Whillans Ice Stream

Results: 44



#Item
1Vol 453 | 5 June 2008 | doi:nature06990 LETTERS Simultaneous teleseismic and geodetic observations of the stick–slip motion of an Antarctic ice stream Douglas A. Wiens1, Sridhar Anandakrishnan2, J. Paul Winber

Vol 453 | 5 June 2008 | doi:nature06990 LETTERS Simultaneous teleseismic and geodetic observations of the stick–slip motion of an Antarctic ice stream Douglas A. Wiens1, Sridhar Anandakrishnan2, J. Paul Winber

Add to Reading List

Source URL: epsc.wustl.edu

Language: English - Date: 2010-06-22 12:55:50
2Downloaded from rspa.royalsocietypublishing.org on November 6, 2013 Subglacial hydrology and the formation of ice streams T. M Kyrke-Smith, R. F Katz and A. C Fowler Proc. R. Soc. A, , published 6 Novem

Downloaded from rspa.royalsocietypublishing.org on November 6, 2013 Subglacial hydrology and the formation of ice streams T. M Kyrke-Smith, R. F Katz and A. C Fowler Proc. R. Soc. A, , published 6 Novem

Add to Reading List

Source URL: foalab.earth.ox.ac.uk

Language: English - Date: 2013-11-06 09:55:10
3www.sut.org MSLED: The Micro Subglacial Lake Exploration Device Alberto E Behar*1,2, Daming D Chen**2, Colin Ho2, Emily McBryan2, Christian Walter1, Joseph Horen2, Scott Foster2, Tyler Foster2, Andrew Warren2, Sai H Vem

www.sut.org MSLED: The Micro Subglacial Lake Exploration Device Alberto E Behar*1,2, Daming D Chen**2, Colin Ho2, Emily McBryan2, Christian Walter1, Joseph Horen2, Scott Foster2, Tyler Foster2, Andrew Warren2, Sai H Vem

Add to Reading List

Source URL: www.dcddcc.com

Language: English - Date: 2016-08-05 04:38:18
4Chapman Conference on the Exploration and Study of Antarctic Subglacial Aquatic Environments (SAE) Baltimore, Maryland USA 15–17 MarchConveners

Chapman Conference on the Exploration and Study of Antarctic Subglacial Aquatic Environments (SAE) Baltimore, Maryland USA 15–17 MarchConveners

Add to Reading List

Source URL: www.agu.org

Language: English - Date: 2015-04-16 11:32:56
5and 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

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:54
6The 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

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:14
7We are presently engaged in fieldwork to study the relict margin area using surface-based ice-penetrating radar to examine the continuity of internal layers, and geodetic surveying to measure ice velocities and strain ra

We are presently engaged in fieldwork to study the relict margin area using surface-based ice-penetrating radar to examine the continuity of internal layers, and geodetic surveying to measure ice velocities and strain ra

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 17:40:16
8wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei

wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 21:19:52
9relative 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

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:49
10Further 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

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:24