1![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 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](https://www.pdfsearch.io/img/4f00b21b575aa4feeb317044fb6321b3.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 16:45:14
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2![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 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](https://www.pdfsearch.io/img/05415f2b96d966b82064648b1251c4aa.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 07:07:49
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3![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 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](https://www.pdfsearch.io/img/7125d1cb065c907925a6ba74dd731830.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 16:45:24
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4![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 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](https://www.pdfsearch.io/img/04ebb56957b6118576100396b3e99ac5.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 15:41:32
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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](https://www.pdfsearch.io/img/010fdebfb2d83601543bdc5b5b35ef1d.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 07:07:42
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6![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 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](https://www.pdfsearch.io/img/c5f62892857c4c09d65d29201310a8eb.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 18:00:47
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7![](https://www.pdfsearch.io/img/4db932ef46a6bfb703251f87e58f0d76.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 15:41:27
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