The orbit of the 1967-92A satellite was studied to ascertain the extent to which tidal forces contribute to orbital perturbations. Parameters describing the ocean tide potential-in particular for the M2 and S2 constituents-were estimated. Since the ocean tide potential is less well known than the solid Earth tide, the ocean tide parameter estimation is based upon the use of a value of 0.3 for the solid Earth tide Love number in the orbit determination procedure. These tidal parameter values are in good agreement with those appearing in numerical models of the M2 and S2 tides derived from surface data
A theory is presented which predicts tides in turbulent, self-gravitating, and loading oceans posses...
The nature of the orbit error and its effect on the sea surface heights calculated with satellite al...
Maps and tables for the global ocean tides, 69 degree N to 68 degree S, derived from two years of Ge...
The luni-solar tidal perturbations in the inclination of the GEOS-I and GEOS-II satellite orbits wer...
Effective tidal Love numbers and phase angles for the O sub one, K sub one, M sub two, K sub two, P ...
An analysis of the orbital inclination of the Beacon Explorer C spacecraft over a period of nearly f...
Semi-analytic perturbation equations for the influence of M2 and K1 ocean tidal constituents on sate...
Some geophysical aspects of the tidal perturbations in the motion of artificial satellites are inves...
A theory is presented that points out the existence of several long period and 'cross effects' in th...
Seventeen months of laser tracking of the Beacon Explorer C spacecraft by a Goddard Space Flight Cen...
Trigonometrical expansion for calculation of tidal effects on motion of artificial satellite
One hundred sets of mean elements of GEOS-3 computed at 2-day intervals yielded observation equation...
International audienceThe orbits of two geodetic satellites, Starlette and Stella, have been analyse...
The magnitude of the tidal effects depends upon the elastic properties of the earth as described by ...
The method of expansion of the satellite's perturbations, as caused by the oceanic tides, into Fouri...
A theory is presented which predicts tides in turbulent, self-gravitating, and loading oceans posses...
The nature of the orbit error and its effect on the sea surface heights calculated with satellite al...
Maps and tables for the global ocean tides, 69 degree N to 68 degree S, derived from two years of Ge...
The luni-solar tidal perturbations in the inclination of the GEOS-I and GEOS-II satellite orbits wer...
Effective tidal Love numbers and phase angles for the O sub one, K sub one, M sub two, K sub two, P ...
An analysis of the orbital inclination of the Beacon Explorer C spacecraft over a period of nearly f...
Semi-analytic perturbation equations for the influence of M2 and K1 ocean tidal constituents on sate...
Some geophysical aspects of the tidal perturbations in the motion of artificial satellites are inves...
A theory is presented that points out the existence of several long period and 'cross effects' in th...
Seventeen months of laser tracking of the Beacon Explorer C spacecraft by a Goddard Space Flight Cen...
Trigonometrical expansion for calculation of tidal effects on motion of artificial satellite
One hundred sets of mean elements of GEOS-3 computed at 2-day intervals yielded observation equation...
International audienceThe orbits of two geodetic satellites, Starlette and Stella, have been analyse...
The magnitude of the tidal effects depends upon the elastic properties of the earth as described by ...
The method of expansion of the satellite's perturbations, as caused by the oceanic tides, into Fouri...
A theory is presented which predicts tides in turbulent, self-gravitating, and loading oceans posses...
The nature of the orbit error and its effect on the sea surface heights calculated with satellite al...
Maps and tables for the global ocean tides, 69 degree N to 68 degree S, derived from two years of Ge...