Simulation of the present-day climate with the climate model INMCM5

By E. Volodin, E. Mortikov, S. Kostrykin, V. Galin, V. N. Lykossov, A. Gritsun, N. Diansky, A. Gusev, N. Iakovlev. Climate Dynamics, 2017

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DeepMIP: model intercomparison of early Eocene climatic optimum (EECO) large-scale climate features and comparison with proxy data (2020, unknown): “The scaled SST anomalies, relative to the zonal mean of the preindustrial SST, for CESM, COSMOS, GFDL, HadCM3, IPSL, and NorESM, along with the proxy SST data from Hollis et al. (2019) (also relative to the zonal mean of the preindustrial), are shown in Figure 5.”
Resolving and Parameterising the Ocean Mesoscale in Earth System Models (2020, methodology): “Two new ocean models with flexible grids have been introduced in CMIP6: FESOM [12] and MPAS [13], and although CMIP6 models generally use quasi-geopotential grids (‘z-coordinates’), one model has terrain-following coordinates (INM-CM5) [14] and two models use Lagrangian hybrid coordinates following ”