Ice cover deformations at Adams Island, winter 1982–1983

Measurements of horizontal movements of the ice cover near Adams Island, March to June 1983, and in Eclipse Sound, December 1982 to June 1983, indicate no apparent coupling between movement direction and wind or current. Average strain rates in the plane of the ice cover were 10 −10 s −1 , with a ma...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Authors: Sayed, M., Frederking, R. M. W., Bradford, D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1986
Subjects:
Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
Arctic
Arctic Ocean
Adams Island
Eclipse Sound
Online Access:http://dx.doi.org/10.1139/t86-049
http://www.nrcresearchpress.com/doi/pdf/10.1139/t86-049
Description
Summary:Measurements of horizontal movements of the ice cover near Adams Island, March to June 1983, and in Eclipse Sound, December 1982 to June 1983, indicate no apparent coupling between movement direction and wind or current. Average strain rates in the plane of the ice cover were 10 −10 s −1 , with a maximum of 10 −8 s −1 . Similar strain rate values were obtained on Eclipse Sound. Movement rates at Eclipse Sound were of the same magnitude as those at Adams Island, but the direction was quite different. Maximum calculated and measured ice pressures were 500 and 140 kPa, respectively. Key words: ice movements, ice pressures, Canadian Arctic Ocean, oceanography, wind.

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