[Physics] Height of tidal bulge: reference needed

tidal-effect

The tides raised by the moon on the Earth's oceans are adequately and universally explained by:

  1. The shape of the equipotential surface whose peaks are at the sublunar point and its antipode.

  2. The sloshing effect of a real ocean, with viscosity, inertia, coastlines and an irregular bottom, as the points mentioned in 1 move across the surface of the Earth and the water tries to keep up.

…although Galileo, of course, described the whole idea of the moon influencing tides as lunacy.

My question is purely about the shape of the equipotential surface in 1 – or equivalently, and more graphically, about the difference in height between high tide and low tide if the Earth were entirely covered by an inertialess ocean with zero viscosity.

Wikipedia says "The theoretical amplitude of oceanic tides caused by the moon is about $54~\mathrm{cm}$" but gives no reference for this figure. Other sources (including this Stack Exchange site) talk about "$60~\mathrm{cm}$" or "just over half a metre" or even "a few feet", also without giving a reference – and without even clearly specifying whether "$60~\mathrm{cm}$" means "from $-60\,\mathrm{cm}$ to $+60\,\mathrm{cm}$" or "from $-30\,\mathrm{cm}$ to $+30\,\mathrm{cm}$".

What I am looking for, therefore, is a source which can be considered authoritative and is not just a referenceless repeating of "what everyone knows".

Best Answer

The value of 0.54 m is derived in the supplement resources "Tidal Distortions" to [1]. This is freely available on this page, and here is the address of the PDF for convenience. The computation of 0.54 m is done just after equation (20) on p. 13.

[1] Hale Bradt , Astrophysics Processes — The Physics of Astronomical Phenomena, Cambridge University Press, 2008