Abstract
There are different equations to describe relations between different classes of Love–Shida numbers. In this study with the use of the time-varying gravitational potential an integral relation was obtained which connects tidal Love–Shida numbers (h, l, k), load numbers (h′, l′, k′), potential free Love–Shida numbers generated by normal (h″, l″, k″) and horizontal (h‴, l‴, k‴) stresses. The equations obtained in frame of present study is the only one which
-
holds for every type of Love–Shida numbers,
-
describes a relationship not between different, but the same type of Love–Shida numbers,
-
does not follow from the sixth-order differential equation system of motion usually applied to calculate the Love–Shida numbers.
Similar content being viewed by others
References
Alterman, Z., Jarosch, H., & Pekeris, C. L. (1959). Oscillations of the Earth. Proceedings of the Royal Society London A, 252, 80–95.
Calvo, M., Hinderer, J., Rosat, S., Legros, H., Boy, J.-P., Ducarme, B., et al. (2014). Time stability of spring and superconducting gravimeters, through the analysis of very long gravity records. Journal of Geodynamics, 80(2014), 20–33.
Ducarme, B. (2012). Determination of the main lunar waves generated by the third degree tidal potential and validity of the corresponding body tides models. Journal of Geodesy, 86(1), 65–75.
Grafarend, E., Engels, J., & Varga, P. (1997). The spacetime gravitational field of a deformable body. Journal of Geodesy, 72, 11–30.
Jeffreys, H. (1959). The Earth its origin, history and physical constitution. Cambridge: University Press.
Melchior, P. J. (1950). Sur l’influence de la loi de répartition des densités á l’intérieur de la Terre dans les variations Luni-Solaires de lagravité en un point. Geophysica Pura et Applicata, 16(3–4), 105–112.
Meurers, B., Van Camp, M., Francis, O., & Pálinkáš, V. (2016). Temporal variation of tidal parameters in superconducting gravimeter time-series. Geophysical Journal International, 205(1), 284–300.
Molodensky, M. S. (1953). Elastic tides, free nutations and some questions concerning the inner structure of the Earth. Trudi Geofizitseskogo Instituta Akademii Nauk of the USSR, 19(146), 3–42.
Molodensky, S. M. (1977). On the relation between the Love numbers and the load coefficients. Fizika Zemli, 3, 3–7.
Moritz, H. (1990). The figure of the Earth: theoretical geodesy and the Earth’s interior. Karlsruhe: Wichmann.
Saito, M. (1978). Relationship between tidal and load numbers. Journal of Physics of the Earth, 26, 13–16.
Takeuchi, H. (1953). On the Earth tide of the compressible Earth of variable density and elasticity. Transactions American Geophysical Union, 31(5), 651–689.
Van Camp, M., Meurers, B., de Viron, O., & Forbriger, Th. (2016). Optimized strategy for the calibration of superconducting gravimeters at the one per mille level. Journal of Geodesy, 90(1), 91–99.
Acknowledgements
We thank the Guest Editor David Crossley and an anonymous reviewer colleague for their helpful comments. The research described in this paper was completed during research stay of P. Varga (01.03.2016–31.05.2016) supported by the Alexander Humboldt Foundation at the Department of Geodesy and Geoinformatics, Stuttgart University. P. Varga thanks Professor Nico Sneeuw for the excellent research conditions provided by him. Financial support from the Hungarian Scientific Research Found OTKA (Project K125008) is acknowledged.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Varga, P., Grafarend, E. & Engels, J. Relation of Different Type Love–Shida Numbers Determined with the Use of Time-Varying Incremental Gravitational Potential. Pure Appl. Geophys. 175, 1643–1648 (2018). https://doi.org/10.1007/s00024-017-1532-z
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00024-017-1532-z