Investigating the accuracy of gravity field models using satellite laser ranging data

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Authors

Botai, Mihloti Christina
Combrinck, Ludwig

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Geological Society of South Africa

Abstract

Continuous tracking of geodetic satellites using the Satellite Laser Ranging technique has provided unprecedented opportunity in long- to medium-wavelength gravity field modelling. Numerous gravity field models have been derived from such observations and have been made freely available to the science community for research purpose. The accuracy of most of the latest gravity field models in terms of precise orbit determination is currently at cm level. Improvement in the Earth gravity field modelling is anticipated as quantitative and qualitative data (in particular from low earth orbit satellites) become available in the future. Such expectations require that the accuracy and precision of existing gravity field models be assessed. The validation of gravity field models in terms of satellite orbit determination is often based on the difference between the observed and computed range. The resulting range residuals are considered an important index when determining the accuracy of the gravity models and hence the satellite orbits. In this contribution we investigate the general improvement in gravity field modelling over a period of 15 years. The orbit accuracy of twelve gravity field models (both satellite-only and combined models) were assessed by analysing seven months of data from LAGEOS 1 and 2 using HartRAO analysis software. Results show that the gravity field models developed over the years have improved by at least a factor of 2 since 1990, considering improvement in O-C residuals.

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Keywords

Gravity field models accuracy, Satellite laser ranging, Global geopotential models, Dedicated satellite missions, Satellite orbit determination

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Citation

Botai, CM & Combrinck, L 2011, 'Investigating the accuracy of gravity field models using satellite laser ranging data', South African Journal of Geology, vol. 114, no. no. 3-4, pp. 535-540.