Ice decay and the ice regime system ...

The Canadian Ice Regime System takes into account the decay of sea ice by allowing the addition of +1 to the Ice Multiplier for ice that is deemed to be decayed at the "rotten" stage. This report examines this approach based on an analysis of the strength of both first-year sea ice and mul...

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Bibliographic Details
Main Authors: Timco, G. W., Johnston, M., Kubat, I.
Format: Report
Language:English
Published: National Research Council of Canada 2001
Subjects:
Online Access:https://dx.doi.org/10.4224/12340994
https://nrc-publications.canada.ca/eng/view/object/?id=5081890e-146a-4a9f-a82c-2c70019b0329
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spelling ftdatacite:10.4224/12340994 2023-07-23T04:17:50+02:00 Ice decay and the ice regime system ... Timco, G. W. Johnston, M. Kubat, I. 2001 https://dx.doi.org/10.4224/12340994 https://nrc-publications.canada.ca/eng/view/object/?id=5081890e-146a-4a9f-a82c-2c70019b0329 en eng National Research Council of Canada report Report Technical report 2001 ftdatacite https://doi.org/10.4224/12340994 2023-07-03T18:43:08Z The Canadian Ice Regime System takes into account the decay of sea ice by allowing the addition of +1 to the Ice Multiplier for ice that is deemed to be decayed at the "rotten" stage. This report examines this approach based on an analysis of the strength of both first-year sea ice and multi-year sea ice, and the damage statistics for Arctic vessels. The analysis shows that there is no quantitative scientific basis for the current approach of taking into account the decay of sea ice in the Ice Regime System. The report provides a detailed discussion of the analysis with recommendations that (1) the decay of sea ice should be recast in terms of the strength of ice; (2) the summer bonus for reduced ice strength should be given once the ambient air temperature has been above 0°C for one month; (3) an analysis should be performed to define a similar criterion to be used during the growth (autumn) season; and (4) there should be no bonus for decayed multi-year ice. ... Report Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Rotten ENVELOPE(-53.417,-53.417,68.867,68.867)
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language English
description The Canadian Ice Regime System takes into account the decay of sea ice by allowing the addition of +1 to the Ice Multiplier for ice that is deemed to be decayed at the "rotten" stage. This report examines this approach based on an analysis of the strength of both first-year sea ice and multi-year sea ice, and the damage statistics for Arctic vessels. The analysis shows that there is no quantitative scientific basis for the current approach of taking into account the decay of sea ice in the Ice Regime System. The report provides a detailed discussion of the analysis with recommendations that (1) the decay of sea ice should be recast in terms of the strength of ice; (2) the summer bonus for reduced ice strength should be given once the ambient air temperature has been above 0°C for one month; (3) an analysis should be performed to define a similar criterion to be used during the growth (autumn) season; and (4) there should be no bonus for decayed multi-year ice. ...
format Report
author Timco, G. W.
Johnston, M.
Kubat, I.
spellingShingle Timco, G. W.
Johnston, M.
Kubat, I.
Ice decay and the ice regime system ...
author_facet Timco, G. W.
Johnston, M.
Kubat, I.
author_sort Timco, G. W.
title Ice decay and the ice regime system ...
title_short Ice decay and the ice regime system ...
title_full Ice decay and the ice regime system ...
title_fullStr Ice decay and the ice regime system ...
title_full_unstemmed Ice decay and the ice regime system ...
title_sort ice decay and the ice regime system ...
publisher National Research Council of Canada
publishDate 2001
url https://dx.doi.org/10.4224/12340994
https://nrc-publications.canada.ca/eng/view/object/?id=5081890e-146a-4a9f-a82c-2c70019b0329
long_lat ENVELOPE(-53.417,-53.417,68.867,68.867)
geographic Arctic
Rotten
geographic_facet Arctic
Rotten
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_doi https://doi.org/10.4224/12340994
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