C. Hwang, INVERSE VENING-MEINESZ FORMULA AND DEFLECTION-GEOID FORMULA - APPLICATIONS TO THE PREDICTIONS OF GRAVITY AND GEOID OVER THE SOUTH CHINA SEA, JOURNAL OF GEODESY, 72(5), 1998, pp. 304-312
Using the spherical harmonic representations of the earth's disturbing
potential and its functionals, we derive the inverse Vening Meinesz f
ormula, which converts deflection of the vertical to gravity anomaly u
sing the gradient of the H function. The deflection-geoid formula is a
lso derived that converts deflection to geoidal undulation using the g
radient of the C function. The two formulae are implemented by the 1D
FFT and the 2D FFT methods. The innermost zone effect is derived. The
inverse Vening Meinesz formula is employed to compute gravity anomalie
s and geoidal undulations over the South China Sea using deflections f
rom Seasat, Geosat, ERS-1 and TOPEX//POSEIDON satellite altimetry. The
1D FFT yields the best result of 9.9-mgal rms difference with the shi
pborne gravity anomalies. Using the simulated deflections from EGM96,
the deflection-geoid formula yields a 4-cm rms difference with the EGM
96-generated geoid. The predicted gravity anomalies and geoidal undula
tions can be used to study the tectonic structure and the ocean circul
ations of the South China Sea.