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If I take the limit as x-> infinity, by considering only the highest order terms in x (the only way to deal with the very messy expressions), I'm finally getting the same answers for the tidal forces.
I think some comment on the case on the error induced in tidal forces from acceleration is useful - not so much for the moving case, as for it's application to the static case. If one is accelerating at 1g, assuming I've done the numbers right, one will falsely measure a stretching tidal force of about 10^-16 g / meter in the direction of acceleration (an error of 1+gz/c^2).
This measurement is done just by mounting accelerometers on "rigid rods" in the fermi-normal frame of the accelerating observer, and comparing the accelerometer readings. The accelerometer "above" the observer will be slightly low, the one "below" slightly high, hence an apparent stretching force.
So it's not a big issue in practice with reasonable accelerations.
I think some comment on the case on the error induced in tidal forces from acceleration is useful - not so much for the moving case, as for it's application to the static case. If one is accelerating at 1g, assuming I've done the numbers right, one will falsely measure a stretching tidal force of about 10^-16 g / meter in the direction of acceleration (an error of 1+gz/c^2).
This measurement is done just by mounting accelerometers on "rigid rods" in the fermi-normal frame of the accelerating observer, and comparing the accelerometer readings. The accelerometer "above" the observer will be slightly low, the one "below" slightly high, hence an apparent stretching force.
So it's not a big issue in practice with reasonable accelerations.
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