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Author : Robert A. Bindschadler
Publisher : Unknown
Page : 158 pages
File Size : 55,9 Mb
Release : 1991
Category : Ice sheets
ISBN : NASA:31769000469653
Author : Robert A. Bindschadler
Publisher : Unknown
Page : 156 pages
File Size : 43,9 Mb
Release : 1991
Category : Ice sheets
ISBN : UCSD:31822005692744
Author : R. A. Bindschadler
Publisher : Unknown
Page : 128 pages
File Size : 49,9 Mb
Release : 1990
Category : Electronic
ISBN : OCLC:664566913
Author : Robert A. Bindschadler
Publisher : Unknown
Page : 68 pages
File Size : 49,8 Mb
Release : 1991
Category : Ice sheets
ISBN : UCSD:31822005692728
Author : Anonim
Publisher : Unknown
Page : 910 pages
File Size : 49,5 Mb
Release : 1991
Category : Aeronautics
ISBN : UIUC:30112075701992
Author : Anonim
Publisher : Unknown
Page : 134 pages
File Size : 51,7 Mb
Release : 1993
Category : Aeronautics
ISBN : STANFORD:36105024716156
Author : Anonim
Publisher : Unknown
Page : 122 pages
File Size : 41,6 Mb
Release : 1993
Category : Aeronautics
ISBN : NASA:31769000660368
Author : W. Richard Peltier
Publisher : Springer Science & Business Media
Page : 673 pages
File Size : 50,5 Mb
Release : 2013-06-29
Category : Science
ISBN : 9783642850165
According to my latest model for the last glacial maximum (LGM) (Grosswald 1988), the Arctic continental margin of Eurasia was glaciated by the Eurasian ice sheet, which consisted of three interconnected ice domes --the Scandinavian, Kara, and East Siberian. The Kara Sea glacier was largely a marine ice dome grounded on the sea's continental shelf. The ice dome discharged its ice in all directions, northward into the deep Arctic Basin, southward and westward onto the mainland of west-central North Siberia, the northern Russian Plain, and over the Barents shelf into the Norwegian-Greenland Sea On the Barents shelf, the Kara ice dome merged with the Scandinavian ice dome. In the Arctic Basin the discharged ice floated and eventually coalesced with the floating glacier ice of the North-American provenance giving rise to the Central-Arctic ice shelf. Along its southern margin, the Kara ice dome impounded the northward flowing rivers, causing the formation of large proglaciallakes and their integration into a transcontinental meltwater drainage system. Despite the constant increase in corroborating evidence, the concept of a Kara ice dome is still considered debatable, and the ice dome itself problematic. As a result, a paleogeographic uncertainty takes place, which is aggravated by the fact that a great deal of existing knowledge, no matter how broadly accepted, is based on ambiguous interpretations of the data, most of which are published in Russian and, therefore, not easily available to western scientists.
Author : Anonim
Publisher : Unknown
Page : 68 pages
File Size : 42,7 Mb
Release : 1991
Category : Electronic
ISBN : NASA:31769000469646
Author : World Data Center A--Oceanography
Publisher : Unknown
Page : 486 pages
File Size : 47,8 Mb
Release : 1990
Category : Oceanography
ISBN : UCSD:31822009792847
Author : Anonim
Publisher : Unknown
Page : 332 pages
File Size : 42,8 Mb
Release : 1991
Category : Cosmic physics
ISBN : UOM:39015023286316
Author : Anonim
Publisher : Unknown
Page : 1374 pages
File Size : 48,5 Mb
Release : 1991
Category : Government publications
ISBN : MINN:31951P001783151
Author : Anonim
Publisher : Unknown
Page : 232 pages
File Size : 48,9 Mb
Release : 1991
Category : Aeronautics
ISBN : UOM:39015022348133
Author : Anonim
Publisher : Unknown
Page : 1162 pages
File Size : 55,9 Mb
Release : 1993-06
Category : Marine biology
ISBN : UVA:X002434907
Author : National Science Foundation (U.S.),West Antarctic Ice Sheet Initiative
Publisher : Unknown
Page : 75 pages
File Size : 53,9 Mb
Release : 1995
Category : Antarctica
ISBN : OCLC:257127059
