t h u k v Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The

Bibliographic Details
Main Authors: Doi:. /j. Quaolga Nikolskaya, Leonid Polyak, Matti Saarnisto, Christine Siegert, Martin J. Siegert, Robert F. Spielhagenw, Ruediger Steins
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Arctic
Ice Sheet
Kanin peninsula
Taimyr
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.2903
Description
Summary:t h u k v Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The

Similar Items