During recent decades, data from space missions have provided strong evidence of deep liquid oceans underneath a thin outer icy crust on several moons of Jupiter 1, 2 , particularly Europa 3, 4 . But these observations have also raised many unanswered questions regarding the oceanic motions generated under the ice, or the mechanisms leading to the geological features observed on Europa 5, 6 . By means of direct numerical simulations of Europa's interior, we show here that Jupiter's magnetic field generates a retrograde oceanic jet at the equator, which may influence the global dynamics of Europa's ocean and contribute to the formation of some of its surface features by applying a unidirectional torque on Europa's ice shell.Whereas both radiogenic and tidal heating 8, 9 produce the energy dissipation necessary to the melting of the ice 10, 11 , motions in the ocean underneath the Jovian moons are believed to be generated through vigorous thermal convection 12 , hydrothermal plumes 13, 14 or double-diffusion convection 15 . Such flows certainly play a dominant role, but may fail at explaining some of the observations if considered alone 9 , strongly suggesting the presence of an additional physical mechanism in these oceans. Because the magnetic dipole axis is tilted by about 10 o with the rotation axis of the gaseous giant, Jupiter's moons also experience a time-varying magnetic field with a rotation rate ω, inducing electrical currents in the oceanic salty water 16 .Here, we argue that as long as the phase lag between the induced field and the Jovian one is non-zero, these induced currents naturally combine with the magnetic field to generate a Lorentz force, leading to a weak magnetohydrodynamic (MHD) process that might play a significant role on the global dynamics of the ocean. We therefore model Europa's interior as a spherical shell (mean radius R = (R i + R E )/2, thickness h = R E − R i ) of salty water (electrical conductivity σ and kinematic viscosity ν) confined between an inner mantle of silicate rocks (radius R i ) and an outer layer (radius R E ) of ice crust (see our Method section for a definition of the control parameters). We specifically model Europa here, but our results should apply equally to subsurface oceans 1