Abstract
AbstractIndonesia released a new regional geoid model in 2020—the Indonesian Geoid 2020 (INAGEOID2020). It covers the Indonesian region with a spatial resolution of 0.01 × 0.01 degree with the unit in meters. The model was generated through a series of data and computations. Three components of gravity data, i.e., the observed free-air anomaly, the long-wave from the global geoid model, and the short-wave from the terrain model, were employed. The computation was performed using the Remove-Compute-Restore technique with the Fast Fourier Transformation approach. The output was then fitted to the geoid at tide stations by adding a fitting plane to the geoid model. The fitting plane was constructed based on the difference between the geoid model and each tide gauge benchmark. The final geoid model was evaluated by comparing the model with the reference data. Based on quality metrics, the accuracy of INAGEOID2020 varied between 6 cm to 29 cm. Any interested user can use this gridded geoid model to convert geodetic to orthometric heights and vice versa.
Publisher
Springer Science and Business Media LLC
Reference50 articles.
1. Petr V. Why Do We Need a Proper Geoid? FIG Working Week 2009 - TS3C- GEOID- Modelling (2009).
2. Heiskanen, W. A. & Moritz, H. Physical geodesy. Bulletin Géodésique 41 (1967).
3. Hotine, M. Mathematical Geodesy. (ESSA Monographs, 1969).
4. Hofmann-Wellenhof, B. & Moritz, H. Physical Geodesy. Physical Geodesy https://doi.org/10.1007/b139113 (2005).
5. Vaníček, P., Kingdon, R. & Santos, M. Geoid versus quasigeoid: A case of physics versus geometry. Contributions to Geophysics and Geodesy 42 (2012).