U. S. Coast and Geodetic Survey - NASA GEOMAGNETIC data reduction program
Geomagnetic data reduction program, and World Data Center information interchange
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Geomagnetic data reduction program, and World Data Center information interchange
Existing satellite in resonant orbits with earth longitudinal gravity field for future satellite geodesy
Gravity field determination computer program for Standard Earth calculation
External testing of satellite determinations of gravitational field variations, namely accelerations of 24-hr orbits, astrogeodetic geoid and spectrum from autocovariance analysis of gravity
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Station Cartesian coordinates in SAO systems using Geos 1
Geopotential surface measurement of ocean using altimeter data
Data analysis of GEOS 1 tracking network
Results derived from short arc, orbital solution of twelve stations, PAGEOS network
Design analysis of GEOS-C/ATS-F tracking experiment
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SECOR observations, satellite tracking, and range difference study
Gravity field measurement by satellite to satellite Doppler tracking, critical configurations for fundamental range networks, and improvement of triangulation systems
Geocentric coordinate determinations for station locations using optical observations of Pageos balloon satellites
Unified set of tracking, station coordinates on geocentric reference system from GEOS 1 and 2 tracking data
Using laser tracking systems to detect motion of pole of rotation for earth
Investigations of triangulation nets and scaling are reported. Adjustment of the BC-4 worldwide geometric satellite triangulation net is described, along with procedures for correcting type II data and the contents of magnetic tapes containing data from the Pageos network. Computational steps for the further reduction of partially reduced satellite image plate coordinates are outlined. The problem of improving existing triangulation systems by means of satellite super-control points was studied. The SAO-69 geometric solution was scaled with C-band radar data, resulting in SAO and C-band adjustment compatible with one another in the Western Hemisphere. The North America solution NA-6, obtained from GEOS 1 data, was readjusted with new heights as constraints on all 30 optical stations and is referred to as the NA-8 solution.