![]() Data files are on the authenticated FTP into fes2014_elevations_and_load/ and fes2014a_currents/ folders.Use: coastal oceanography, operational oceanography, ocean circulationĭescription: combined product based on a hydrodynamic model which assimilate altimeter data (Topex/ Poseidon, Jason-1, Jason-2, TP interleaved -J1 interleaved, ERS-1, ERS-2, and Envisat). FES2014_load must be used to compute the FES2014 geocentric (elastic) tide as follows: FES2014b geocentric (elastic) tide = FES2014b oceanic tide + FES2014a loading tide. Folder is fes2014_elevations_and_load/fes2014a_loadtide/. Tide loading: the new FES2014a tide loading.No extrapolation is done on the coasts for the currents. Tide currents: tidal curents derived from FES2014a model, directly interpolated from the finite element native grid.Folder is fes2014_elevations_and_load/fes2014b_elevations_extrapolated/ The procedure is a simple extrapolation applied on 10 pixels and using mean values when necessary, it can be not enough accurate in some regions. Extrapolated version: the above version has been extrapolated on the coasts in order to cover nearly entirely the coastal regions.Folder is fes2014_elevations_and_load/fes2014b_elevations/ Non extrapolated version: the model is defined on a 1/16° grid directly interpolated from the finite element native grid of the model.Tide elevations: FES2014b ocean tide model is distributed this model has been computed using the new FES2014 tidal loading grids.Altimetry and Doris applications in videosįES (Finite Element Solution)- Global tideĬontents: The FES2014 tides database includes 3 components: tide elevations (amplitude and phase), tide currents (u and v) and tide loading on a 1/16°x1/16° grid.Shortcut to Mono and multi-mission processing.Information about mono and multi-mission processing.Cycle calendar (past and current missions).
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