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Volume 5, issue 4
The Cryosphere, 5, 821–829, 2011
https://doi.org/10.5194/tc-5-821-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 5, 821–829, 2011
https://doi.org/10.5194/tc-5-821-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 14 Oct 2011

Research article | 14 Oct 2011

Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline

L. H. Smedsrud et al.
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Cited articles  
Anderson, D., Hodges, K. I., and Hoskins, B. J.: Sensitivity of feature-based analysis methods of storm tracks to the form of background field removal, Mon. Weather Rev., 131, 565–573, 2003.
Björk, G.: The relation between ice deformation, oceanic heat flux, and the ice thickness distribution in the Arctic Ocean, J. Geophys. Res., 102, 18689–18698, 1997.
Boe, J., Hall, A., and Qu, X.: September sea-ice cover in the Arctic Ocean projected to vanish by 2100, Nat. Geosci., 2, 341–343, https://doi.org/10.1038/NGEO467, 2009.
Chang, E. K. M.: Assessing the increasing trend in Northern Hemisphere winter storm track activity using surface ship observations and a statistical storm track model, J. Climate, 20, 5607–5628, https://doi.org/10.1175/2007jcli1596.1, 2007.
Ezraty, R., Girard-Ardhuin, F., and Croiz-Fillon, D.: Sea ice drift in the central Arctic using the 89 GHz brightness temperatures of the Advanced Microwave Scanning Radiometer, http://www.ifremer.fr/cersat, 2010.
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