Startseite Technik Validation of a tailored gravity field model for precise quasigeoid modelling over selected sites in Cameroon and South Africa
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Validation of a tailored gravity field model for precise quasigeoid modelling over selected sites in Cameroon and South Africa

  • Patroba Achola Odera ORCID logo EMAIL logo , Ojima Isaac Apeh ORCID logo , Loudi Yap ORCID logo und Matthews Siphiwe Mphuthi ORCID logo
Veröffentlicht/Copyright: 19. Januar 2024
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Abstract

In this study, a tailored gravity-field model is developed to fit and recover local terrestrial gravity data by integrating gravity from global gravity-field models, residual gravity derived from topographic data and observed terrestrial gravity over two study sites in Africa (Cameroon and South Africa). During the modelling phase, two-thirds of the terrestrial gravity data is utilised, reserving the remaining one-third for validation purposes. Additionally, an independent validation is conducted by comparing computed quasigeoid models (derived from tailored gravity data) with height anomalies from GPS/levelling data over the two study sites. The accuracy of the tailored gravity model in reproducing observed gravity data is noteworthy, with a ±8.9 mGal accuracy for the study site in South Africa at 2867 test points and a ±10.4 mGal accuracy for the study site in Cameroon at 637 test points. Comparing height anomalies from GPS/levelling with the SATGQG quasigeoid model (developed from tailored gravity data) and the recent CDSM09A quasigeoid model at 11 GPS/levelling data points reveals comparable accuracies of ±0.10 m and ±0.05 m, for SATGQG and CDSM09A, respectively for the site in South Africa. For the Cameroon site, the differences between height anomalies from GPS/levelling and the CTGQG quasigeoid model (developed from tailored gravity data), along with the recent CGM20 quasigeoid model at 38 GPS/levelling data points, show practically equal accuracies of ±0.15 m for CTGQG and ±0.11 m for CGM20. These findings underscore the potential of tailored gravity-field model in developing accurate quasigeoid models, particularly in regions with limited gravity data coverage. This approach holds promise for gravity recovery and precise geoid modelling in developing countries and regions with insufficient coverage of terrestrial gravity data.


Corresponding author: Patroba Achola Odera, Division of Geomatics, School of Architecture, University of Cape Town, Planning and Geomatics, Private Bag X3, Rondebosch 7701, South Africa, E-mail:

Acknowledgments

We are grateful to the following organisations for directly providing or making relevant data freely available on their websites: South Africa’s National Geo-Spatial Information and National Institute of Cartography of Cameroon (GPS/levelling); South Africa’s Council for Geoscience, Bureau Gravimétrique International and National Institute of Cartography of Cameroon (terrestrial gravity); United States Geological Survey (global digital elevation models). International Centre for Global Gravity Field Models (static gravity-field models).

  1. Research ethics: Not applicable.

  2. Author contributions: The authors have accepted responsibility for the entire content of this manuscript and approved its submission.

  3. Competing interests: The authors state no conflict of interest.

  4. Research funding: None declared.

  5. Data availability: Not applicable.

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Received: 2023-10-27
Accepted: 2023-12-31
Published Online: 2024-01-19
Published in Print: 2024-07-26

© 2024 Walter de Gruyter GmbH, Berlin/Boston

Artikel in diesem Heft

  1. Frontmatter
  2. Original Research Articles
  3. Ionospheric TEC modeling using COSMIC-2 GNSS radio occultation and artificial neural networks over Egypt
  4. Regional GPS orbit determination using code-based pseudorange measurement with residual correction model
  5. Analysis of different combinations of gravity data types in gravimetric geoid determination over Bali
  6. Assessment of satellite images terrestrial surface temperature and WVP using GNSS radio occultation data
  7. GNSS positioning accuracy performance assessments on 1st and 2nd generation SBAS signals in Thailand
  8. Differential synthetic aperture radar (SAR) interferometry for detection land subsidence in Derna City, Libya
  9. Advanced topographic-geodetic surveys and GNSS methodologies in urban planning
  10. Detection of GNSS ionospheric scintillations in multiple directions over a low latitude station
  11. Spatiotemporal postseismic due to the 2018 Lombok earthquake based on insar revealed multi mechanisms with long duration afterslip
  12. Practical implications in the interpolation methods for constructing the regional mean sea surface model in the eastern Mediterranean Sea
  13. Validation of a tailored gravity field model for precise quasigeoid modelling over selected sites in Cameroon and South Africa
  14. Evaluation of ML-based classification algorithms for GNSS signals in ocean environment
  15. Development of a hybrid geoid model using a global gravity field model over Sri Lanka
  16. Implementation of GAGAN augmentation on smart mobile devices and development of a cooperative positioning architecture
  17. On the GPS signal multipath at ASG-EUPOS stations
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