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  • Global models of the gravity field of the Earth that involve terrestrial measurements and GOCE-based gravity field models represent two different sources of information on the gravity field of the Earth. The aim of this paper is to focus on their combination. The problem has an essential tie to potential theory and it is not difficult to realize that by nature it is an overdetermined problem. Therefore, methods typical for the solution of boundary-value problems of potential theory will be applied together with an optimization approach, target function and regularization techniques. The aim also is to demonstrate the effect of the two different data sources on the resulting solution and to show its spectral and space domain interpretation. In particular, the use of gravity field information contained in satellite-only models of the gravity field of the Earth or alternatively in GOCE gradiometric data in common with terrestrial gravity measurements is discussed in the paper. The compatibility of these two different data sources is given a considerable attention. The theoretical background outlined above is applied and compatibility indicators are defined. Subsequently numerical tests confronting data derived from EGM2008 and from the latest release of GOCE-based gravity model are performed. Results of this analysis are summarized and interpreted.
  • Global models of the gravity field of the Earth that involve terrestrial measurements and GOCE-based gravity field models represent two different sources of information on the gravity field of the Earth. The aim of this paper is to focus on their combination. The problem has an essential tie to potential theory and it is not difficult to realize that by nature it is an overdetermined problem. Therefore, methods typical for the solution of boundary-value problems of potential theory will be applied together with an optimization approach, target function and regularization techniques. The aim also is to demonstrate the effect of the two different data sources on the resulting solution and to show its spectral and space domain interpretation. In particular, the use of gravity field information contained in satellite-only models of the gravity field of the Earth or alternatively in GOCE gradiometric data in common with terrestrial gravity measurements is discussed in the paper. The compatibility of these two different data sources is given a considerable attention. The theoretical background outlined above is applied and compatibility indicators are defined. Subsequently numerical tests confronting data derived from EGM2008 and from the latest release of GOCE-based gravity model are performed. Results of this analysis are summarized and interpreted. (en)
Title
  • On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth
  • On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth (en)
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  • On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth
  • On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth (en)
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  • RIV/00025615:_____/12:#0001837!RIV13-MSM-00025615
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  • RIV/00025615:_____/12:#0001837
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  • Modelling of the Earth’s gravity field; geodetic boundary-value problems; overdetermined problems; terrestrial and satellite data; optimization (en)
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  • [A378608236AC]
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  • Vienna
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  • European Geoscience Union
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  • Holota, Petr
  • Nesvadba, Otakar
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