West Antarctic Ice Sheet

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517 ARTICLES Articles is much weaker.” This is one explanation for the varying amount of

7 ARTICLES Articles is much weaker.” This is one explanation for the varying amount of

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Source URL: www.egu.eu

Language: English - Date: 2015-01-20 07:42:16
52IceSkedDec2014_Final_Layout:22 PM Page 2 Issue 23: December 2014 IceSked Newsletter of the Antarctic Research Centre

IceSkedDec2014_Final_Layout:22 PM Page 2 Issue 23: December 2014 IceSked Newsletter of the Antarctic Research Centre

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Source URL: www.victoria.ac.nz

Language: English - Date: 2014-11-24 17:18:18
53THE BEHAVIOR OF THE WEST ANTARCTIC ICE SHEET Immense change in the extent and volume of the West Antarctic Ice Sheet has occurred over the past 20,000 years and may be ongoing.

THE BEHAVIOR OF THE WEST ANTARCTIC ICE SHEET Immense change in the extent and volume of the West Antarctic Ice Sheet has occurred over the past 20,000 years and may be ongoing.

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Source URL: cci.siteturbine.com

Language: English - Date: 2010-02-17 15:28:10
54and rotation is slowed or stopped by recrystallization. In general on ice sheets, divergent flow causes C axes to cluster symmetrically about the vertical axis, parallel flow causes C axes to cluster about the vertical a

and rotation is slowed or stopped by recrystallization. In general on ice sheets, divergent flow causes C axes to cluster symmetrically about the vertical axis, parallel flow causes C axes to cluster about the vertical a

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:54
55The 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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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:14
56effects when the results of the stable oxygen isotopic measurements become available. R. Alley has studied the 50-meter core obtained by the Polar Ice Coring Office. He has found grain size and firn-structural variations

effects when the results of the stable oxygen isotopic measurements become available. R. Alley has studied the 50-meter core obtained by the Polar Ice Coring Office. He has found grain size and firn-structural variations

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 06:17:27
57Physical studies of firn and ice cores on the Siple Coast clearly are of interest in understanding processes occurring in and adjacent to ice streams and in interpreting geophysical data collected on the ground and from

Physical studies of firn and ice cores on the Siple Coast clearly are of interest in understanding processes occurring in and adjacent to ice streams and in interpreting geophysical data collected on the ground and from

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 15:41:47
58How important is late Cenozoic tectonic and volcanic activity in the west antarctic rift system on the dynamics of the west antarctic ice sheet? JOHN C. BEHRENDT, U.S. Geological Survey, Federal Center, Denver, Colorado

How important is late Cenozoic tectonic and volcanic activity in the west antarctic rift system on the dynamics of the west antarctic ice sheet? JOHN C. BEHRENDT, U.S. Geological Survey, Federal Center, Denver, Colorado

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 17:40:33
59(Nanophanerophytic Montane Tundra) up near the treeline in this zone, where the climate is cold, wet, and windy, and soils are thin. Vegetation is confined to protected areas and thus covers less than 30 percent of the s

(Nanophanerophytic Montane Tundra) up near the treeline in this zone, where the climate is cold, wet, and windy, and soils are thin. Vegetation is confined to protected areas and thus covers less than 30 percent of the s

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 17:59:58
60relative 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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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:49