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Flow Properties of the Inland Ice at Camp Century, North-East Greenland
Published online by Cambridge University Press: 20 January 2017
Abstract
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The determination of the surface velocity at Camp Century makes it possible to determine an improved velocity versus depth profile. This profile is interpreted in terms of the ice-flow properties of Wisconsin and Holocene ice. As the Camp Century hole has been located, further improvements can be obtained from direct measurements in the old deep hole.
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