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TC | Volume 12, issue 11
The Cryosphere, 12, 3577–3588, 2018
https://doi.org/10.5194/tc-12-3577-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 3577–3588, 2018
https://doi.org/10.5194/tc-12-3577-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 19 Nov 2018

Research article | 19 Nov 2018

What historical landfast ice observations tell us about projected ice conditions in Arctic archipelagoes and marginal seas under anthropogenic forcing

Frédéric Laliberté et al.
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Cited articles  
Alt, B., Wilson, K., and Carrieres, T.: A case study of old ice import and export through Peary and Sverdrup channels in the Canadian Arctic Archipelago: 1998–2004, Ann. Glaciol., 44, 329–338, https://doi.org/10.3189/172756406781811321, 2006. 
Barry, R. G., Moritz, R. E., and Rogers, J. C.: The fast ice regimes of the Beaufort and Chukchi sea coasts, Alaska, Cold Reg. Sci. Technol., 1, 129–152, 1979. 
Brown, R. and Cote, P.: Interannual variability of landfast ice thickness in the Canadian high arctic, 1950–89, Arctic, 45, 273–284, 1992. 
Canadian Ice Service: Sea Ice Climatic Atlas: Northern Canadian Waters 1981–2010, 995 pp., Ottawa, 2011. 
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Short summary
Ice that forms over marginal seas often gets anchored and becomes landfast. Landfast ice is fundamental to the local ecosystems, is of economic importance as it leads to hazardous seafaring conditions and is also a choice hunting ground for both the local population and large predators. Using observations and climate simulations, this study shows that, especially in the Canadian Arctic, landfast ice might be more resilient to climate change than is generally thought.
Ice that forms over marginal seas often gets anchored and becomes landfast. Landfast ice is...
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