EGU21-3284
https://doi.org/10.5194/egusphere-egu21-3284
EGU General Assembly 2021
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

New geoid models computation in the Southeast part of Brazil

Valeria Silva1, Gabriel Guimarães2, Denizar Blitkow1,3, and Ana Cristina Matos3
Valeria Silva et al.
  • 1Universidade de São Paulo, Departamento de Engenharia de Transportes, São Paulo, Brazil (vsilva2@usp.br) (dblitzko@usp.br)
  • 2Universidade Federal de Uberlândia, UFU, Monte Carmelo, MG (gabriel@ufu.br)
  • 3Centro de Estudos de Geodesia, CENEGEO, Sao Paulo, Brazil (acocmatos@gmai.com) (dblitzko@usp.br)

In the last decade, big efforts have been undertaken in terms of gravity surveys in the Southeast part of Brazil. First of all, São Paulo state has gravity data coverage quite completed in terms of 5’ resolution. Second, in the last few years, some field works have been carried out in Minas Gerais state. The purpose of gravity densification is not only to improve the quality of geoid (quasi-geoid) models in Brazil, but also to contribute to the geodetic infrastructure, in particular, at the moment, for the establishment of the International Height Reference Frame, where two of six planned stations are located in the densification area. These efforts resulted in the computation of two quasi-geoid models in the Southeast region of Brazil. The decision is to compute a quasi-geoid instead of a geoid model, once since 2018, the Brazilian vertical system is based on normal heights. The Minas Gerais model was computed using Least Squares Collocation, via Fast Collocation. The spectral decomposition was employed in the technique for quasi-geoid model computation, where the reference field was represented by XGM2019 up to degree and order 200. The model was compared with GNSS/leveling in order to check the consistency of two different data sets. Two quasi-geoidal models for the São Paulo state have been computed. Numerical integration through the Fast Fourier Transform (FFT) was used to perform the integral. The Molodensky gravity anomaly was determined in a 5’ grid, reduced and restored using the Residual Terrain Model (RTM) technique and the XGM2019 with the degree and order 250 and 720. The validation for the São Paulo quasi-geoid model is based on the GNSS measurements in the leveling network too.  The Digital Terrain Model SRTM15 plus was used in the continent and the ocean areas in both states.

How to cite: Silva, V., Guimarães, G., Blitkow, D., and Matos, A. C.: New geoid models computation in the Southeast part of Brazil, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-3284, https://doi.org/10.5194/egusphere-egu21-3284, 2021.

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