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We present a new coupled ocean-circulation–ice model  configuration of the Baltic Sea. The model features, contrary to  most existing configurations, a high horizontal resolution of  ≈ 1 nautical mile (≈ 1.85 km), which is eddy-resolving over much of the  domain. The vertical discretisation comprises a total of 47 vertical  levels. Results from a 1987 to 1999 hindcast simulation show that  the model's fidelity is competitive. As suggested by a comparison  with sea surface temperatures observed from space, this applies  especially to near-surface processes. Hence, the configuration is  well suited to serve as a nucleus of a fully fledged coupled ocean-circulation–biogeochemical model (which is yet to be  developed). A caveat is that the model fails to reproduce major  inflow events.  We trace this back to spurious vertical circulation  patterns at the sills which may well be endemic to high-resolution  models based on geopotential coordinates. Further, we present  indications that – so far neglected – eddy/wind effects exert  significant control on wind-induced up- and downwelling

MOMBA 1.1 – a high-resolution Baltic Sea configuration of GFDL's Modular Ocean Model