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Date: 2011-05-06 15:41:27 Whillans Ice Stream Byrd Polar Research Center Glaciology Glacier Antarctica Greenland ice sheet Kamb Ice Stream Crevasse Shabtaie Ice Ridge Physical geography Geography of Antarctica Glacial landforms		Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 2,43 MB Share Document on Facebook

	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 DocID: 15aDe - View Document
	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 DocID: 159JZ - View Document
	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 DocID: 159xK - View Document
	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 DocID: 159ou - View Document
	(Bentley, Anandakrishnan, and Rooney, Antarctic JourElectromagnetic studies article nal, this issue). Here we outline the airborne and surface-based on DocID: 14zek - View Document