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Are there cases or conditions in which an object orbiting another one (e.g. a satellite and its planet) does not get tidally locked to it?

For example, in this question, it is mentioned that a large moon orbiting a planet could prevent it getting tidally locked both to its star and its moon? If there are situations where a planet getting tidally locked to its star can be prevented, can this happen in planets with multiple moons?

Nilay Ghosh
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vengaq
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In short, the answer is: no.

On some occasions, the solar torque will overpower the lunar torque, and will synchronise the planet with the star. Be mindful though that, for the star to win, it is NOT sufficient for the peak value of the solar torque to supersede the peak value of the lunar torque. Owing to the frequency-dependence of the planet's $k_2/Q$, the situation is more complex, see this discussion.

On other occasions, even a very massive moon may fail to synchronise the planet's rotation because the moon may leave the reduced Hill sphere (when synchronisation is carried out my a tidally receding moon) or fall through the Roche limit (when the synchronisation is performed by a tidally descending moon).

Michael_1812
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    Nice answer. It also may bear mentioning that tiny moons at distant orbits have enormous times to lock to small planets at the edge of a stellar system. Also, Pluto will never lock to our Sun since it is locked to Charon. – Connor Garcia Jul 24 '23 at 00:31
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    Are we considering Mercury to be tidally locked? It's locked in a 2:3 resonance but it isn't "always one face to the sun" which is what we usually mean by tidal lock. It can't get out of that resonance because while the 1:1 lock would be a lower energy state, it would require adding energy to get out of the current resonance. I don't know if there's any planet/moon systems that have a similar resonance relationship but it's at least theoretically possible. – Darth Pseudonym Jul 24 '23 at 20:24
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    @DarthPseudonym The term "tidal locking" is oftentimes used as a synonym to tidal synchronism ( = 1:1 spin-orbit resonance). In reality, the meaning of tidal locking is broader. It includes other spin-orbit resonances (3:2, in the case of Mercury). – Michael_1812 Jul 24 '23 at 23:00
  • @DarthPseudonym The fact that the energy of rotation in a 3:2 spin-orbit resonance is higher than that in a 1:1 resonance does not warrant that the rotator must eventually leave the higher resonance and despin towards synchronism. The capture of a rotator in one or another spin state is defined by the frequency-dependence of the tidal torque. The torque due to the permanent triaxiality of the body also participates in the process -- but this is a higher level of complexity. For the theory of tidal capture see this work. – Michael_1812 Jul 24 '23 at 23:35
  • @DarthPseudonym You have pointed very rightly that it would require adding energy to get out of a higher spin state. In higher spin states, the tidal bulge is running over the circumference of the body, making tidal heating much more intense than under synchronism. For very close planets, this may result in thermal runaways. This study demonstrates that in these situations overheating leads to a change in rheology, which in its turn enables the body to slip out of the higher spin state, and to evolve towards synchronism. – Michael_1812 Jul 24 '23 at 23:41
  • @Michael_1812 I feel that if Mercury hasn't slipped out of its 3:2 by four billion years in, it probably isn't going to. But more to the point, I was mostly asking if the OP would consider a 3:2 resonance to be a tidal lock or if the question really meant a 1:1 in specific. If they meant 1:1 specifically, then a spin-orbit resonance is another way to reach a long-term stable state without getting to that "forever facing" situation. – Darth Pseudonym Jul 25 '23 at 14:43
  • This answer seems to be about the planet becoming tidally locked to its moon, rather than vice versa. Do I misunderstand? I think the question was asking whether you could have a moon that did eventually keep one face towards the planet. (I'm ignoring the 3:2 resonance possibility as I suspect that's not what was meant either.) – Mark Foskey Jul 25 '23 at 16:48
  • @MarkFoskey This is how I understood the question. (Tidal capture of a moon seems to be a trivia matter.) – Michael_1812 Jul 25 '23 at 18:45
  • @MarkFoskey If the moon keeps one face to the planet, then the moon is locked to the planet, not the other way around. After all, the Earth is still rotating despite the Moon keeping only one face to the planet. – Thomas Jul 25 '23 at 21:38
  • @Thomas I'm sorry, I wasn't clear (and I left out a "not"). The question is asking, "Will all satellites get tidally locked to their planet?" and the answer is saying "No, not all planets will get tidally locked to their satellite." There's a mismatch. – Mark Foskey Jul 26 '23 at 13:11
  • @MarkFoskey I mean, the secret answer there is that there's no true distinction between a planet and a moon. They're just two bodies interacting in space, and anything that happens to a moon will happen to its planet, just slower. In most cases moons are so vastly smaller than their planet that the effects on the planet are negligible, with Earth being a notable exception because our moon is a chonker, but given sufficient time all the same results will apply. – Darth Pseudonym Jul 26 '23 at 20:35
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A moon in an elliptical orbit may come into a tidal resonance with its planet instead of a full tidal lock. Or, a moon may not lock to its planet if it is in resonance with another moon. In addition tidal influences with the spin of the planet or with other moons in the system can cause a moon to be pushed out of the system, tidal acceleration, or pulled into the planet,tidal deceleration, before it ever has a chance to fully lock.

An alternative to tidal locking is orbital resonance, which occurs when celestial bodies exert periodic gravitational influence on each other, with their orbital periods related by a ratio of small integers. This phenomenon can be considered a form of tidal locking. A classic example of orbital resonance is seen in Jupiter's Galilean moons, where the orbital periods of Ganymede, Europa, and Io are in a stable 1:2:4 resonance configuration, effectively countering the planet-moon tidal effects. Callisto will someday also come into resonance.

Another type of resonance is spin-orbit resonance, where the spin periods of moons are multiples of orbit period multiples.

Over extremely long timescales, on the order of hundreds of billions of years, the Sun's gravitational influence on Jupiter (raising a tidal bulge locked onto the Sun) will inevitably lead to energy dissipation through friction, gradually slowing down Jupiter's rotation until it becomes nearly locked to the Sun, completing one rotation in its solar year.

If a planet's spin were already tidally locked to the orbital period of a large moon, the interaction of the Sun's tidal forces and interacting of tidal bulges with winds in the atmosphere over an immensely long timescale would lead to the gradual removal of orbital energy from the moon's orbit. As a consequence, the moon's orbit would slowly decay (while spinning up the planet and maintaining the tidal lock), and it would eventually fall into the planet. It would then be free to start locking to its host star.

As for the moons of Jupiter, due to its rapid rotation, the gravitational drag from the bulges raised on Jupiter will cause the moons to slowly spiral outward, gradually increasing their orbital periods, likely maintaining their orbital period ratios as the periods lengthen. Eventually, they may escape the system altogether. If the moons have not been lost by the time Jupiter becomes nearly locked to the Sun, they will be pulled inward until they are either torn apart or burn up in Jupiter's atmosphere.

This generalizes to any planet with moons orbiting a star.

However, after ONLY 30 billion years or so, the entire solar system will probably have disintegrated from the disturbances of passing stars. See, “The Great Inequality and the Dynamical Disintegration of the Outer Solar System,” Jon K. Zink et al 2020 AJ 160 232.

On the longest time frame, gravity waves emitted by orbiting objects will remove their energy causing them to spiral in; moons into planets, planets into stars, stars into black holes at the center of galaxies, clusters and groups into their own centers.

eshaya
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Yes, at least for a 2-body system, all gravitationally interacting bodies will eventually stop rotating, given enough time. This applies even to perfect spheres. This is because the finite speed of gravity (which is equal to the speed of light c in the theory of Relativity) leads to a retarded interaction, which makes the receding part of the rotating body appear to have a higher density, and the approaching part of the body a lower density as illustrated in the below diagram

retarded density of rotating object

This figure shows the density of an initially (when at rest) uniform distribution when it rotates counter-clockwise with a speed of $0.5 c$ as it appears for an observer on the positive x-axis at x=3. A mass at this point would therefore experience a stronger gravitational attraction to the upper half than the lower half, therefore slowing the rotation down.

The same effect due to the presence of other satellites will be a) much smaller due to their much smaller mass (and thus gravitional force) compared to that of the planet, and b) it will be periodical. So they will only lead to a small wobble around the mean locked position. After all, the Earth's Moon is not perfectly locked either but shows a small periodical wobble due to disturbances by other bodies.

For more details regarding the retardation effect see my paper "Computational Visualization of Retardation Effects on Observed Particle Distributions" published in European Journal of Physics (you can download a full text version here ).

Thomas
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  • but as the other answer and its comments show, there are systems where tidally locking can be avoided @Thomas – vengaq Jul 24 '23 at 23:34
  • @vengaq The other answers did not take the retardation efffect into account I mentioned. This will eventually stop any rotation. and thus lock the satellite and eventually also the planet. Due to their much smaller mass compared to the planet, other satellites could only cause a small periodical wobble around the locked position (similar to the libration of the Moon). – Thomas Jul 25 '23 at 21:44
  • The linked paper has no discussion of any supposed torques from this (alleged) effect or where the angular momentum would go, not to mention the effects of self-gravity. This is not a plausible effect. – Peter Erwin Feb 25 '24 at 21:13
  • @PeterErwin It is nowhere claimed above that the linked paper discusses the torque issue. This is merely a trivial conclusion from the results shown in the paper, namely that, if applied to gravitational interaction, the direction of the net gravitational force is offset from the center of mass of a rotating object even for a perfect sphere, which implies by definition a torque (in the reference frame of the rotating sphere a mass element on the receding side sees the interacting mass at a smaller retarded distance than on the approaching side, which will slow down the rotation). – Thomas Feb 26 '24 at 21:10