“…The hydrodynamical core is based on NEMO general circulation ocean model (version 3.6; Madec et al, 2016), implemented in the BS domain with horizontal resolution of 1/27° x 1/36° and 31 vertical levels. NEMO is forced by atmospheric surface fluxes computed by bulk formulation using ECMWF ERA5 atmospheric fields at the resolution of 0.25° in space and 1-h in time [5,6,9,10,11,12,13,14].…”