Abstract:To cite this version:Mehdi Eshagh. Least-squares modification of extended Stokes' formula and its second-order radial derivative for validation of satellite gravity gradiometry data. Journal of Geodynamics, Elsevier, 2010, 49 (2) This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in … Show more
“…Sprlak and Novak (2014a) used the deflections of vertical for generating the gravity gradients at satellite level, also Sprlak and Novak (2014b) found integral relations between the GOCE and GRACE types of data which can be used for validation purpose of their data. The stochastic modification was used by Eshagh (2010a) to modify the second-order radial derivative of the extended Stokes formula. He proposed two methods of a) modification prior to derivative and b) derivative prior to modification.…”
Section: C) Validation Of Goce Data By External Sources Of Datamentioning
confidence: 99%
“…The truncation coefficients of the estimators are simply generated by their spectral forms. Eshagh (2010a) showed that because of the inclusion of the parameters 0 n , 1 n and 2 n the series will be convergent due to the elevation of the satellite, but the series should be used to high degrees. He showed that a maximum degree of 5000 should be enough for this purpose.…”
Section: Numerical Investigationsmentioning
confidence: 99%
“…As can be seen, Figure 1 shows this issue for the modified kernels, by comparing them to the original ones, especially for the modified kernels of the VH and HH estimators. This can somehow show that the modification processes have been successful.The system of equations from which the modification parameters are obtained is ill-conditioned for the VH and HH estimators (ESHAGH, 2010a). This is due to inclusion of i k u in the mathematical expressions of the elements of the coefficient matrix of the systems.…”
Section: Behaviours Of Isotropic Parts Of the Modified Kernelsmentioning
The Earth's global gravity field modelling is an important subject in Physical Geodesy. For this purpose different satellite gravimetry missions have been designed and launched. Satellite gravity gradiometry (SGG) is a technique to measure the second-order derivatives of the gravity field. The gravity field and steady state ocean circulation explorer (GOCE) is the first satellite mission which uses this technique and is dedicated to recover Earth's gravity models (EGMs) up to medium wavelengths. The existing terrestrial gravimetric data and EGM scan be used for validation of the GOCE data prior to their use. In this research, the tensor of gravitation in the local north-oriented frame is generated using deterministicallymodified integral estimators involving terrestrial data and EGMs. The paper presents that the SGG data is assessable with an accuracy of 1-2 mE in Fennoscandia using a modified integral estimatorby the Molodensky method. A degree of modification of 100 and an integration cap size of 2.5 o for integrating 55 terrestrial data are proper parameters for the estimator.
“…Sprlak and Novak (2014a) used the deflections of vertical for generating the gravity gradients at satellite level, also Sprlak and Novak (2014b) found integral relations between the GOCE and GRACE types of data which can be used for validation purpose of their data. The stochastic modification was used by Eshagh (2010a) to modify the second-order radial derivative of the extended Stokes formula. He proposed two methods of a) modification prior to derivative and b) derivative prior to modification.…”
Section: C) Validation Of Goce Data By External Sources Of Datamentioning
confidence: 99%
“…The truncation coefficients of the estimators are simply generated by their spectral forms. Eshagh (2010a) showed that because of the inclusion of the parameters 0 n , 1 n and 2 n the series will be convergent due to the elevation of the satellite, but the series should be used to high degrees. He showed that a maximum degree of 5000 should be enough for this purpose.…”
Section: Numerical Investigationsmentioning
confidence: 99%
“…As can be seen, Figure 1 shows this issue for the modified kernels, by comparing them to the original ones, especially for the modified kernels of the VH and HH estimators. This can somehow show that the modification processes have been successful.The system of equations from which the modification parameters are obtained is ill-conditioned for the VH and HH estimators (ESHAGH, 2010a). This is due to inclusion of i k u in the mathematical expressions of the elements of the coefficient matrix of the systems.…”
Section: Behaviours Of Isotropic Parts Of the Modified Kernelsmentioning
The Earth's global gravity field modelling is an important subject in Physical Geodesy. For this purpose different satellite gravimetry missions have been designed and launched. Satellite gravity gradiometry (SGG) is a technique to measure the second-order derivatives of the gravity field. The gravity field and steady state ocean circulation explorer (GOCE) is the first satellite mission which uses this technique and is dedicated to recover Earth's gravity models (EGMs) up to medium wavelengths. The existing terrestrial gravimetric data and EGM scan be used for validation of the GOCE data prior to their use. In this research, the tensor of gravitation in the local north-oriented frame is generated using deterministicallymodified integral estimators involving terrestrial data and EGMs. The paper presents that the SGG data is assessable with an accuracy of 1-2 mE in Fennoscandia using a modified integral estimatorby the Molodensky method. A degree of modification of 100 and an integration cap size of 2.5 o for integrating 55 terrestrial data are proper parameters for the estimator.
“…It is simple because its mathematical formulation is easier than the other gradients, and it is important as it has the most power with respect to the others. Let the following estimator for this gradient at satellite level (Sjö berg, 2003;Eshagh, 2009aEshagh, , 2010a:…”
Section: Sord Of Extended Stokes' Formula and Its Modificationmentioning
“…Visser (2009) tried to estimate the biases and scale factors of the accelerometers used in the GOCE spacecraft by using its precise orbit. The stochastic modification was used by Eshagh (2010a) to modify the second-order radial derivative of the extended Stokes formula. Eshagh (2011a) also modified the second-order radial derivative of the Abel-Poisson formula in a least-squares sense to generate the second-order radial gradient at satellite level using an EGM and geoid model.…”
Different gravitational force models are used for determining the satellites' orbits. The satellite gravity gradiometry (SGG) data contain this gravitational information and the satellite accelerations can be determined from them. In this study, we present that amongst the elements of the gravitational tensor in the local north-oriented frame, all of the elements are suitable for this purpose except Txy. Three integral formulae with the same kernel function are presented for recovering the accelerations from the SGG data. The kernel of these integrals is well-behaving which means that the contribution of the far-zone data is not very significant to their integration results; but this contribution is also dependent on the type of the data being integrated. Our numerical studies show that the standard deviations of the differences between the accelerations recovered from Tzz, Txz and Tyz and those computed by an existing Earth´s gravity model reduce by increasing the cap size of integration. However, their root mean squared errors increase for recovering Ty from Tyz. Larger cap sizes than 5 on is recommended for recovering Tx and Tz but smaller ones for Ty.
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