Gravitational potential induced by the tidal response of an ocean planet with deformable solid regions in the system of coordinates rotating with the perturber for P_rot = 10 hr and obliquity values ranging between 0° and 90°. Left: maximum amplitude of the tidal potential obtained from the full calculation (FULL). Right: maximum amplitude of the tidal potential obtained with the standard approximation based on the equatorial degree-2 Love number (APPROX). Amplitudes are plotted as functions of longitude, $\widehat{\phi }$ (horizontal axis), and latitude, ${\widehat{\theta }}^{\prime }={90}^{°}-\widehat{\theta }$ (vertical axis). Red areas indicate large amplitudes, and yellow areas small amplitudes. The black dot at $\left({\widehat{\theta }}^{\prime },\widehat{\phi }\right)=\left(0^{°},0^{°}\right)$ designates the sub-satellite point.