Tide -- from Eric Weisstein's World of Physics

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Tide

The difference in heights between the pole and equator can be found by expanding the potential from the Moon about the center of mass of the Earth. Define the coordinate system centered on Earth. Let the positive z-axis lie along the Earth-Moon line, and the x- and y-axes lie in the plane perpendicular to the moon-Earth line. The potential from the moon is then

(1)

Define , then

The first term is constant, so it contributes no force. The second term produces a constant attractive force in the direction, so it is not tidal. The lowest higher order term is the quadrupole, which is this term responsible for tides.

(2)
(3)
(4)

The total potential will be the tidal potential plus that of the Earth Eric Weisstein's World of Astronomy,
(5)
(6)
(7)

The total potential at and will be equal when
(8)

(9)

(10)

which agrees with the exact result.

Tidal Acceleration, Tidal Heating, Tidal Torque




References

Stacey, F. D. Physics of the Earth, 2nd ed. New York: Wiley, 1977.



© 1996-2007 Eric W. Weisstein

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