Abstract
Synthetic presentation of planetary tide theories in the simple case of a homogeneous primary rotating around an axis orthogonal to the orbital plane of the companion. The considered theories are founded on the dynamical equilibrium figure of the tidally deformed body, assumed as an ellipsoid whose rotation is delayed with respect to the motion of the companion. The orbital and rotational evolutions of the system are derived using standard physical laws. The main theory considered is the creep tide theory, a first-principles hydrodynamical theory where the dynamical tide is assimilated to a low-Reynolds-number flow and determined using a Newtonian creep law. The Darwin theories are also considered and are formally derived from the creep tide theory. The various rheologies used in Darwin theories are discussed, with emphasis on the CTL (constant time lag) and CPL (constant phase lag) theories. One introductory session is devoted to the main classical results on the hydrostatic figures of equilibrium of the celestial bodies (static tide).
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Notes
- 1.
For the exact definition of the words elastic and anelastic, see the online supplement to [14]. One must keep in mind, however, that the involved restoring forces are gravitational, not elastic.
- 2.
The minus sign in the first term means that we are adopting the exact Physics convention: force is equal to minus the gradient of the potential.
- 3.
Auxiliary first-order relations:
$$\displaystyle \begin{aligned} \begin{array}{rcl} a&\displaystyle =&\displaystyle R_e(1+\epsilon_\rho/2) \\ b&\displaystyle =&\displaystyle R_e(1-\epsilon_\rho/2) \\ c&\displaystyle =&\displaystyle R_e(1-\epsilon_z). \end{array} \end{aligned} $$ - 4.
The Cayley functions introduced here correspond to the degree 3 in a∕r—since 𝜖 ρ ∝ (a∕r)3. These functions are equivalent to the Hansen coefficients preferred by other authors and the equivalence is given by \(E^{(n)}_{q,p}=X^{-n,q}_{2-p}\) (see [8]).
- 5.
We have, however, to keep in mind that these “years” are very short. In type 3 tides, “diurnal” is slower than “annual”.
- 6.
Remember that in the considered case, the equations of the relative motion are \(M \ddot {\mathbf {r}} \hspace {1mm} = \hspace {1mm} (1+\frac {M}{m})\mathbf {F}\).
- 7.
This does not mean that a negative mass is being assigned to void spaces; it means just that forces included in the calculation of the equilibrium figure need to be subtracted when the masses creating them are no longer there.
- 8.
We avoided to overcharge this text with asterisks. We will only use them in Sect. 8 to indicate the mean anomaly and the argument of the pericenter of Diana. If the other Lagrange variational equations are used, other elements of Diana also need to be indicated. In that case, it is convenient to use the asterisk for all orbital parameters of Diana, from the beginning, and drop the asterisks only after all derivatives of the disturbing potential are calculated. Note added in proof: The presentation of the creep tide theory becomes much simpler when the new Folonier equations are used. See [28].
- 9.
Remind that we are only considering the orthogonal case in which the rotation axis of the primary is perpendicular to the orbital plane.
- 10.
The reader may pay attention to the opposite signs appearing in the definitions of \({\mathcal {C}}_k\) and \({\mathcal {C}}^{\prime \prime }_k\), which is often a source of mistakes in the transformation of the equations.
- 11.
The results of Sect. 4 are consistent with those obtained with the creep tide theory (or with Darwin’s theory) when all lags are made equal to zero. Indeed, the expressions for \(\dot {a}\), \(\dot {e}\), \(\dot {W}\) of Sects. 8 and 9 are trigonometric series in the arguments \(\sin {}(j\ell +\sigma _k)\) and \(\sin {}(j\ell +\sigma ^{\prime \prime }_k)\), which average to zero when the lags vanish. The vanishing of the torque when the σ k vanish is less obvious. However, the auxiliary expansions given in the Online Supplement to [20], allow one to see that \( \sum _{k\in \mathbb {Z}} E_{2,k} \sin \big (2v-(2-k)\ell \big )=0\), and so that M 2 = 0 when the lags vanish.
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Acknowledgements
This text follows closely the course given at the University of São Paulo in 2017 and it is a pleasure to thank Profs. J.A.S. de Lima and T.A.Michtchenko and Drs. H.A.Folonier and E.Andrade-Ines, for their many comments. Thanks are also due to G.O.Gomes for reading the entire manuscript and for the suggestions improving the clarity. The investigation on the creep tide theory is funded by the National Research Council, CNPq, grant 302742/2015-8, by FAPESP, grants 2014/13407-4, 2016/13750-6 and 2017/10072-0 and by the INCT Inespaço procs. FAPESP 2008/57866-1 and CNPq 574004/2008-4.
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Ferraz-Mello, S. (2019). Planetary Tides: Theories. In: Baù, G., Celletti, A., Galeș, C., Gronchi, G. (eds) Satellite Dynamics and Space Missions. Springer INdAM Series, vol 34. Springer, Cham. https://doi.org/10.1007/978-3-030-20633-8_1
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