Shabtaie Ice Ridge

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1The purpose is to register the image as to its precise location and scale and to quantify the size of features that appear on the images. From Byrd Station, we cooperated with R. Bindschadler (National Aeronautics and Sp

The purpose is to register the image as to its precise location and scale and to quantify the size of features that appear on the images. From Byrd Station, we cooperated with R. Bindschadler (National Aeronautics and Sp

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Language: English - Date: 2011-05-06 16:45:14
2relative movement of the reflecting surface. Since the ice is moving at about 1.5 meters per day and the experimental resolution was about 1 meter, the implication is that the reflecting surface, which we presume to be t

relative movement of the reflecting surface. Since the ice is moving at about 1.5 meters per day and the experimental resolution was about 1 meter, the implication is that the reflecting surface, which we presume to be t

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Language: English - Date: 2011-05-06 07:07:49
3Further data analysis will be a cooperative project involving both institutions. Jerry Bradley (USGS, Denver), Tom Grover (USGS, Denver), Bruce Vaughn (USGS, Tacoma), and Kurt Hayden (Ohio State University) participated

Further data analysis will be a cooperative project involving both institutions. Jerry Bradley (USGS, Denver), Tom Grover (USGS, Denver), Bruce Vaughn (USGS, Tacoma), and Kurt Hayden (Ohio State University) participated

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Language: English - Date: 2011-05-06 16:45:24
4Ice stream C, which is next to ice stream B, is in contrast, virtually stagnant. Its velocity is less than 10 meters per year (McDonald and Whillans, in press), and it must be thickening. The net mass accumulation for th

Ice stream C, which is next to ice stream B, is in contrast, virtually stagnant. Its velocity is less than 10 meters per year (McDonald and Whillans, in press), and it must be thickening. The net mass accumulation for th

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Language: English - Date: 2011-05-06 15:41:32
5 (Bentley, Anandakrishnan, and Rooney, Antarctic JourElectromagnetic studies article nal, this issue). Here we outline the airborne and surface-based on

(Bentley, Anandakrishnan, and Rooney, Antarctic JourElectromagnetic studies article nal, this issue). Here we outline the airborne and surface-based on

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Language: English - Date: 2011-05-06 07:07:42
6Thompson, L.G., E. Mosley-Thompson, J.F. Bolzan, and B.R. KociA 1500 year record of tropical precipitation recorded in ice cores from the Quelccaya Ice Cap, Peru. Science, ), Thompson, L.G., E. M

Thompson, L.G., E. Mosley-Thompson, J.F. Bolzan, and B.R. KociA 1500 year record of tropical precipitation recorded in ice cores from the Quelccaya Ice Cap, Peru. Science, ), Thompson, L.G., E. M

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Language: English - Date: 2011-05-06 18:00:47
7

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Language: English - Date: 2011-05-06 15:41:27