice to quickly ablate. Meteorites that once fell over a large region of East Antarctica have been carried by glacier motion into this small locality.
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Antarctica1757 viewsSea ice concentration from the NSIDC Sea Ice Index.
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Ross Ice Shelf2375 viewsAVHRR image of West Ross Ice Shelf, Antarctica on 27 January 2001.
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Antarctic Snow Dunes1657 viewsExtensive snow dunes wrinkle the surface of large parts of East and West Antarctica. The dunes are up to 100 kilometers long and separated by 2 to 4 kilometers, but only a few meters high. Comparison of modern satellite images with images acquired four decades earlier reveals that the dunes are nearly motionless.
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Fimbul Ice Shelf1632 viewsThe Fimbul Ice Shelf is punctuated by numerous ice rises that occur where isolated rocky islands are covered by ice. Ice shelves may be particularly sensitive to changes in climate, and recently ice shelves in the Antarctic Peninsula have experienced rapid retreat
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Tabular Iceberg2418 viewsThis tabular iceberg was photographed near Antarctica during the IceTrek expedition in 2006.
Photo Credit: Courtesy Ted Scambos, NSIDC
IceTrek Web site
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1623 viewsThis Landsat image of Crane Glacier on the Antarctic Peninsula is overlain with ICESat and Airborne Topopgraphic Mapper (ATM) tracks. ATM is a lidar sensor that is now part of the IceBridge mission. Over time, ICESat and ATM measurements, together with visible imagery, can detect thinning of the ice and accelerated flow of ice into the ocean. Large glaciers such as Crane have the potential to contribute significantly to sea level rise.
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1104 viewsOne of the most studied and interesting ice streams in Antarctica, Ice Stream B shows a number of features that indicate past changes and ongoing evolution. In this subscene the upstream ends of several ice stream shear margins are highlighted. Characteristic crevasse patterns, nicknamed "chromosomes," mark the ends of several of these margin traces.
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995 viewsThis poster illustrates the required protective gear for traveling to Antarctica.
Image Credit: Ted Scambos, NSIDC
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988 viewsThis display shows the clothing required for travel to Antarctica.
Image Credit: Ted Scambos, NSIDC
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