
Fourier analysis of ocean tides
Some physics and some trigonometry
The tides are caused by gravitation. But in fact the "tidal force" depends
on the gradient of the gravitational field. Because what creates
the bulge in the Earth's oceans on the side facing the Moon is the fact that
the surface of the Earth is closer to the Moon than the center, and is
therefore attracted more strongly. This also explains the bulge on the opposite
side: there the center is closer than the surface. In general a variable
gravitational field will stretch bodies along its gradient; our ocean tides
are a special case of this effect.
The gravitational force exerted by a body of mass m on one gram of matter
at a distance L centimeters
is
G m
----- dynes,
L2
where G= 6.67x10-8dyne-cm2/g2 is Newton's gravitational constant.
Suppose another gram of matter is one centimeter farther in the same direction.
Then it feels a force
G m
------- dynes.
(L+1)2
The difference between these two forces can be thought of as a force
pulling the two grams apart. To first order approximation this
difference is
-2 G m
------- dynes,
L3
the derivative of the gravitational force with respect to L.
This is the "tidal force" separating two one-gram objects at distances
L and L+1 centimeters respectively.
-
This calculation explains why the Sun (m = 2x1033, L = 1.5x1013, m/L3= 6x10-7) and the Moon
(m = 7.3x1025, L = 3.8x1010, m/L3=13.3x10-7) exert comparable tidal forces at the
surface of the Earth.
This force is very tine, but if one of the grams is at the center of
the earth and one on the surface, so the L values differ by
6x108cm.,
In more detail. At any moment, at any point of the surface of the earth,
the tidal force causing the ocean to bulge up at that point is the upward-pointing
component of the sum of the Moon's and the Sun's contributions. As a function of time
this will depend on
- the time of day,
- the direction and distance of the Moon,
- the direction and distance of the Sun.
On to the next tides page.
Back to the first tides page.
Comments: webmaster@ams.org
© copyright 1999, American Mathematical Society.