International audienceWe present results of an implementation of the Elastic Viscous Plastic (EVP) sea ice dynamics scheme into the Hadley Centre coupled ocean-atmosphere climate model HadCM3. Although the large-scale simulation of sea ice in HadCM3 is quite good with this model, the lack of a full dynamical model leads to errors in the detailed representation of sea ice and limits our confidence in its future predictions. We find that introducing the EVP scheme results in a worse initial simulation of the sea ice. This paper documents various improvements made to improve the simulation, resulting in a sea ice simulation that is better than the original HadCM3 scheme overall. Importantly, it is more physically based and provides a more soli...
International audienceA new rheological model is developed that builds on an elasto-brittle (EB) fra...
HadGEM1 is a new coupled atmosphere-ocean climate model developed at the Met Office’s Hadley Centre,...
We propose to make the damping time scale, which governs the decay of pseudo-elastic waves in the El...
International audienceWe present results of an implementation of the Elastic Viscous Plastic (EVP) s...
In this paper, we show that one of the most widely used methods to solve the non-linear viscous–plas...
A nonlinear viscous-plastic (VP) rheology proposed by Hibler (1979) has been demonstrated to be the ...
The viscous-plastic (VP) rheology and the Maxwell elasto-brittle (MEB) rheology were compared in a c...
The performance of the sea ice component of two ocean general circulation models (OGCMs) is investig...
Current sea ice models are far from simulating the complex behavior of the Arctic ice pack. When use...
Most dynamic sea ice models for climate type simulations are based on the viscous-plastic (VP) rheol...
The elastic-viscous-plastic (EVP) sea ice rheology has been introduced in the large-scale Louvain-la...
The standard model for sea ice dynamics treats the ice pack as a viscous-plastic material that flows...
new rheology that explicitly accounts for the subcontinuum anisotropy of the sea ice cover is implem...
A rapid increase in the variety, quality, and quantity of observations in polar regions is leading t...
Sea ice dynamics determine the drift and deformation of sea ice. Nonlinear physics, usually expresse...
International audienceA new rheological model is developed that builds on an elasto-brittle (EB) fra...
HadGEM1 is a new coupled atmosphere-ocean climate model developed at the Met Office’s Hadley Centre,...
We propose to make the damping time scale, which governs the decay of pseudo-elastic waves in the El...
International audienceWe present results of an implementation of the Elastic Viscous Plastic (EVP) s...
In this paper, we show that one of the most widely used methods to solve the non-linear viscous–plas...
A nonlinear viscous-plastic (VP) rheology proposed by Hibler (1979) has been demonstrated to be the ...
The viscous-plastic (VP) rheology and the Maxwell elasto-brittle (MEB) rheology were compared in a c...
The performance of the sea ice component of two ocean general circulation models (OGCMs) is investig...
Current sea ice models are far from simulating the complex behavior of the Arctic ice pack. When use...
Most dynamic sea ice models for climate type simulations are based on the viscous-plastic (VP) rheol...
The elastic-viscous-plastic (EVP) sea ice rheology has been introduced in the large-scale Louvain-la...
The standard model for sea ice dynamics treats the ice pack as a viscous-plastic material that flows...
new rheology that explicitly accounts for the subcontinuum anisotropy of the sea ice cover is implem...
A rapid increase in the variety, quality, and quantity of observations in polar regions is leading t...
Sea ice dynamics determine the drift and deformation of sea ice. Nonlinear physics, usually expresse...
International audienceA new rheological model is developed that builds on an elasto-brittle (EB) fra...
HadGEM1 is a new coupled atmosphere-ocean climate model developed at the Met Office’s Hadley Centre,...
We propose to make the damping time scale, which governs the decay of pseudo-elastic waves in the El...