Global internal tide solution based on a simultaneous inversion of both mesoscale and internal tide using altimeter measurements available between 01/1993 and 06/2017. The four (M2, S2, K1, O1) internal tide elevations are available for download, distributed on 1/10° grids (amplitude and phase). A simple prediction algorithm is also distributed within the MIOST-IT package to compute the internal tide height at any location of the world ocean. Notice that diurnal tides are filled with zeros...