We provide here tilt variations due to atmospheric
(ECMWF operational or reanalysis models) and induced oceanic response (Inverted
Barometer or TUGO-m barotropic ocean model), as well as hydrological
(GLDAS/Noah v1, MERRA-land and MERRA2) and non-tidal oceanic (ECCO and ECCO2)
loading for a selection of sites.
Sites can be added upon request.
Figure 1: Location of the sites where tilt variations are computed.
Careful, it is not possible to combine ECCO or ECCO2 and ECMWF+TUGO-m loading estimates, as TUGO-m is forced by both pressure and winds. Classical ocean circulation models (such as ECCO and ECCO2) are forced by winds, heat and fresh water fluxes.