Weight Measurement on Mutually Orbiting Planets

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SUMMARY

The discussion centers on the measurement of weight on mutually orbiting planets, specifically addressing the gravitational effects experienced at different points on a planet's surface. It concludes that weight measurements taken on the side of a planet facing another planet will be approximately the same as those taken on the opposite side, assuming negligible diameters compared to their separation. The conversation highlights that tidal gravity, influenced by the proximity of another celestial body, can cause measurable variations, similar to the effects observed on Earth due to the Sun and Moon, which can vary by up to 0.3 milligal, detectable by precision gravimeters.

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So at the end of the lengthy thread https://www.physicsforums.com/showthread.php?t=404650", a similar but new question of mine arose:

If you consider the Earth rotating, you can measure differences in weight at different points on the Earth (namely, the extremes being the poles and the equator.) I am assuming you know why, etc.
Now if you have two mutually orbiting planets, I wanted to verify that if you measured weight at the point on a planet facing the other planet, and compared it with the weight measured at the opposite side of the planet, they should be approximately the same. (Assuming the diameters of the planets are negligible compared to their separation)
Or also, I am verifying that their revolution does not affect this measurement.

P.S.
I am asking this because when I originally posted the above thread, I had in mind that that measurement was not the same, as if it were similar to a merry-go-round, however I recently realized that this shouldn't be so, and before I went on to think about it more I wanted to verify that I'm right.
 
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Tidal gravity is measurable. The difference is greatest not between the zenith and nadir points but between the point at which the other planet is at zenith (or nadir) and a point where the other planet is on the horizon. For example, the tidal gravitational effects due to the Sun and Moon on the surface of the Earth vary by up to 0.3 milligal over time (a gal is 1 cm/s2), a quantity that is easily measurable by precision gravimeters.
 

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