GEOS-3

The satellite mission was designed to further an understanding of the earth's gravitational field, size and shape of the terrestrial geoid, deep ocean tides, sea state, current structure, crustal structure, solid earth dynamics, and remote sensing technology. Jerome Rosenburg at NASA Headquarters initiated the GEOS-3 project in 1970. == Instruments ==

The following is a list of instruments/systems that were on board or part of the GEOS-3 satellite, including a description of their general purpose: • Radar Altimeter (ALT) – A multimode radar system with the ability to provide precise satellite-to-ocean surface height measurements. The radar system provided global and intensive data gathering modes, which could provide height precision measurements at 50 cm and 20 cm respectively. • Retroreflector Array (RRA) – An array of retroreflectors. These allow a ground-based laser to provide range information. • Doppler System – A system of dual frequency space borne doppler beacons at 162 and 324 MHz and a ground-based receiver station. This system was used to measure the effects of first-order ionospheric refraction and make corrections to the Doppler frequency. • S-band Tracking System – A tracking system which had three modes of operations for satellite to satellite tracking, ground-station tracking, and direct unified S-band. • C-band System – A system of two C-band radar transponders used to better understand the accuracies of the gravimetric and geometric measurements. The system also supported the altimeter and C-band calibration. • Satellite-to-Satellite Tracking (SST) – The SST experiment consisted of the ground-based ATS ranging system, the wideband communication transponder on the ATS-6 geosynchronous spacecraft, and the ranging transponder on the GEOS-3 satellite. == Impacts on the scientific community ==

The GEOS-3 mission provided data that furthered scientific understanding in various fields. The ocean height data set from this mission provided the first comprehensive coverage in most areas of the world's oceans, providing a better understanding of the ocean geoid. Ocean height also provided information about quasi-stationary departures from the geoid (the sea surface topography), for events like currents, eddies, storm surges, etc. The return waveform data was used to better understand the sea state at a level that was comparable to buoy-collected data. An unexpected result was the ability to use waveform data to derive surface wind speed, and the ability to maintain track over terrain and ice. Altimeter data from GEOS-3 has been utilized by many Earth's gravity models, including GEM-T3, JGM-1 and JGM-2. == References ==