References of "Francis, Olivier 50001803"
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See detailPresent State of Absolute Gravity Measurements in Brussels and Comparison with the Superconducting Gravimeter Drift
Francis, Olivier UL; Ducarme, Bernard; De Meyer, F. et al

in Hsu, H. T. (Ed.) Proceedings of the 12th International Symposium on Earth Tides (1995)

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See detailOMP1: an Inverse Model of the Global Ocean Tides
Mazzega, Pierre; Francis, Olivier UL; Bergé, Muriel

in Hsu, H.T. (Ed.) Proceedings of the 12th International Symposium on Earth Tides (1995)

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See detailValidation of ocean tide models by comparison to gravity loading measurements
Francis, Olivier UL

in Marées Terrestres Bulletin d'Informations (1995), 122

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See detailEstimate of the radial orbit error by complex demodulation
Francis, Olivier UL; Berge, M.

in Journal of Geophysical Research. Solid Earth (1993), 98(B9), 16083-16094

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See detailInteractions between Earth and ocean tides
Francis, Olivier UL

in Marées Terrestres Bulletin d'Informations (1992), 112

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See detailIntroduction aux Problèmes Inverses
Francis, Olivier UL

Report (1991)

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See detailSome Results of Heterogeneous Data Inversions for Oceanic Tides
Jourdin, F.; Francis, Olivier UL; Vincent, P. et al

in Journal of Geophysical Research (1991), 96(B12), 20267-20288

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See detailM2 World Ocean Tide from Tide Gauge Measurements
Francis, Olivier UL; Mazzega, P.

in Geophysical Research Letters (1991), 18(6), 1167-1170

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See detailWhat we can learn about ocean tides from tide gauge and gravity loading measurements?
Francis, Olivier UL; Mazzega, P.

in Kakkuri, Juhani (Ed.) Eleventh International Symposium on Earth Tides, Proceedings of the meeting held July 31 - August 5, 1989, in Helsinki, Finland (1991)

The harmonic constants from tide gauge stations and from gravity loading measurements of the ICET (International Center for Earth Tides) data bank are separately inverted to produce M2 cotidal maps on a ... [more ▼]

The harmonic constants from tide gauge stations and from gravity loading measurements of the ICET (International Center for Earth Tides) data bank are separately inverted to produce M2 cotidal maps on a global scale. The optimal interpolation of these data, based on the total inverse theory in L2 norm, makes use of a set of a priori stationary and isotropic covariance functions deduced from a global hydrodynamical model and from its corresponding gravity loading map. The preliminary results presented with formal error estimates are surprisingly good, in particular the M2 maps obtained from the numerous tide gauge data. These results are discussed and further lines of work are drawn. [less ▲]

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See detailM2 World Ocean Tides from Tide Gauge and Gravity Loading Measurements
Francis, Olivier UL; Mazzega, Pierre

in Paquet, Paul; Flick, Johnny; Ducarme, Bernard (Eds.) GPS for Geodesy and (1990)

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See detailGlobal Charts of Ocean Tide Loading Effects
Francis, Olivier UL; Mazzega, P.

in Journal of Geophysical Research (1990), 95(C7), 11411-11424

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See detailOn the accuracy of the Platzman's charting for loading estimations
Francis, Olivier UL

in Marées Terrestres Bulletin d'Informations (1988), (101), 7010-7018

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See detailRecomputation of the Green's functions for tidal loading estimations
Francis, Olivier UL; Dehant, V.

in Marées Terrestres Bulletin d'Informations (1987), (100), 6962-6986

Detailed reference viewed: 172 (27 UL)