How does jupiter's moon get so hot?

  • Thread starter ehab_s
  • Start date
  • Tags
    Hot Moon
In summary, the conversation discusses the heating of the moon Io due to tides, and where the energy for this heating comes from. It is explained that the tidal forces from Jupiter and its other large moons contribute to this heating, and while the orbital characteristics of Io may change, the total angular momentum of the Jovian system remains constant. The conversation also touches on the concept of energy conservation and how the Jovian system is not a closed system, therefore energy is not conserved.
  • #1
ehab_s
5
0
This question is really starting to bug me!:bugeye:

Consider for example Io is orbiting Jupiter and the force of the gravity pulling the moon towards the planet vs the momentum pulling in the other direction creates friction in the moon's core.
First of all, this should heat up the moon. But where exactly did the energy come from? Gravity isn't an example of energy, energy can only be 'held' in gravity as a potential energy if a force acts against it.The force against it in this case is the 'centrifugal' force acting on the moon. You'd assume that it is caused by the kinetic energy of the moon, only it seems as if it never runs out even though it obviously heating it? Where does the energy actually come from?

It seemed like a really trivial and simple question at first but the more I thought of it the more it confused me. I have a limited understanding of physics as I have just turned 14 and it's early in the morning. :tongue2:

P.S about 7:53 where I live on a weekend not 3:53 soo yeah.
 
Last edited:
Astronomy news on Phys.org
  • #2
Welcome to PF;
Io is heated primarily through tides - the tidal forces get complicated because there are other large moons present to change things about.
http://www.astro.washington.edu/users/smith/Astro150/Tutorials/TidalHeat/

Note: the time stamp on the posts is the tie at the server - the local time of day does not matter as much as knowing how long ago the post was made.

So I posted this 1745 NZDT - the time stamp reads 0445. (give or take)
You posted at 0753 or 1953 your local time and the time-stamp is 0353
That means I posted the reply an hour and 8 mins after you asked the question.
See?
 
  • #3
Simon Bridge said:
Welcome to PF;
Io is heated primarily through tides - the tidal forces get complicated because there are other large moons present to change things about.
http://www.astro.washington.edu/users/smith/Astro150/Tutorials/TidalHeat/

Note: the time stamp on the posts is the tie at the server - the local time of day does not matter as much as knowing how long ago the post was made.

So I posted this 1745 NZDT - the time stamp reads 0445. (give or take)
You posted at 0753 or 1953 your local time and the time-stamp is 0353
That means I posted the reply an hour and 8 mins after you asked the question.
See?

this explains the mechanism but wouldn't the orbit or orbits of the moons slow down as the energy is turned into heat
 
  • #4
The orbital characteristics of Io about Jupiter are complicated by the orbits of the other large moons.

This article explains how these interactions contribute to the heating of Io and to its orbit's stability:

http://en.wikipedia.org/wiki/Io_(moon)
 
  • #5
pixelpuffin said:
this explains the mechanism but wouldn't the orbit or orbits of the moons slow down as the energy is turned into heat
Sort of. The have gravitational PE and regular KE to exchange for heat. It can't go on forever but it can go on for a very long time - especially considering that Io-Jupiter-Europa-etc are not a closed system.

Of course things can get arbitrarily complicated.
We've got it easy with just the one big moon.
 
  • #6
Another thing to ponder: in the past Earth rotated much faster then it does today (the day was shorter, there were more days in the year). What happened to the rotational energy?

(no, I am not asking you to explain it to me, I want OP to think about it for a moment, as it gives partial answer to his original question)
 
  • #7
I think Borek's question might put the OP on a wrong track, since Earth's rotation was certainly not all slowed by heating. So let me clarify.

The heating siphons energy from the rotation and revolution of the system's components. Tidal forces cause exchange of angular momentum between the interacting bodies, but due to heating it is not a 100% efficient process.

Take Earth-Moon system as it is today for an example that is simpler to analyse than multi-satellite system of Jupiter. Currently, with the Moon tidally locked, and disregarding libration, precession, and slight excentricity of its orbit, the only process still going on is the reduction of Earth's rotation (making days longer) and simultainous raising of the Moon's orbit(so it drifts away). If not for the tidal heating, the total angular momentum would be conserved, and the Moon's increased contribution would match exactly the decreased contribution of Earth. But since there is heating, Earth loses more angular momentum than it imparts to its satellite.

With Jupiter and its moons, it becomes much harder to pinpoint wchich way the angular momenta exchanges go, but you can be sure of one thing: the TOTAL angular momentum of the whole system gets reduced as a result of tidal heating.
 
  • #8
Bandersnatch said:
With Jupiter and its moons, it becomes much harder to pinpoint wchich way the angular momenta exchanges go, but you can be sure of one thing: the TOTAL angular momentum of the whole system gets reduced as a result of tidal heating.
What makes you say that? The total angular momentum of the Jovian system is going to be very close to a conserved quantity. It's the energy of the Jovian system that is not conserved.

The three innermost Galilean moons are slowly migrating outward from Jupiter. This means their angular momentum is increasing, which in turn means Jupiter's rotational angular momentum is decreasing. The total is very close to constant. You'd have to look to interactions between Jupiter and the Sun, and between Jupiter and the other planets to see whether the total angular momentum of the Jovian system is increasing or decreasing.
 
Last edited:
  • #9
D H said:
It's energy that is not conserved.



I guess you mean kinetic :smile:
 
  • #10
I edited my post to say "It's mechanical energy that is not conserved.", but I think I should change it back. Energy is not conserved. The Jovian system is not a closed system. Why should energy be conserved? The heat generated by tidal stresses is eventually radiated away.
 
  • #11
While I understand what you are saying, I strongly disagree with the statement. Energy is conserved - period. Some of the energy is radiated away, so it is not conserved inside of the system, but it doesn't mean it disappeared in general.

I was always taught "Energy is conserved. If you miss some energy, it wasn't lost - it is just somewhere else, or in some other form." And I have a feeling every other approach is pedagogically either wrong or at least dangerous - as it suggests energy conservation is something that sometimes works, sometimes not. Say

D H said:
Energy is not conserved.

and then try to convince an over unity crackpot he can't be right, as energy is conserved.
 
  • #12
i tried to make a program for the duration of the cycle but it gives me all sorts of errors because the numbers are too long :/
 
  • #13
just fixed my program using the difference in escape velocity from the surface to their orbit to calculate that the system would last a bit over 2 billion years on it's own at it's current rate
exact info is in the text file
this is assuming a scenario in which all the major moons contribute all of their energy
 

Attachments

  • majormoons.txt
    1.3 KB · Views: 603
  • #14
@Borek - this was my take on it too ... it is pedagogically dangerous. The way the "elastic collisions" topic gets taught is bad enough but at east they say it's kinetic energy that isn't conserved.

The observation that the Jovian system, considered alone, is not closed is valid, but still tricky pedagogically for the same sorts of reasons: it's too easy for the student to miss the proviso. Anyway - how "non-closed" is it?

@pixelpuffin: you mean 2 billion years from now - assuming the system changes at a constant rate?
That constant rate over 2by is a big ask though... is the rate expected to accelerate or decelerate over time? (i.e. do the influences on the rate get bigger or smaller?)
 
  • #15
i would expect the process to go exponentially faster as they get closer to Jupiter however the 2 billion years doesn't account for that it also assumes a system where all the moons contribute
that answer is the longest it could potentially go given it taps all of the energy from the moons around it that it can
i would expect based on my math that it lasts 400,000,000 to 500,000,000
 
  • #16
Simon Bridge said:
The observation that the Jovian system, considered alone, is not closed is valid, but still tricky pedagogically for the same sorts of reasons: it's too easy for the student to miss the proviso. Anyway - how "non-closed" is it?
I disagree. Tidal migration necessitates that the total energy (thermal + kinetic + potential) of a planet and its moons not be a conserved quantity. There can be no tidal migration unless some mechanism by which the system loses energy exists. How does it lose energy? Simple: Mechanical energy is converted to heat by some mechanically lossy mechanism, and that generated heat is eventually radiated into space. The universe makes for a very, very large and very, very cold heat sink to which lots of energy can be transferred.

In the case of Io, the mechanism by which mechanical energy is converted to heat is the viscoelastic-plastic nature of semi-molten rock. Io's orbit is somewhat eccentric. This eccentricity means Io is subject to significant tidal stresses. Coupled with the nature of the material that forms Io, those tidal stresses result in heat. If Jupiter had no other moons, these tidal stresses and the resultant heat generation would act to circularize Io's orbit. Jupiter does have other moons. The three innermost moons, Io, Europa, and Ganymede, are locked in a 1:2:4 orbital resonance. Europa and Ganymede collectively act to increase the eccentricity of Io's orbit. The tidal stresses act to decrease Io's eccentricity. The end result is that Io's orbit is slightly eccentric, and that all three of those innermost Galilean moons are *slowly* migrating outward. Eventually they'll move far enough out that Io, Europa, Ganymede, and Callisto will be in a 1:2:4:8 orbital resonance. That won't happen for a long, long time.
 
  • #17
pixelpuffin said:
i would expect the process to go exponentially faster as they get closer to Jupiter however the 2 billion years doesn't account for that it also assumes a system where all the moons contribute
that answer is the longest it could potentially go given it taps all of the energy from the moons around it that it can
i would expect based on my math that it lasts 400,000,000 to 500,000,000
That's just wrong. Look at it this way: The Galilean moons have been in existence for over 4.5 billion years.

With regard to your calculations, where's the Q and k2 Love numbers of Jupiter and the Galilean moons?
 
  • #18
Thanks for all the interesting replies! I wasn't really expecting this kind of response (maybe it's because I'm used to yahoo and the likes..)

Anyway, an answer to what someone said

What makes you say that? The total angular momentum of the Jovian system is going to be very close to a conserved quantity. It's the energy of the Jovian system that is not conserved.

Correct me if I'm wrong but I thought that the total angular momentum of Jupiter's system would be lost if the total energy is lost. e.g. if our moon was moving away from the Earth, my assumption would be that rather than the moon's angular momentum increasing and Earth's decreasing, both of them were decreasing however it was mostly the Earth's rotational angular momentum decreasing because of the energy lost through tides. Otherwise energy wouldn't be conserved in the system, it would have to be created.

What is really confusing to me is that if Io's orbit is eccentric, it must have to be losing its kinetic energy at a quicker rate than the other moons around jupiter. So why is it moving away from Jupiter, surely the planet couldn't be losing angular momentum faster than Io (After all, Jupiter is massive compared to it)?
 
Last edited:
  • #19
D H said:
That's just wrong. Look at it this way: The Galilean moons have been in existence for over 4.5 billion years.

With regard to your calculations, where's the Q and k2 Love numbers of Jupiter and the Galilean moons?

that is what my math suggests will be the end of the system from the current date so they could have been much further from Jupiter longer ago
for such a length of time they would have to be about 7 times further than they currently are assuming a continuing exponential increase in the rate at which they affect each other
 
  • #20
pixelpuffin said:
I would expect the process to go exponentially faster as they get closer to Jupiter...
... [the Jovian sattelites] could have been much further from Jupiter longer ago...
You are imagining that the Jovian moons are getting closer to Jupiter over time then?
ehab_s said:
Correct me if I'm wrong but I thought that the total angular momentum of Jupiter's system would be lost if the total [mechanical] energy is lost.
I think you need to be careful about what energy, where it comes from, and where it goes.

How does energy leave a gravitationally bound system again?
How big is this effect?

So why is it moving away from Jupiter, surely the planet couldn't be losing angular momentum faster than Io (After all, Jupiter is massive compared to it)?
The relative masses have nothing to do with the change in angular momentum.

The Jovian system is very complicated - but basically Io moves away for the same reason the Moon moves away from the Earth. The elliptical orbit is because Io gets a periodic kick from the other moons to keep it like that. Without that, the orbit would settle towards a circle with slowly increasing radius.

The fun part would if the closest approach was inside a certain limit...
 
  • #21
ehab_s said:
Correct me if I'm wrong but I thought that the total angular momentum of Jupiter's system would be lost if the total energy is lost.
That is indeed wrong. Someone posted words to that effect earlier, but D H cleared that up-- energy and angular momentum are two quite different things, and are changed in a non-closed system in different ways. Energy is changed by heat loss or work done, angular momentum is changed by external torques. It turns out the latter is actually more difficult to accomplish, so in the Jupiter-plus-moons system, angular momentum is a better conserved quantity than energy. (To deflect the objections to that language raised above, one could say more precisely, "the Jupiter-plus-moons systems acts much more like a closed system in regard to its angular momentum than in regard to its energy." The "better conserved" language D H used is a standard way to say that in fewer words, though keep the full statement in the back of your mind.)
What is really confusing to me is that if Io's orbit is eccentric, it must have to be losing its kinetic energy at a quicker rate than the other moons around jupiter. So why is it moving away from Jupiter, surely the planet couldn't be losing angular momentum faster than Io (After all, Jupiter is massive compared to it)?
This question shows you have some misconceptions that are causing you to pose it (which is what is so great about posing questions). An eccentric orbit is not an example of an orbit losing energy, it is an example of an orbit that has some energy sloshing periodically back and forth between kinetic energy (the energy of motion, seen in the speed of the planet) and gravitational potential energy (as calculated from the changing distance to the gravity source). Energy loss from the system (say, by radiated heat from the warmed planet) manifests differently, in a slowing down of the spin and a change in the orbit. As our Moon spirals away from Earth, the Moon itself is actually rising in energy, but the Earth's spin is losing even more kinetic energy than that, because the whole system has to be losing energy in the form of radiated heat. The total angular momentum of Earth spin, plus Moon spin, plus orbital motion of both, is holding fairly constant. What is mostly happening there is the Earth spin angular momentum is being converted, one for one, into Moon orbital angular momentum. Jupiter and Io is a more complicated subsystem, because of those two other Galilean moons that maintain resonances, and Callisto to boot. Hence I imagine that Jupiter is losing spin angular momentum, as all the Galilean moons increase in orbital angular momentum. That probably means most of Jupiter's lost spin angular momentum ends up in Ganymede's orbital angular momentum as the resonances move out, though it may have some effect on Callisto too, I don't know.
 
  • #22
An eccentric orbit is not an example of an orbit losing energy, it is an example of an orbit that has some energy sloshing periodically back and forth between kinetic energy (the energy of motion, seen in the speed of the planet) and gravitational potential energy (as calculated from the changing distance to the gravity source)

I get that energy in this case is sloshing back and forth from KE to GPE, but then where does the heat in Io's core come from? I assumed that there is force acting on Io which caused a tidal effect on the moon's core, creating friction and heat. So it looks at first glance as if the energy comes from the constant pulling from the angular momentum of the moon. Where else would the energy come from?? Although I was wrong about the fact that an eccentric orbit loses energy faster, (the orbit converts the same amount of energy through the tidal effect whether it's eccentric or circular, only less spread out when eccentric) I still can't get my head around this angular momentum being conserved while energy being lost even when it looks as if this energy is coming from the angular momentum in the first place thing. It can't simply be shifted around in a 'closed' system if it is heating the planet and the moon by causing tides. There have to be countering forces in order to create friction in the moon's core, the only thing I can think of is angular momentum and gravity. Either there is something else I'm missing or I fail to understand what 'angular momentum' actually is..
 
  • #23
ehab_s said:
I still can't get my head around this angular momentum being conserved while energy being lost

Momentum and energy are separate things, conserved separately - period.

Do you know what the ballistic pendulum is? It is a perfect example of how to use the fact that these things are conserved separately to determine the velocity of the bullet, regardless of the fact kinetic energy is converted entirely to heat.
 
  • #24
ehab_s said:
I get that energy in this case is sloshing back and forth from KE to GPE, but then where does the heat in Io's core come from?
It comes from inelastic changes in the shape of Io, where parts of Io essentially "rub together" as they reconform to the new shape.
I assumed that there is force acting on Io which caused a tidal effect on the moon's core, creating friction and heat.
Tidal stresses by themselves don't heat anything, they just give the moon a characteristic (tiny) football shape. It is changes in that shape that cause heating-- constant pulling doesn't heat.
So it looks at first glance as if the energy comes from the constant pulling from the angular momentum of the moon. Where else would the energy come from?? Although I was wrong about the fact that an eccentric orbit loses energy faster, (the orbit converts the same amount of energy through the tidal effect whether it's eccentric or circular, only less spread out when eccentric) I still can't get my head around this angular momentum being conserved while energy being lost even when it looks as if this energy is coming from the angular momentum in the first place thing.
Actually, you were right that an eccentric orbit creates heat and a circular one does not, because the eccentric orbit changes the tidal stresses so changes the shape of the moon. My point is only that it is not the steady component of the force that does this, all that does is cause energy to slosh back and forth between KE and GPE as the orbital distance varies. It is a higher order effect that does the heating, the change in the tidal stresses that cause a change in the shape. An analogy often used is "kneading dough".
 
  • #25
ehab_s said:
I get that energy in this case is sloshing back and forth from KE to GPE, but then where does the heat in Io's core come from? I assumed that there is force acting on Io which caused a tidal effect on the moon's core, creating friction and heat. So it looks at first glance as if the energy comes from the constant pulling from the angular momentum of the moon. Where else would the energy come from??
From gravity. Jupiter's gravity is (approximately) a 1/r2 force. This variation, or gradient, in the gravitational force is what causes the ocean tides on Earth and the heating on Io. Jupiter's gravity pulls on a rock on the near side of Io more than it pulls on a similar rock at Io's center of mass, and it pulls on that rock at Io's center of mass more than it pulls on a rock on the far side of Io. Jupiter "wants" to pull Io apart. Io fights this pulling apart with its own gravity, but not completely. Io is stretched from the ends / squeezed at the middle into a slightly out-of-round shape.

While gravitation is a 1/r2 force, the tidal forces that result from the gradient in gravitational force is a 1/r3 force. The amount by which Io is stretched and squeezed out of round varies because Io's orbit is not circular. Io flexes. Think of what happens when you repeatedly bend and unbend a wire coat hanger. It heats up and eventually gets hot enough to cause the hanger to break. That's what's happening to Io. The flexing between a non-spherical and not quite so non-spherical shape as Io moves from perijove to apojove and back again causes Io to heat up a bit.

So far this sounds like a way to create an over-unity machine. It isn't. Suppose Jupiter didn't have any other moons. What would happen, at least immediately, is that this stretching and squeezing would act to circularize Io's orbit at the perijove distance. Angular momentum is (nearly) conserved, but energy can be dissipated throughout the universe.

One way to restate the second law of thermodynamics is that dissipative systems tend toward a minimum energy configuration. The minimum energy configuration for an orbiting body with constant angular momentum is a circular orbit. Jupiter would eventually circularize Io's orbit, and then the stretching and squeezing would stop. Io would be frozen into a fixed slightly out-of-round shape as it orbits Jupiter and rotates at the same rate as the orbital rate.

There's another, longer term effect. Jupiter rotates rather quickly, much faster than Io's orbital rate. Just as Jupiter causes distortions in Io's shape, Io causes distortions in Jupiter's shape. This slight distortion in Jupiter's shape would be frozen in if Jupiter rotated at the same rate as Io's orbital rate. Since Jupiter rotates much faster than Io orbits Jupiter, Jupiter's rotation pulls the slight bulge caused by Io ahead of Io due to frictional forces. This leading bulge gives a little gravitational kick to Io. Io moves out. At the same time, Jupiter's rotation rate slows down just a bit. The total angular momentum of the Jupiter + Io system is conserved, but energy is not. It decreases. Those frictional forces are dissipative. Friction converts kinetic energy into thermal energy, and that thermal energy eventually radiates away into the universe.

So what would happen to Io if it was an isolated moon in a slightly eccentric orbit? Initially its orbital energy would decrease so that the eccentricity goes to zero. Then it would very slowly climb to an ever higher orbit as Jupiter's rotation rate slowly slows down.

Io isn't an isolated moon. The next two innermost moons are in a 1:2:4 orbital resonance with Io. This makes the picture a lot more complicated, but the basic principles still apply. Those moons are gradually moving away from Jupiter as they steal a tiny bit of oJupiter's rotational angular momentum.
 
  • Like
Likes 1 person
  • #26
Ken G said:
It comes from inelastic changes in the shape of Io, where parts of Io essentially "rub together" as they reconform to the new shape.Tidal stresses by themselves don't heat anything, they just give the moon a characteristic (tiny) football shape. It is changes in that shape that cause heating-- constant pulling doesn't heat.
Actually, you were right that an eccentric orbit creates heat and a circular one does not, because the eccentric orbit changes the tidal stresses so changes the shape of the moon. My point is only that it is not the steady component of the force that does this, all that does is cause energy to slosh back and forth between KE and GPE as the orbital distance varies. It is a higher order effect that does the heating, the change in the tidal stresses that cause a change in the shape. An analogy often used is "kneading dough".

I know really, I just didn't mention that clearly :rolleyes:
 
  • #27
D H said:
From gravity. Jupiter's gravity is (approximately) a 1/r2 force. This variation, or gradient, in the gravitational force is what causes the ocean tides on Earth and the heating on Io. Jupiter's gravity pulls on a rock on the near side of Io more than it pulls on a similar rock at Io's center of mass, and it pulls on that rock at Io's center of mass more than it pulls on a rock on the far side of Io. Jupiter "wants" to pull Io apart. Io fights this pulling apart with its own gravity, but not completely. Io is stretched from the ends / squeezed at the middle into a slightly out-of-round shape.

While gravitation is a 1/r2 force, the tidal forces that result from the gradient in gravitational force is a 1/r3 force. The amount by which Io is stretched and squeezed out of round varies because Io's orbit is not circular. Io flexes. Think of what happens when you repeatedly bend and unbend a wire coat hanger. It heats up and eventually gets hot enough to cause the hanger to break. That's what's happening to Io. The flexing between a non-spherical and not quite so non-spherical shape as Io moves from perijove to apojove and back again causes Io to heat up a bit.


So far this sounds like a way to create an over-unity machine. It isn't. Suppose Jupiter didn't have any other moons. What would happen, at least immediately, is that this stretching and squeezing would act to circularize Io's orbit at the perijove distance. Angular momentum is (nearly) conserved, but energy can be dissipated throughout the universe.

One way to restate the second law of thermodynamics is that dissipative systems tend toward a minimum energy configuration. The minimum energy configuration for an orbiting body with constant angular momentum is a circular orbit. Jupiter would eventually circularize Io's orbit, and then the stretching and squeezing would stop. Io would be frozen into a fixed slightly out-of-round shape as it orbits Jupiter and rotates at the same rate as the orbital rate.

There's another, longer term effect. Jupiter rotates rather quickly, much faster than Io's orbital rate. Just as Jupiter causes distortions in Io's shape, Io causes distortions in Jupiter's shape. This slight distortion in Jupiter's shape would be frozen in if Jupiter rotated at the same rate as Io's orbital rate. Since Jupiter rotates much faster than Io orbits Jupiter, Jupiter's rotation pulls the slight bulge caused by Io ahead of Io due to frictional forces. This leading bulge gives a little gravitational kick to Io. Io moves out. At the same time, Jupiter's rotation rate slows down just a bit. The total angular momentum of the Jupiter + Io system is conserved, but energy is not. It decreases. Those frictional forces are dissipative. Friction converts kinetic energy into thermal energy, and that thermal energy eventually radiates away into the universe.

So what would happen to Io if it was an isolated moon in a slightly eccentric orbit? Initially its orbital energy would decrease so that the eccentricity goes to zero. Then it would very slowly climb to an ever higher orbit as Jupiter's rotation rate slowly slows down.

Io isn't an isolated moon. The next two innermost moons are in a 1:2:4 orbital resonance with Io. This makes the picture a lot more complicated, but the basic principles still apply. Those moons are gradually moving away from Jupiter as they steal a tiny bit of oJupiter's rotational angular momentum.


Phew, great explanation thanks!
 

1. How does Jupiter's moon Ganymede get so hot?

Ganymede, like most moons, gets its heat from multiple sources. One of the main sources is tidal heating, caused by the gravitational pull of Jupiter and other nearby moons. This causes Ganymede's core to constantly flex and release heat. Additionally, Ganymede has a thin atmosphere that traps heat and helps to warm the surface.

2. Is Ganymede hotter than other moons in the solar system?

Yes, Ganymede is one of the hottest moons in the solar system. This is due to its size and location, as well as its multiple heat sources. Ganymede is the largest moon in the solar system and its proximity to Jupiter means it experiences stronger tidal forces compared to other moons.

3. Does Ganymede have any other sources of heat besides tidal heating?

Yes, Ganymede also has a small amount of radioactive elements in its core, which contribute to its heat. This heat is leftover from the formation of the moon and continues to slowly dissipate over time.

4. Could Ganymede's heat be caused by the sun?

No, the sun plays a very small role in Ganymede's heat. Since Ganymede is located in the outer solar system, it receives only a fraction of the sun's energy compared to the inner planets. Tidal heating and radioactive decay are the primary sources of heat for Ganymede.

5. Will Ganymede continue to get hotter over time?

No, while Ganymede does have a small amount of radioactive elements in its core, they are not producing enough heat to significantly increase the moon's temperature over time. Tidal heating is also expected to decrease as Ganymede's orbit moves farther away from Jupiter. Therefore, Ganymede's heat will likely remain relatively constant in the future.

Similar threads

  • Astronomy and Astrophysics
Replies
33
Views
3K
  • Astronomy and Astrophysics
Replies
10
Views
2K
  • Astronomy and Astrophysics
Replies
7
Views
2K
  • Astronomy and Astrophysics
Replies
3
Views
1K
  • Special and General Relativity
Replies
6
Views
2K
  • Sci-Fi Writing and World Building
Replies
21
Views
968
  • Astronomy and Astrophysics
Replies
21
Views
1K
Replies
8
Views
5K
  • Other Physics Topics
Replies
8
Views
5K
  • Astronomy and Astrophysics
Replies
13
Views
1K
Back
Top