Richard H. Rapp
30 works on record
Works
Global gravity field and its temporal variations
The earth's gravity field to degree and order 180 using Seasat altimeter data, terrestrial gravity data, and other data
1981
Potential coefficient and anomaly degree variance modelling revisited
1979
Determination of the geoid
Advances in geodesy
Satellite perturbations due to zonal gravitational harmonics
The prediction of point and mean gravity anomalies through the use of a digital computer
Accuracy of the determination of mean anomalies and mean geoid undulations from a satellite gravity field mapping mission
Methods for the computation of detailed geoids and their accuracy
Detailed gravity anomalies and sea surface heights derived from GEOS-3/SEASAT altimeter data
A Fortran program for the computation of gravimetric quantities from high degree spherical harmonic expansions
Improvement of the earth's gravity field from terrestrial and satellite data
A global atlas of sea surface heights based on the adjusted Seasat altimeter data
Statistical analysis of gravity anomalies and elevations by long profiles and by areas / by Richard H. Rapp
Altimeter and gravity data analysis
The development of a degree 360 expansion of the dynamic ocean topography of the POCM4̲B global circulation model
Global anomaly and undulation recovery using GEOS-3 altimeter data
Ellipsoidal corrections for geoid undulation computations
A global 1℗ʻx1℗ʻ anomaly field combining satellite, GEOS03 altimeter and terrestrial anomaly data
A summary of the results from the OSU analysis of Seasat altimeter data
Spherical harmonic expansions of the Earth's gravitational potential todegree 360 using 30' mean anomalies
Artifacts introduced in the point evaluation of functions expanded into a degree 360 spherical harmonic series
Comparison of potential coefficient determinations with 5℗ʻ and 1℗ʻ anomalies
Statistical analysis of gravity anomalies and elevations by longprofiles and by areas
The use of gravity anomalies on a bounding sphere to improve portential coefficient determinations
Geometric geodesy
The determination of high degree potential coefficient expansions from the combination of satellite and terrestrialgravity information
Mean gravity anomalies and sea surface heights derived from GEOS-3 altimeter data
The Ohio state 1991 geopotential and sea surface topography harmonic coefficient models
The representation of the Earth's gravitational potential in a spherical harmonic expansion to degree 250