Ridging, strength, and stability in high-resolution sea ice models

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The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities (2015, background): “6, the amount of ice that rafts/ridges depends on the strain rate tensor invariants (shear and divergence) as in Flato and Hibler (1995), while the ice categories involved are determined by a participation function favouring thin ice (Lipscomb et al., 2007).”
The DOE E3SM Coupled Model Version 1: Overview and Evaluation at Standard Resolution (2019, background): “…(2015), the level ice melt pond scheme of Hunke et al. (2013), a delta-Eddington shortwave (SW) radiation scheme (Briegleb & Light, 2007; Holland et al., 2012), a scheme for transport in thickness space (Lipscomb, 2001), and a representation of mechanical redistribution (Lipscomb et al., 2007).”
The Flexible Global Ocean‐Atmosphere‐Land System Model Grid‐Point Version 3 (FGOALS‐g3): Description and Evaluation (2020, methodology): “For the dynamic component, the elastic‐viscous‐plastic rheology (Hunke & Dukowicz, 1997), mechanical redistribution scheme (Lipscomb et al., 2007), and incremental remapping advection scheme (Lipscomb & Hunke, 2004) are used.”