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Volume 10, issue 3
The Cryosphere, 10, 1055–1073, 2016
https://doi.org/10.5194/tc-10-1055-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 1055–1073, 2016
https://doi.org/10.5194/tc-10-1055-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 May 2016

Research article | 20 May 2016

neXtSIM: a new Lagrangian sea ice model

Pierre Rampal et al.
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Amante, C. and Eakins, B. W.: ETOPO1 Global Relief Model converted to PanMap layer format, NOAA – National Geophysical Data Center, https://doi.org/10.1594/PANGAEA.769615, 2009.
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Batchelor, G. K.: Diffusion in a field of homogeneous turbulence, Math. Proc. Cambridge, 48, 345–362, https://doi.org/10.1017/S0305004100027687, 1952.
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The Arctic sea ice cover has changed drastically over the last decades and undergone a shift in its dynamical regime, as seen by the increase of extreme fracturing events and the acceleration of sea ice drift. In this paper we present a new sea ice model, neXtSIM, that is capable of simulating both sea ice drift and deformation as observed from satellites, with similar spatial and temporal scaling properties. At the same time, the model reproduces sea ice area, extent, and volume correctly.
The Arctic sea ice cover has changed drastically over the last decades and undergone a shift in...
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