Add to ORKGA determination of the fine scale sea surface topography in the GEOS-3 calibration area using the radar altimeter data is presented. Estimates of the north-south and east-west components of the deflections of the vertical as well as values of the geoidal heights were made. Three major stages of processing were used in obtaining the final results. The first two use pass processors; in the final stage, the processor combines all the pass results to compute the final results. The results obtained compare favorably with gravimetrically determined geoids for this calibration area
GEOS 3 altimeter data in a 5 degree X 5 degree square centered at 30 deg N, 70 deg W were analyzed t...
The Air Force Geophysics Laboratory computer program SARRA (Short Arc Reduction of Radar Altimetry) ...
The purpose of this investigation is to develop methods and procedures are reported for computing a ...
The primary experiment on the Geodynamics Experimental Ocean Satellite-3 (GEOS-3) is the radar altim...
The accuracy with which the local ocean geoid structure could be determined using satellite altimetr...
A number of detailed gravimetric geoids of portions of the world's oceans from marine gravity measur...
From the adjusted altimeter data an approximation to the geoid height in ocean areas is obtained. Me...
A new set of 1 deg x 1 deg mean free air anomalies was used to construct a gravimetric geoid by Stok...
The mean surfaces of several regions of the world's oceans were estimated using GEOS-3 altimeter dat...
Both quasi-stationary and dynamic departures from the marine geoid were successfully detected using ...
A number of GEOS-3 passes over the Atlantic Ocean and Southeastern U.S. are examined. Surface-truth ...
The procedures used to process the GEOS-3 radar altimeter data from raw telemetry data to a final us...
Gravity anomalies have been recovered in the North Atlantic and the Indian Ocean regions. Comparison...
Using statistical analysis, geoidal admittance (the relationship between the ocean geoid and seafloo...
The GEOS-C spacecraft is scheduled to carry onboard a radar altimeter for the purpose of measuring t...
GEOS 3 altimeter data in a 5 degree X 5 degree square centered at 30 deg N, 70 deg W were analyzed t...
The Air Force Geophysics Laboratory computer program SARRA (Short Arc Reduction of Radar Altimetry) ...
The purpose of this investigation is to develop methods and procedures are reported for computing a ...
The primary experiment on the Geodynamics Experimental Ocean Satellite-3 (GEOS-3) is the radar altim...
The accuracy with which the local ocean geoid structure could be determined using satellite altimetr...
A number of detailed gravimetric geoids of portions of the world's oceans from marine gravity measur...
From the adjusted altimeter data an approximation to the geoid height in ocean areas is obtained. Me...
A new set of 1 deg x 1 deg mean free air anomalies was used to construct a gravimetric geoid by Stok...
The mean surfaces of several regions of the world's oceans were estimated using GEOS-3 altimeter dat...
Both quasi-stationary and dynamic departures from the marine geoid were successfully detected using ...
A number of GEOS-3 passes over the Atlantic Ocean and Southeastern U.S. are examined. Surface-truth ...
The procedures used to process the GEOS-3 radar altimeter data from raw telemetry data to a final us...
Gravity anomalies have been recovered in the North Atlantic and the Indian Ocean regions. Comparison...
Using statistical analysis, geoidal admittance (the relationship between the ocean geoid and seafloo...
The GEOS-C spacecraft is scheduled to carry onboard a radar altimeter for the purpose of measuring t...
GEOS 3 altimeter data in a 5 degree X 5 degree square centered at 30 deg N, 70 deg W were analyzed t...
The Air Force Geophysics Laboratory computer program SARRA (Short Arc Reduction of Radar Altimetry) ...
The purpose of this investigation is to develop methods and procedures are reported for computing a ...