Modeling Sea Ice Transport Using Incremental Remapping

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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.”
Design and implementation of the infrastructure of HadGEM3: the next-generation Met Office climate modelling system (2010, methodology): “The sea ice is advected using the CICE incremental remapping scheme (Lipscomb and Hunke, 2004).”
Ridging, strength, and stability in high-resolution sea ice models (2007, methodology): “The model includes EVP dynamics [Hunke and Dukowicz, 1997, 2002], an incremental remapping advection scheme [Lipscomb and Hunke, 2004], multilayer energy-conserving thermodynamics [Bitz and Lipscomb, 1999], a remapping scheme for ice thickness [Lipscomb, 2001], and the standard ridging scheme of T75”
The DOE E3SM Coupled Model Version 1: Overview and Evaluation at Standard Resolution (2019, methodology): “2092 of ice concentration, volume, and tracers is achieved with an incremental remapping scheme similar to that described in Dukowicz and Baumgardner (2000), Lipscomb and Hunke (2004), and Lipscomb and Ringler (2005) but adapted to MPAS meshes.”