Half Question/Half-Challenge: Dimensions of of the Earth-Moon System

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Discussion Overview

The discussion revolves around the problem of determining the radius of the Moon using classical astronomical methods, with specific constraints on measurement techniques. Participants explore various theoretical approaches to achieve this goal without relying on traditional triangulation or two-way measurements.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant proposes measuring gravitational lensing of the Moon to determine its mass, followed by using tidal measurements to calculate the distance and radius, but expresses uncertainty about whether this method would yield a mass value or an M/D ratio.
  • Another participant suggests using the parallax method based on the Earth's rotation to measure the Moon's position at different times, while acknowledging the challenge posed by the Moon's movement during that period.
  • A joke answer is provided, suggesting sending an astronaut with a meter stick, highlighting the constraints of the problem humorously.
  • One participant questions how to obtain the Moon's velocity, which is necessary for the parallax method to work effectively.
  • Another participant speculates that the eccentricity of the Moon's orbit could be used to derive its velocity through the Doppler effect, although they admit this is a guess and not fully worked out.

Areas of Agreement / Disagreement

Participants express various ideas and methods, but there is no consensus on a definitive solution or approach to the problem. Multiple competing views and uncertainties remain throughout the discussion.

Contextual Notes

Participants acknowledge limitations in their proposed methods, such as the need for assumptions about the Moon's velocity and the challenges posed by its orbital characteristics. The discussion does not resolve these limitations.

Vorde
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I've been considering this problem for about a year now (whenever I remember about it, that is), and I've come to the conclusion that I can't figure out a way to do what I want to see is possible, and so I've decided to ask it here to see if anyone else can.

The original question I considered was: could a classical astronomer determine the size of the moon to an arbitrary level of accuracy? Since then I've sort of refined the question, and here are my qualifications:

1) The process has to be able to be theoretically done from a single spot on the Earth (so triangulation is allowed, but only one point of the triangle can be on Earth).
2) You are only allowed one-way measurements, so you can throw something at the moon and measure that, or measure something coming from the moon (or somewhere else), but you can't involve the measurements of one object going to and from the moon (including light).
3) An arbitrary amount of accuracy is allowed with imaginary telescopes and the like.
4) You don't know any distance or velocity values for other solar system objects.

With that in mind, the question is: What is the radius of the moon?

My solution is to, using an extremely accurate telescope, measure the gravitational lensing of the moon, thereby getting its mass. Using a tide-measuring system, and knowing the moons mass, you could figure out the acceleration/force you are experiencing from the moon, and thereby figure out the distance to the moon, and then the radius.

However to me this fails on two counts. 1) I'm not positive the gravitational lensing test will produce a value for M instead of an M/D ratio, and 2) It feels like the use of GR goes against the original purpose of the question.

Does anyone have a more elegant solution? Or knowledge that there isn't one?
 
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Vorde said:
I've been considering this problem for about a year now (whenever I remember about it, that is), and I've come to the conclusion that I can't figure out a way to do what I want to see is possible, and so I've decided to ask it here to see if anyone else can.

The original question I considered was: could a classical astronomer determine the size of the moon to an arbitrary level of accuracy? Since then I've sort of refined the question, and here are my qualifications:

1) The process has to be able to be theoretically done from a single spot on the Earth (so triangulation is allowed, but only one point of the triangle can be on Earth).
2) You are only allowed one-way measurements, so you can throw something at the moon and measure that, or measure something coming from the moon (or somewhere else), but you can't involve the measurements of one object going to and from the moon (including light).
3) An arbitrary amount of accuracy is allowed with imaginary telescopes and the like.
4) You don't know any distance or velocity values for other solar system objects.

With that in mind, the question is: What is the radius of the moon?

My solution is to, using an extremely accurate telescope, measure the gravitational lensing of the moon, thereby getting its mass. Using a tide-measuring system, and knowing the moons mass, you could figure out the acceleration/force you are experiencing from the moon, and thereby figure out the distance to the moon, and then the radius.

However to me this fails on two counts. 1) I'm not positive the gravitational lensing test will produce a value for M instead of an M/D ratio, and 2) It feels like the use of GR goes against the original purpose of the question.

Does anyone have a more elegant solution? Or knowledge that there isn't one?

Joke answer: send an astronaut to the moon with a meter stick to measure the distance, and have him beam back a radio signal with the answer. One object went, and a different one came back :)

Serious answer: The closest method that comes to mind is of course to use the parallax method. You've thrown in the monkey wrench of not being able to use triangulation from different points on the Earth, but you could avoid that by using the parallax occurring from the Earth's rotation (for example, measure the angular position on the sky at sunset and then again at sunrise). Unfortunately, the Moon will move through space during that several hour period (though it works better for more distant objects whose proper motions are smaller in that period -- David Gill used this to measure parallaxes from a single spot to high accuracy, for his time anyway). If you're allowed to know the velocity of the moon (and surely one can measure that using classical techniques) then one might be able to account for that proper motion during the interim period, but I haven't given it much thought as to exactly how you would do it.
 
That would work, I think, if you knew the velocity of the moon, but how would that be obtained?
 
Well, the moon's orbit is eccentric. Suppose one could figure out the degree of eccentricity of the orbit using the change in apparent angular size of the moon from perigee to apogee. Then, one could in principle use the Doppler effect to figure out what the non-circular component of the velocity is, and perhaps from there work out what the total velocity must be? Just a guess, I haven't even worked it out to see if this is enough information.
 

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