Could a Moon Make Gliese 581 g Habitable?

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Discussion Overview

The discussion revolves around the habitability of Gliese 581 g, particularly considering its potential for having a moon and how that might affect its tidal locking and rotation. Participants explore the implications of tidal forces, the stability of moon orbits, and the conditions necessary for a moon to influence the planet's habitability.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants suggest that Gliese 581 g, being tidally locked, may not be very habitable due to one side being extremely hot and the other extremely cold, with only the margins potentially supporting life.
  • There is speculation about whether a moon could allow Gliese 581 g to rotate like Earth, with some participants expressing uncertainty about the physics of tidal locking.
  • One participant discusses the concept of the Hill sphere and calculates its size, suggesting that a moon would need to be significantly massive to exert a tidal force greater than that of the parent star.
  • Concerns are raised about the stability of a moon's orbit around Gliese 581 g, with a participant noting that a moon could be ejected due to tidal interactions if it does not have a suitable orbit.
  • Some participants mention that a moon would need to have a slower orbital period than the planet's rotation to speed up the planet's rotation, which is unlikely given the conditions of moon formation.
  • There is a discussion about the possibility of capturing a moon, with some suggesting that this could be more feasible if the moon entered a retrograde orbit, although this remains a rare event.

Areas of Agreement / Disagreement

Participants express multiple competing views regarding the habitability of Gliese 581 g and the role of a moon in potentially altering its conditions. The discussion remains unresolved, with no consensus on the feasibility of a moon significantly affecting the planet's rotation or habitability.

Contextual Notes

Limitations include the dependence on assumptions about the mass of Gliese 581 g, the nature of its parent star, and the dynamics of tidal interactions, which are not fully resolved in the discussion.

sderamus
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Gliese 581 g, assuming it's real, is supposedly tidally locked being so close to its parent star. That makes sense. It also means it is probably not a very habitable planet - one side being a burnt desert and the other a frozen wasteland, with only the margins capable of supporting life. Maybe.

But what if it had a moon? Would that "unlock" it and allow it to rotate like the earth? I don't understand the details of the physics of tidally locking well enough to answer it, but intuitively it seems like it ought to.

I was reading that moons around our gas planets don't have moonlets because the gravitational pull of the close giant would disrupt their orbits so much that a moonlet would just get thrown off. Would that be the case with Gliese 581 g? Or is it far enough away from its parent star so that wouldn't happen?

TIA!

sderamus
 
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I think that the effect that causes moons to be unable to have moonlets is actually the same as what causes planets to be tidally locked. Our two innermost planets, Mercury and Venus, are the only planets without moons. While they do rotate very slowly, they are not tidally locked.
 
Algr said:
Mercury and Venus ... are not tidally locked.

Uh, well, you're half right...
 
I'm at least 584/224.65ths right.
 
Algr said:
I'm at least 584/224.65ths right.

Ha ha. That's what I get for staying up past my bedtime. Spent too long with my head in the Gliese system, all rusty in the Sol system. :sheepish:
 
sderamus said:
Gliese 581 g, assuming it's real, is supposedly tidally locked being so close to its parent star. That makes sense. It also means it is probably not a very habitable planet - one side being a burnt desert and the other a frozen wasteland, with only the margins capable of supporting life. Maybe.

But what if it had a moon? Would that "unlock" it and allow it to rotate like the earth? I don't understand the details of the physics of tidally locking well enough to answer it, but intuitively it seems like it ought to.

I was reading that moons around our gas planets don't have moonlets because the gravitational pull of the close giant would disrupt their orbits so much that a moonlet would just get thrown off. Would that be the case with Gliese 581 g? Or is it far enough away from its parent star so that wouldn't happen?

TIA!

sderamus

There are two factors to consider: How large would the Hill sphere for Gliese 581g be, and how would a moon within effect the planet tidally compared to the star?

Taking the high side estimate of the planet's mass, I get a Hill sphere of 524966 km. Fore an orbit to really be considered stable we need an orbit of about 1/3 that or 174930 km (about 0.45 the distance of our moon).

Tidal force is proportional to mass and inversely proportional to the cube of the distance. Gliese 581 g is 0.146 the distance from the Earth to Sun, and Gliese 581 is 0.31 the mass of the Sun, so its tidal force will be 100 times that of the Sun on the Earth.

Our moon orbiting at 174930 km would exert 11 times the tidal force that it does now, and at it present distance exerts about twice the tidal force the sun does, so a Moon orbiting Gliese 581 g at 174930 km would have to be more than 5 times the mass of the Moon in order to dominate the planet tidally. A Moon the same mass as our Moon would have to orbit closer than a distance of 102,299 km to exert more tidal force than the star.

Also, A moon orbiting with a period less than the rotation period of the Planet will slow the planet's rotation, climbing to a higher and slower orbit. Given Gliese 581 g's smaller hill sphere, I'm going to guess that it would eventually eject the moon.

It will only speed the planet's rotation up if it has a slower period or orbiting retrograde.

A moon formed at the same time as the planet is going to start with a longer orbital period than the planet's rotation and will not be retrograde. Our Moon was likely to have been created by a collision, but even that should leave the planet spinning faster.

This leaves us with the possibility of capture. The capture of an object into orbit is actually easier if it enters a retrograde orbit, so at least this is a factor in favor. But still you are left with a fairly rare event; the capture of a body large enough to significantly effect the rotation of the planet.

So while I wouldn't put in the range of impossible, I would consider it highly improbable.
 

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