The GEM-T2 is the latest in a series of Goddard Earth Models of the terrestrial field. It was designed to bring modeling capabilities one step closer towards ultimately determining the TOPEX/Poseidon satellite's radial position to an accuracy of 10-cm RMS (root mean square). It also improves models of the long wavelength geoid to support many oceanographic and geophysical applications. The GEM-T2 extends the spherical harmonic field to include more than 600 coefficients above degree 36 (which was the limit for its predecessor, GEM-T1). Like GEM-T1, it was produced entirely from satellite tracking data, but it now uses nearly twice as many satellites (31 vs. 17), contains four times the number of observations (2.4 million), has twice the num...
A new medium-wavelength gravity field model has been calculated from 110 days of GRACE tracking data...
Laser data from nine satellites and 12 stations are combined with surface-gravity data to obtain sph...
A new generation of Earth gravity field models called GGM02 are derived using approximately 14 month...
Major new computations of terrestrial gravitational field models were performed by the Geodynamics B...
Improved models of the Earth's gravitational field have been developed from conventional tracking da...
Two models of the earth's gravitational field have been computed at Goddard Space Flight Center. The...
The Japanese Experimental Geodetic Satellite Ajisai was launched on August 12, 1986. In response to ...
Several tests were designed to determine the correct error variances for the GEM-T1 gravitational so...
The use of collocation permitted GEM 9 to be a larger field than previous derived satellite models, ...
The computation is described of a geopotential model to deg 360, a sea surface topography model to d...
An improved model for the Earth's gravity field, TEG-1, was determined using data sets from fourteen...
Contour maps are presented of the global geoid. Free air gravity anomalies of the GEM-4 earth gravit...
A refinement was obtained in the earth's gravitational field using satellite and surface data. In ad...
A new technique was developed for the weighting of data from satellite tracking systems in order to ...
A new technique has been developed for the weighting of data from satellite tracking systems in orde...
A new medium-wavelength gravity field model has been calculated from 110 days of GRACE tracking data...
Laser data from nine satellites and 12 stations are combined with surface-gravity data to obtain sph...
A new generation of Earth gravity field models called GGM02 are derived using approximately 14 month...
Major new computations of terrestrial gravitational field models were performed by the Geodynamics B...
Improved models of the Earth's gravitational field have been developed from conventional tracking da...
Two models of the earth's gravitational field have been computed at Goddard Space Flight Center. The...
The Japanese Experimental Geodetic Satellite Ajisai was launched on August 12, 1986. In response to ...
Several tests were designed to determine the correct error variances for the GEM-T1 gravitational so...
The use of collocation permitted GEM 9 to be a larger field than previous derived satellite models, ...
The computation is described of a geopotential model to deg 360, a sea surface topography model to d...
An improved model for the Earth's gravity field, TEG-1, was determined using data sets from fourteen...
Contour maps are presented of the global geoid. Free air gravity anomalies of the GEM-4 earth gravit...
A refinement was obtained in the earth's gravitational field using satellite and surface data. In ad...
A new technique was developed for the weighting of data from satellite tracking systems in order to ...
A new technique has been developed for the weighting of data from satellite tracking systems in orde...
A new medium-wavelength gravity field model has been calculated from 110 days of GRACE tracking data...
Laser data from nine satellites and 12 stations are combined with surface-gravity data to obtain sph...
A new generation of Earth gravity field models called GGM02 are derived using approximately 14 month...