A global coupled sea ice–ocean model

By D. Mélia. 2002

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Evaluation of CNRM Earth System Model, CNRM‐ESM2‐1: Role of Earth System Processes in Present‐Day and Future Climate (2019, methodology): “…Version 3.6 (Madec et al., 2017) which is coupled to both the Global Experimental Leads and ice for ATmosphere and Ocean (GELATO) sea ice model (Salas Mélia, 2002) Version 6 and also the marine biogeochemical model Pelagic Interaction Scheme for Carbon and Ecosystem Studies version 2‐gas…”
The CNRM-CM5.1 global climate model: description and basic evaluation (2013, unknown): “Table 1 Annual global means of energy budget quantities calculated over 400 years of the pre-industrial control simulations done with CNRM-CM3 and CNRM-CM5.1 and for the 1970–1999 period of the historical simulations compared to observed estimates from Trenberth et al. (2009) in W m (except albedo)”
Evaluation of CMIP6 DECK Experiments With CNRM‐CM6‐1 (2019, methodology): “Depending on sea ice thickness, rafting, and ridging may take place in case of sea ice convergence, as described in Salas Mélia (2002).”
Overview of the Meso-NH model version 5.4 and its applications (2018, methodology): “Sea ice is treated either where sea surface temperature is below −4 C or by the GELATO sea ice model (Mélia, 2002) coupled with a 3-D ocean model.”