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Martin Pitoňák1, Michal Šprlák2 and Pavel Novák1

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Presentation on theme: "Martin Pitoňák1, Michal Šprlák2 and Pavel Novák1"— Presentation transcript:

1 Regional recovery of the disturbing gravitational potential from GOCE observables
Martin Pitoňák1, Michal Šprlák2 and Pavel Novák1 1New Technologies for Information Society, Faculty of Applied Sciences, University of West Bohemia, Plzeň, Czech Republic 2School of Engineering and Built Environment, University of Newcastle, Callaghan, NSW 2308, Australia 10 YEARS OF THE CZECH REPUBLIC IN ESA, November , 2018, Prague

2 Theoretical background, Numerical experiment, Results,
Content: Colaboration with ESA Motivation, Theoretical background, Numerical experiment, Results, Conclusion and discussion Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 1/20

3 Colaboration with ESA (1/4 ):
ESTEC Project /11/NL/FvO/ef „Towards a Better Understanding of the Earth’s Interior and Geophysical Exploration Research – GOCE-GDC“ GOCE+ GeoExplore funded by ESA through the Support To Science Element–STS Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 2/20

4 Colaboration with ESA (2/4):
More information and details on the website Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 3/20

5 Colaboration with ESA (3/4 ):
Please visit the website: Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 4/20

6 Colaboration with ESA (4/4 ): Projects publications
Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 5/20

7 Comparison of two strategies for reduction the far zone effect,
Motivation: The GOCE mission - more than three years of outstanding measurements which resulted into five releases of global gravitational models (GGMs), Comparison of two strategies for reduction the far zone effect, How compare results from downward continuation with EGM2008 and quantify the differences? Can we improve regional gravity field in Europe from EGG data? How various time-span of the EGG data influence accuracy of the final results? Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 6/20

8 Theoretical background (1/2): Integral transformation
The relationship between the disturbing gravitational gradients and the disturbing gravitational potential can be obtained by differentiating the spherical Abel-Poisson integral formula (Šprlák et al., 2015) IRF – Inertial Reference Frame The corresponding integral kernel functions were derived by (ibid.) EFRF – Earth Fixed Reference Frame LNOF – Local North Oriented Frame GRF – Gradiometer Reference Frame The isotropic kernel functions in the previous equations are (ibid.) The nomenclature which was used in the previous equations Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 7/20

9 Theoretical background (2/2): Regularization
Eq. (1) in the vector-matrix form well-known as the Gauss-Markov model for the least-squares estimate of x we can write The system of normal equations (5) represents the discretized Fredholm integral equation of the first kind with the ill-conditioned matrix of normal equations N (its condition number in numerical experiments reached values ≈ 1016). The Tikhonov regularization (Tikhonov 1963a, b) with the estimate of x in the following form was applied In our numerical experiments we applied the general cross-validation (GCV) method (Hansen and O’Fleary, 1993) and L-curve criterion (Miller, 1970) to determine regularization parameter. The bias of the solution can formally be computed from (Xu et al., 2006) Combination of all four well-measured gravitational gradients: Variance Component estimation (Koch and Kusche, 2002) The Tikhonov regularization (Eq. 6) Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 8/20

10 Numerical experiment (1/4): Test area and input data
Input data: GOCE Level 2 EGG_TRF_2 (1 November 2009 to 30 June 2010) ≈ 8 months (≈ values for each gravitational gradient) Solution area: Integration radius: Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 9/20

11 Numerical experiment (2/4): Computation scheme
Strategy I Strategy II Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 10/20

12 Numerical experiment (3/4):
Strategy I: - the truncation error formulas computed according to (Šprlák et al., 2015) up to the degree 150 from the GRACE-based global gravitational model GGM05S (Tapley et al., 2013). Strategy II: Low frequencies of the gravitational field should be removed to reduce the effect of the omitted distant zone data. The long-wavelength effect was generated from the TIM-r4 model (Pail et al., 2011) up to the degree 180 version a: 30 days (November 2009) of the input data, version b: 72 days (1 November 2009 – 11 January 2010) of the input data, version c: 212 days (1 November 2009 – 30 June 2013) of the input data. Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 11/20

13 Numerical experiment (4/4): Test of the results
Spherical harmonic synthesis Spherical harmonic analysis Degree correlation with Rock-Water-Ice topographic-isostatic gravitational model (Grombein et al., 2014) Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 12/20

14 Results (Strategy I): Differences between the values of the disturbing gravitational potential obtained from Txx, Tyy, Tzz and Txz, as well as from their combination using joint inversion and the VCE method (truncation error reduction) from the 212 day data coverage, and from EGM2008 up to the degree 240 (unit 1 m2 s-2) Txx Tyy Tzz Txz Joint inversion VCE RMS 22.346 24.941 8.514 74.641 2.971 3.201 Min Max 4.170 35.139 1.149 5.568 5.000 mean -1.806 -4.859 Differences between values of the disturbing gravitational potential from the selected models and EGM2008 up to the degree 240 (unit 1 m2 s-2) TIM-r2 DIR-r2 SPW-r2 RMS 1.110 1.262 1.485 min -4.959 -3.967 -8.203 max 2.968 3.789 6.432 mean 0.002 -0.014 0.034 Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 13/20

15 Results (Strategy II):
Differences between the values of the disturbing gravitational potential obtained from Txx, Tyy, Tzz and Txz, as well as from their combination using joint inversion and the VCE method (remove-compute-restore scenario) from the 30, 72 and 212 day data coverage, and from EGM2008 up to the degree 240 (unit 1 m2 s-2) 30 days Txx Tyy Tzz Txz Joint inversion VCE RMS 2.055 2.331 2.627 2.626 1.805 1.712 Min -9.054 -8.963 max 8.850 10.583 7.861 8.041 5.123 9.437 mean 0.044 -0.018 0.015 -0.050 0.019 0.014 72 days rms 1.916 2.176 2.041 2.152 1.584 1.497 min -8.947 -9.062 -8.340 8.444 10.651 8.136 7.666 6.529 8.215 0.030 0.027 0.034 -0.052 0.023 212 days 1.789 2.015 1.515 1.719 1.326 1.231 -9.341 -8.739 -8.326 -7.522 7.930 10.769 5.053 5.946 5.166 5.036 0.025 0.021 -0.030 Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 14/20

16 Results (Strategy I): Degree correlation coefficients between selected GOCE-based global gravitational models, EGM2008, selected regional solutions (GOCE gradient data from November June 2010 with truncation error reduction applied) and RWI model. Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 15/20

17 Results (Strategy II version a):
Degree correlation coefficients between selected GOCE-based global gravitational models, EGM2008, selected regional solutions (GOCE data from November 2009 with the remove-compute-restore scenario applied) and RWI model. Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 16/20

18 Results (Strategy II version b):
Degree correlation coefficients between selected GOCE-based global gravitational models, EGM2008, selected regional solutions (GOCE data from 1 November 2009 – 11 January 2010 with the remove-compute-restore scenario applied) and RWI model. Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 17/20

19 Results (Strategy II version c):
Degree correlation coefficients between selected GOCE-based global gravitational models, EGM2008, selected regional solutions (GOCE data from 1 November 2009 – 30 June 2010 with the remove-compute-restore scenario applied) and RWI model Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 18/20

20 Conclusion and discussion:
A method for comparing results from downward continuation with EGM2008 was suggested, Our regional models are comparable with the second release of GOCE-based GGMs, More data improved an accuracy of regional models about 0.5 mGal for combined solutions and more than 1 mGal for Tzz , In the future experiment the reprocessed gravitational gradients in the gradiometric reference frame will be applied. NOTHING TO FEAR FROM REAL GRAVITATIONAL GRADIENTS MEASURED BY GOCE GRADIOMETER Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 19/20

21 Thank you for your attention
Pitoňák et al. Regional recovery of the disturbing gravitational potential from GOCE observables 20/20

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