Results 161 to 170 of about 401,804 (204)
Origin of surface undulations at the Kamb Ice Stream grounding line, West Antarctica
F. Seifert
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Footprint of the Expanded West Antarctic Ice Sheet: Ice Stream History and Behavior
John B. Anderson +4 more
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Seasonal ice dynamics of the Northeast Greenland Ice Stream [PDF]
Bjørk, Anders Anker +5 more
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Evolution of subglacial bedforms along a paleo‐ice stream, Antarctic Peninsula continental shelf
Colm Ó Cofaigh +3 more
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Quaternary Science Reviews, 2001
Abstract The location and behaviour of ice streams is one of the most important controls on ice sheet configuration and stability. In order to reconstruct former ice sheets we need to know ice stream location and timing. Once identified, the beds of palaeo-ice streams provide an unprecedented opportunity to glean information about their basal ...
Chris R. Stokes, Chris D. Clark
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Abstract The location and behaviour of ice streams is one of the most important controls on ice sheet configuration and stability. In order to reconstruct former ice sheets we need to know ice stream location and timing. Once identified, the beds of palaeo-ice streams provide an unprecedented opportunity to glean information about their basal ...
Chris R. Stokes, Chris D. Clark
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Science, 2000
GEOLOGY The size and behavior of past Antarctic ice sheets are essential elements in the quest to understand how and why climate changed in the past and what the consequences may be in the future. Modern observations have shown that Antarctic ice flow is slow and diffuse over most of the interior of the ice sheet but focuses into relatively rapid ...
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GEOLOGY The size and behavior of past Antarctic ice sheets are essential elements in the quest to understand how and why climate changed in the past and what the consequences may be in the future. Modern observations have shown that Antarctic ice flow is slow and diffuse over most of the interior of the ice sheet but focuses into relatively rapid ...
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Paleo-Ice Streams and Ice Stream Boundaries, Ross Sea, Antarctica
1997During the RVIB Nathaniel B. Palmer 1994–01 and 1995–01 cruises, approximately 7141 km of 50 in3 airgun seismic profiles and 12,150 km of 3.5 kHz trackline data were collected from the Ross Sea continental shelf. Ross Sea is a broad embayment, approximately 1500 km wide and 900 km long, on the Antarctic coast (Fig. 1). Water depths range from less than
Stephanie Shipp, John B. Anderson
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