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31#
發(fā)表于 2025-3-26 21:35:22 | 只看該作者
32#
發(fā)表于 2025-3-27 04:33:10 | 只看該作者
33#
發(fā)表于 2025-3-27 05:36:52 | 只看該作者
34#
發(fā)表于 2025-3-27 10:49:19 | 只看該作者
Die Stellung des Zahlungsverkehrs im Betriebdwide 1° x 1° grid at 26995 grid points located mainly on land. The gravity tide parameters have been derived from gravity tide amplitudes of the Tamura (1987) tidal potential referring to a rigid Earth model, body tide amplitude factors using a model of an ocean-free, elastic, rotating, isotropic a
35#
發(fā)表于 2025-3-27 16:00:37 | 只看該作者
https://doi.org/10.1007/978-3-658-44795-3 satellite Global Positioning System (GPS) and the geoid. The GPS provides only h or Δh. To convert these mathematical ellipsoidal quantities to physically meaningful orthometric H or ΔH, the geoidal undulations N or ΔN must be computed from gravimetric data. To achieve ΔH accuracies which are compa
36#
發(fā)表于 2025-3-27 18:48:23 | 只看該作者
https://doi.org/10.1007/978-3-531-91407-7d mission in order to obtain an important objective: the resolution of the spatial variations of the gravity field to 100 km half wavelenght. Nevertheless, though many concepts were studied (SLALOM, GRAVSAT, GRIM, ARISTOTELES,...), none of the proposed missions has been launched so far and the reali
37#
發(fā)表于 2025-3-28 01:05:50 | 只看該作者
https://doi.org/10.1007/978-94-011-9331-3the beginning of the next century. Although the final mission parameters are not yet fixed, an one-axial gradiometer with an accuracy of 10. E.U. (PAIK et al (1991)) is prefered. This gradiometer is supposed to measure the out-of-plane component .. of the Marussi-tensor in an orbit of 350 km height
38#
發(fā)表于 2025-3-28 04:48:08 | 只看該作者
39#
發(fā)表于 2025-3-28 06:15:26 | 只看該作者
Versicherung und Risikoforschung carried out in close collaboration with the Ordnance Survey of Great Britain (who were simultaneously undertaking a reciprocal heighting traverse) and with the Institute Géographique National (who undertook first order geodetic levelling).
40#
發(fā)表于 2025-3-28 11:36:29 | 只看該作者
https://doi.org/10.1007/978-94-011-9331-3the beginning of the next century. Although the final mission parameters are not yet fixed, an one-axial gradiometer with an accuracy of 10. E.U. (PAIK et al (1991)) is prefered. This gradiometer is supposed to measure the out-of-plane component .. of the Marussi-tensor in an orbit of 350 km height and an orbital plane inclination of 96, 85°.
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