How do tides vary over a lunar cycle?

  • Thread starter Hak
  • Start date
In summary, tides vary over a lunar cycle primarily due to the gravitational pull of the moon and sun on Earth's oceans. As the moon orbits the Earth, its position relative to the sun changes, resulting in different tidal patterns. During the new and full moons, when the sun, moon, and Earth align, we experience spring tides, which are higher and lower than average. Conversely, during the first and third quarter phases, when the moon is at a right angle to the sun, neap tides occur, resulting in less extreme tidal fluctuations. This cyclical variation is influenced by the lunar cycle, taking approximately 29.5 days to complete.
  • #36
haruspex said:
I set ##R_1, R_2## to be the distances to the common mass centre. I found the sum of the centrifugal and M2-based gravitational potentials for two points, one at ##y## from the centre of M1, towards M2, and one at 'moonrise', i.e such that the point and M2 subtend an angle of 90° at the centre of M1.
I then took the difference between these two sums and discarded terms order ##y^3## and higher. (Note that a trap with this sort of calculation is taking approximations too soon and ending up with 0.)
I ended up with ##\frac{GM_2y^2(R_2+3R_1)}{2(R_1+R_2)^3R_1}##. See if you get the same.

If this results in a tide height difference of h then that potential difference should equal ##gh##.

I haven't validated it numerically by plugging in the numbers for Earth and Moon.
Thank you, @haruspex! I'll see if I can achieve the same, although it seems difficult. I will post my results even if they are wrong. However, I didn't understand one thing: from these expressions you got, how should you arrive at the answers to 1. and 2.? I didn't understand...
 
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  • #37
Hak said:
Thank you, @haruspex! I'll see if I can achieve the same, although it seems difficult. I will post my results even if they are wrong. However, I didn't understand one thing: from these expressions you got, how should you arrive at the answers to 1. and 2.? I didn't understand...
You already answered 1 in post #1.
For 2., we need to estimate the max tide height due to the moon alone and that due to the sun alone. We can do both of those from the formula in post #35. Then we can see what tide heights we get when they reinforce and when they oppose.

But the first step is to validate that formula numerically for Earth-Moon. I leave that to you.
 
  • #38
haruspex said:
You already answered 1 in post #1.
For 2., we need to estimate the max tide height due to the moon alone and that due to the sun alone. We can do both of those from the formula in post #35. Then we can see what tide heights we get when they reinforce and when they oppose.

But the first step is to validate that formula numerically for Earth-Moon. I leave that to you.

As for the answer to point 1, I thought it was wrong, because you, @jbriggs444 and @kuruman had replied by asking me questions to get me to the correct answer. So, I didn't understand which point the answers to posts #2, #3, #5 and #6 were referring to. Is point #1 therefore correct in light of these replies? I did not understand.

As for point #2, I think I understand. I'll see if I can get the same result as you, then do the numerical verification. Thank you.
 
  • #39
Hak said:
As for the answer to point 1, I thought it was wrong, because you, @jbriggs444 and @kuruman had replied by asking me questions to get me to the correct answer. So, I didn't understand which point the answers to posts #2, #3, #5 and #6 were referring to. Is point #1 therefore correct in light of these replies? I did not understand.

As for point #2, I think I understand. I'll see if I can get the same result as you, then do the numerical verification. Thank you.
The queries in posts #5 and #6 refer to your explanation of the process in post #4. Post #2 referred to your answer to part 2. I don't see any responses that challenged your answer to part in post #1.

Anyway, it was not clear to me whether your explanation in post #4 was just oversimplified or a genuine misconception. The process of answering part 2, with the balance of potentials/forces, should help you to word it better.
 
  • #40
haruspex said:
The queries in posts #5 and #6 refer to your explanation of the process in post #4. Post #2 referred to your answer to part 2. I don't see any responses that challenged your answer to part in post #1.

Anyway, it was not clear to me whether your explanation in post #4 was just oversimplified or a genuine misconception. The process of answering part 2, with the balance of potentials/forces, should help you to word it better.
Thank you for the clarification. My reply to post #4 is not an oversimplification, it should be a genuine misunderstanding. What is excessively wrong with it? Is it all to be thrown away? Could you clarify for me what is right and what is wrong with this post, also in light of the talk of potentials and forces you introduced me to? Thank you very much.
 
  • #41
Hak said:
Thank you for the clarification. My reply to post #4 is not an oversimplification, it should be a genuine misunderstanding. What is excessively wrong with it? Is it all to be thrown away? Could you clarify for me what is right and what is wrong with this post, also in light of the talk of potentials and forces you introduced me to? Thank you very much.
You wrote
the tides are mainly caused by the gravitational attraction of the Moon and the Sun on the Earth’s oceans. … The gravitational force of the Moon and the Sun creates bulges of water on the side of the Earth facing them and on the opposite side
If it were that simple, the high tide would only be on the side facing the sun/moon.

Potentials and forces are just two ways of analysing it. You can use either, but it is easier to conceptualise the result using potentials; the water will always flow towards the lowest potential, so forms an equipotential surface. As discussed, these potentials/ forces have three sources (in the two body case): the two gravitational fields and the rotation.

The challenge is to sum up this up in words. For Earth+Sun we could say "The Earth rotates around the Sun because of Sun's gravity. The water on the side nearest the Sun is both more attracted by that gravity and less 'thrown out' by the rotation. Conversely, that on the far side is less attracted and more thrown out."

For Earth/Moon it is the same, but it becomes necessary to refer to rotation about the common mass centre. We do not normally think of the Earth as orbiting the Moon!
 

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