Ground tracks from SEASAT were used in an effort to develop qualititative relationships between the gravity field and MAGSAT magnetic anomalies in the eastern Indian Ocean. Investigation of data quality led to analyses of the average value (over 80 vector data points, or approximately 36 km intervals) and of the standard deviation of this average, as a mean of identifying noisy portions of the data. It was discovered that the plots of the average value minus the individual (measured) point value are most useful for identifying noisy areas and data spikes. Spectrum analysis using edited (spikes removed) data show that the noise floor is less than 1 nT and the slope of the spectrum in the region of wavelengths between 1200 km and 250 km is ap...
Magnetic anomalies of lithospheric origin are weak at Magsat altitudes (20 to 30 nT at most), and ar...
Techniques and significant results of an analysis of MAGSAT and surface data of the Indian region ar...
The MAGSAT data were used to produce a scalar anomaly map of the U.S. In order to remove the east-we...
Progress in software development and in preliminary analysis of MAGSAT tracks crossing the Indian Oc...
The quality of the MAGSAT data was assessed, especially the characterization of spikes. The spectral...
MAGSAT Investigator-B tapes were preprocessed by (1) removing all data points with obvious erroneous...
Data tapes were decoded and 24 tracks over the Indian region were reduced to common elevation. Profi...
A higher resolution anomaly map of the Broken Ridge area (2 degree dipole spacing) was produced and ...
Processing continued on the data set covering the first three months of the mission. Orbits were sel...
Crustal magnetic anomalies in a region of the eastern Indian Ocean were studied using data from NASA...
Current limitations in the quantitative interpretation of satellite-elevation geopotential field dat...
Progress in the development and modification of software to accommodate total field anomaly data and...
The analysis and preliminary interpretation of investigator-B MAGSAT data are addressed. The data pr...
The results of modeling satellite-elevation magnetic and gravity data using the constraints imposed ...
Efforts on the analysis of MAGSAT scalar anomaly data, the application of the scalar analysis result...
Magnetic anomalies of lithospheric origin are weak at Magsat altitudes (20 to 30 nT at most), and ar...
Techniques and significant results of an analysis of MAGSAT and surface data of the Indian region ar...
The MAGSAT data were used to produce a scalar anomaly map of the U.S. In order to remove the east-we...
Progress in software development and in preliminary analysis of MAGSAT tracks crossing the Indian Oc...
The quality of the MAGSAT data was assessed, especially the characterization of spikes. The spectral...
MAGSAT Investigator-B tapes were preprocessed by (1) removing all data points with obvious erroneous...
Data tapes were decoded and 24 tracks over the Indian region were reduced to common elevation. Profi...
A higher resolution anomaly map of the Broken Ridge area (2 degree dipole spacing) was produced and ...
Processing continued on the data set covering the first three months of the mission. Orbits were sel...
Crustal magnetic anomalies in a region of the eastern Indian Ocean were studied using data from NASA...
Current limitations in the quantitative interpretation of satellite-elevation geopotential field dat...
Progress in the development and modification of software to accommodate total field anomaly data and...
The analysis and preliminary interpretation of investigator-B MAGSAT data are addressed. The data pr...
The results of modeling satellite-elevation magnetic and gravity data using the constraints imposed ...
Efforts on the analysis of MAGSAT scalar anomaly data, the application of the scalar analysis result...
Magnetic anomalies of lithospheric origin are weak at Magsat altitudes (20 to 30 nT at most), and ar...
Techniques and significant results of an analysis of MAGSAT and surface data of the Indian region ar...
The MAGSAT data were used to produce a scalar anomaly map of the U.S. In order to remove the east-we...