Ice action on Nanisivik wharf, Strathcona Sound, N.W.T., winter 1978–1979

Field observations have been made over three winters at a vertically faced wharf in an area of limited horizontal ice movement but substantial vertical movement due to tides. Ice thickness was profiled and vertical ice movements were measured. A reasonably consistent pattern of ice behaviour adjacen...

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Bibliographic Details
Published in:Canadian Journal of Civil Engineering
Main Author: Frederking, R. M. W.
Format: Article in Journal/Newspaper
Language:French
Published: Canadian Science Publishing 1980
Subjects:
Online Access:http://dx.doi.org/10.1139/l80-064
http://www.nrcresearchpress.com/doi/pdf/10.1139/l80-064
Description
Summary:Field observations have been made over three winters at a vertically faced wharf in an area of limited horizontal ice movement but substantial vertical movement due to tides. Ice thickness was profiled and vertical ice movements were measured. A reasonably consistent pattern of ice behaviour adjacent to the wharf was established, characterized by the formation of a transition ice zone between the first-year sea ice and the wharf. The behaviour and factors affecting growth of this zone are described.