Does Tidal Friction Affect the Moon's Gravitational Potential Energy?

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Discussion Overview

The discussion revolves around the effects of tidal friction on the Moon's gravitational potential energy and its relationship with the Earth's rotation. Participants explore the mechanisms of tidal locking, angular momentum transfer, and energy loss due to tidal friction, with a focus on theoretical implications and calculations related to these phenomena.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant questions how the Moon can acquire greater potential energy while the Earth loses angular momentum, suggesting that the energy must come from somewhere.
  • Another participant notes that tidal locking causes some of the Earth's angular momentum to be transferred to the Moon's orbital momentum, leading to a slowing of the Earth's rotation and an increase in the Moon's distance from Earth.
  • It is proposed that tidal friction is the mechanism by which rotational energy is transferred from the Earth to the Moon, but the source of energy for this process is debated.
  • Some participants argue that tidal friction is not the only force at play, with tidal locking also contributing but to a lesser extent.
  • There is speculation about the role of gravitational anomalies, such as mountain ranges, in affecting the Moon's distance and the Earth's rotation, though some participants express skepticism about their significance compared to tidal effects.
  • A detailed calculation is presented regarding the energy lost from Earth's rotation daily, estimating significant energy loss and its conversion primarily to heat, with only a small fraction transferring to the Moon.

Areas of Agreement / Disagreement

Participants express various viewpoints on the mechanisms of tidal friction and tidal locking, with no clear consensus on the exact contributions of each factor or the implications for energy transfer. The discussion remains unresolved regarding the specific sources of energy and the significance of gravitational anomalies.

Contextual Notes

Some calculations presented depend on assumptions about the Earth's moment of inertia and the relationship between the length of the day and energy loss, which may not be universally accepted or agreed upon by all participants.

Andrew Mason
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I am a little puzzled by the following:

The moon in causing Earth tides causes the Earth to generate heat loss due to friction and slows down the Earth rotation. This decreases the angular momentum of the earth. The angular momentum of the Earth and moon system combined cannot change. So the moon and Earth have to increase their angular momentum. It is said that they do this by increasing their radii of rotation about the earth-moon centre of mass: the Earth and moon have to move farther apart.

I don't see how that can happen. Since the moon acquires greater potential energy, this compensation for loss of angular momentum takes energy. Where is the energy supposed to come from?

Would the Earth not simply develop more of a wobble to provide the needed angular momentum?

AM
 
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Due to tidal locking, some of the Earth's angular momentum is gradually being transferred to the Moon's orbital momentum, which causes a slowing of the Earth's rotation [days lengthen ~15 µs per year] and an increase in the Moon's distance from Earth [~38 mm per year]. Note: most of the slowing of the Earth's rotation is caused by tidal friction in the oceans, not tidal locking by the Moon.
 
Chronos said:
Due to tidal locking, some of the Earth's angular momentum is gradually being transferred to the Moon's orbital momentum, which causes a slowing of the Earth's rotation [days lengthen ~15 µs per year] and an increase in the Moon's distance from Earth [~38 mm per year]. Note: most of the slowing of the Earth's rotation is caused by tidal friction in the oceans, not tidal locking by the Moon.
But the problem is: It has to do WORK to move farther away. Where does the energy come from?

AM
 
From the angular momentum of the Earth. Earth slows its rotation, Moon increases it's distance from Earth.
 
Chronos said:
From the angular momentum of the Earth. Earth slows its rotation, Moon increases it's distance from Earth.
Ok. That makes sense. But, in that case, the explanation for the Earth slowing down cannot be that it is due only to the energy loss from tidal friction. Perhaps this is one of those interactions analogous to an inelastic collision: momentum is conserved, some energy is lost and some is transferred.

AM
 
It might be a more helpfull description to say that tidal friction is the mechanism by which energy (rotational energy) is transferred from the Earth to the Moon (in the form of gaining altitude).
 
Correct, tidal friction is not the only force in play. Tidal locking, a form of torque is also in play, but has a much smaller effect compared to tidal friction.
 


Chronos said:
Correct, tidal friction is not the only force in play. Tidal locking, a form of torque is also in play, but has a much smaller effect compared to tidal friction.

Would tidal locking arise from gravitational anomalies such as a mountain range pulling on the moon, effectually slowing Earth's rotation while adding that angular momentum to the moon rotation around the earth?

I am wondering generally how much energy is lost from Earth's rotation daily, assuming 2 millisecond spin down over 100 years.
 


shomas said:
Would tidal locking arise from gravitational anomalies such as a mountain range pulling on the moon, effectually slowing Earth's rotation while adding that angular momentum to the moon rotation around the earth?

It arises mostly from the ocean, with some also from "tides" in regular rock. I am not sure how significant gravitational anomalies might be... not as much as tides.

I am wondering generally how much energy is lost from Earth's rotation daily, assuming 2 millisecond spin down over 100 years.

Earth's moment of inertia J is about 8 x 1037 kg m2.

The energy is 0.5 J ω2, where ω is the rotational velocity in radians/sec.

The rotational velocity is 2 pi / P, where P is the period (seconds in a day).

So energy is E = 2 pi2 J P-2 = 1.58 x 1039 P-2.

The CHANGE in energy with the length of the day is dE/dP = -3.16 x 1039 P-3. The minus sign means a longer day corresponds to less energy.

So, if the change in the length of the day is 0.002 (2 milliseconds), then the energy change is dE = -3.16 x 1039 P-3 dP = 1022 Joules, approximately. That's over 100 years, so the energy lost per day is about 2.7 x 1017 J. That works out to about 3.1 TeraWatts. Most of this energy goes into heat, with only a small fraction actually transferring to the Moon as it takes up the loss in angular momentum.

Cheers -- sylas

PS. Very old thread... but good question to revive it.
 
  • #10


shomas said:
Would tidal locking arise from gravitational anomalies such as a mountain range pulling on the moon, effectually slowing Earth's rotation while adding that angular momentum to the moon rotation around the earth?

Earth's mascons and mountains cannot have much to do with it. Consider: the reason that we can accelerate the moon is because the Earth is rotating at a higher frequency than the revolution of the moon: 1/24hours vs 1/28days. Now, the leading parts of the planet drag the moon forward, whereas the training parts retard it. However, a mountain or Petronas tower leads and trails roughly equally long each day, so their effects pretty nearly cancel out. Therefore the moon isn't really receding.
I blame it all on global warming.

Mind you, some other spin doctor seems to have the idea that tidal forces on our sloppy planet (not just the watery bits, lawyers and other slush, but the solid bits like politicians and statues of general Haig) form bulges under the attraction of Luna (Hah! and you thought that only money attracted them? Their schemes aren't called lunatic for nothing!) But says the spin doctor, the bulge stays a bit ahead of the moon because, once lifted, it cannot simply reside immediately, because of inertia and viscosity and stuff (not to mention global warming!) so its attraction is systematically forrard of the moon, speeding it up.

And a good job too, because if it were the other way round, we would by now be spinning like crazy and ducking every time the moon passed overhead a few times a day.

You reckon that couldn't happen? Hm? Think what would happen if either the Earth or moon moved retrograde. But not both? Hm?

Couldn't both!

Global warming say I!

Jon
 

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