An elastic-viscous-plastic sea ice model formulated on Arakawa B and C grids

By Sylvain Bouillon, M. Maqueda, Vincent Legat, T. Fichefet. 2009

210 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/898b4598873fd2b1994829450bc206e148b21676

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In Atmospheric Science

Citations in the corpus

On the formulation of sea-ice models. Part 1: Effects of different solver implementations and parameterizations (2010, methodology): “As model resolution increases, more and more46 ocean and sea ice models use an Arakawa C grid discretization (e.g., Marshall47 et al., 1997a, Ip et al., 1991, Tremblay and Mysak, 1997, Lemieux et al., 2008,48 Bouillon et al., 2009).”
Evaluation of the CMCC eddy‐permitting global ocean physical reanalysis system (C‐GLORS, 1982–2012) and its assimilation components (2016, methodology): “The rheology used is the Elasto-Visco-Plastic (EVP: Bouillon et al., 2009), solving the momentum equation on the Arakawa C-grid.”
Evaluation of CMIP6 DECK Experiments With CNRM‐CM6‐1 (2019, methodology): “The elastic‐viscous‐plastic sea ice rheology implemented by Bouillon et al. (2009) on an Arakawa C‐grid is used, consistently with the formulation of NEMO finite difference scheme, whereas it was solved on an Arakawa B‐grid in Gelato 5. The sea ice transport follows an incremental remapping scheme b”
The Canadian Earth System Model version 5 (CanESM5.0.3) (2019, methodology): “CanESM5 uses the LIM2 sea-ice model (Fichefet and Morales Maqueda, 1997; Bouillon et al., 2009), which is run within the NEMO framework.”
The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities (2015, methodology): “…including brine dynamics and their impact on thermal properties and ice–ocean salt exchanges (Vancoppenolle et al., 2009b) and a C-grid formulation (Bouillon et al., 2009) for ice dynamics using the modified elasticviscous-plastic (EVP) rheology (Bouillon et al., 2013), instead of the more…”
Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, methodology): “The model is coupled to LIM2, a two-level thermodynamicdynamic sea ice model (Fichefet and Maqueda, 1997; Bouillon et al., 2009) and is relaxed weakly towards a climatology in temperature (3-yr e-folding time).”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, background): “The elastic‐viscous‐plastic rheology is solved on the C‐grid following Bouillon et al. (2009).”
Climate model configurations of the ECMWF Integrated Forecasting System (ECMWF-IFS cycle 43r1) for HighResMIP (2018, methodology): “…version 3.4 of the Nucleus for European Modelling of the Ocean (NEMO), which consists of a hydrostatic, finite-difference, primitive equation general circulation model (Madec, 2008) coupled to version 2 of the Louvain-la-Neuve Sea-Ice Model (LIM2; Bouillon et al., 2009; Fichefet and Maqueda, 1997).”