Maps and tables for the global ocean tides, 69 degree N to 68 degree S, derived from two years of Geosat altimetry are presented. Global maps of local and Greenwich admittance of the (altimetric) ocean tide, and maps of amplitude and Greenwich phase lag of the ocean tide are shown for M(sub 2), S(sub 2), N(sub 2), O(sub 1), and K(sub 1). Larger scale maps of amplitude and phases are also shown for regional areas of special interest. Spherical harmonic coefficients of the ocean tide through degree and order 8 are tabulated for the six major constituents
Satellite altimetry and gravimetry are used to determine the mean seasonal cycle in relative sea lev...
Two trends evident in global tidal modelling since the first GEOP conference in 1972 are described. ...
The recently upgraded barotropic tidal model TiME is employed to study the influence of fundamental ...
The 1977 altimetry data bank is analyzed for the geometrical shape of the sea surface expressed as s...
A high-degree spherical harmonic series is used to compute the radial deformation of the Earth by oc...
The gravitational influence of the Moon and Sun have a well-known influence on the Earth’s ocean lev...
This study is a part of the on-going effort aimed at improved determinations of the earth\u27s gravi...
Direct estimation of the absolute dynamic topography from satellite altimetry has been confined to t...
Effective tidal Love numbers and phase angles for the O sub one, K sub one, M sub two, K sub two, P ...
The luni-solar tidal perturbations in the inclination of the GEOS-I and GEOS-II satellite orbits wer...
The computation is described of a geopotential model to deg 360, a sea surface topography model to d...
Previous studies have demonstrated that tides are subject to considerable changes on secular time sc...
The nature of the orbit error and its effect on the sea surface heights calculated with satellite al...
copyrighted by American Geophysical UnionOver 20 global ocean tide models have been developed since ...
A new empirical model of ocean tides has been developed for the Weddell Sea, south of 668S, between ...
Satellite altimetry and gravimetry are used to determine the mean seasonal cycle in relative sea lev...
Two trends evident in global tidal modelling since the first GEOP conference in 1972 are described. ...
The recently upgraded barotropic tidal model TiME is employed to study the influence of fundamental ...
The 1977 altimetry data bank is analyzed for the geometrical shape of the sea surface expressed as s...
A high-degree spherical harmonic series is used to compute the radial deformation of the Earth by oc...
The gravitational influence of the Moon and Sun have a well-known influence on the Earth’s ocean lev...
This study is a part of the on-going effort aimed at improved determinations of the earth\u27s gravi...
Direct estimation of the absolute dynamic topography from satellite altimetry has been confined to t...
Effective tidal Love numbers and phase angles for the O sub one, K sub one, M sub two, K sub two, P ...
The luni-solar tidal perturbations in the inclination of the GEOS-I and GEOS-II satellite orbits wer...
The computation is described of a geopotential model to deg 360, a sea surface topography model to d...
Previous studies have demonstrated that tides are subject to considerable changes on secular time sc...
The nature of the orbit error and its effect on the sea surface heights calculated with satellite al...
copyrighted by American Geophysical UnionOver 20 global ocean tide models have been developed since ...
A new empirical model of ocean tides has been developed for the Weddell Sea, south of 668S, between ...
Satellite altimetry and gravimetry are used to determine the mean seasonal cycle in relative sea lev...
Two trends evident in global tidal modelling since the first GEOP conference in 1972 are described. ...
The recently upgraded barotropic tidal model TiME is employed to study the influence of fundamental ...