Q: What causes the rhythmic ebb and flow of the tides?
A: The tides are an effect of gravitation. The moon is the primary cause
as it pulls on the waters of the oceans and holds them in lockstep while
the earth rotates under them. The tidal force is due to the difference in
distance between the moon and the opposite sides of the earth. The pull
of gravity depends on distance and one side of the earth is closer to the
moon than the other side. As a result the water is pulled away from the
earth on one side and the earth is pulled away from the water on the other
side. This results in two small tidal bulges about one foot high which line
up with the moon, one on each side of the earth. As the earth rotates under
them a high tide occurs directly under the bulges on both sides of the earth.
The tides would be very regular and barely noticeable if this was the entire
story, but the moon is not the only thing involved. For one thing, as the
earth rotates it drags the bulges just slightly ahead of the moon causing
the high and low tides to occur before the moon is overhead. Another factor
is the sun. Its tidal force is about half of the moon's so that when the
sun and moon are aligned their pulls add up to cause higher tides and a
greater tidal range. At other times the sun and moon are pulling in different
directions and produce a smaller tidal range. The tidal bulges are also
modified by geography. The ocean basins and the coastline act together to
magnify the slight bulges into tidal ranges as great as fifty feet in some
places and to alter their arrival times at different shores. After being
constricted between Africa and Antarctica, when the tidal bulge is released
into the Atlantic Ocean it spreads northward in long, low ripples like water
sloshing in a flat tray. A similar effect occurs in the Pacific Ocean but
with a different result because of its greater width. Thus, the actual tides
observed at a particular place depend on where it is in the ocean and the
shape of the coastline and adjacent sea floor. The declination of the moon
and sun north or south of equator also has an effect as does the periodically
changing distance between the earth, sun and moon. The astronomical factors
repeat in an eighteen year cycle, and so do the tides.
Richard Brill is assistant professor of science at Honolulu Community
College where he teaches earth and physical science. Send questions to him
at Honolulu Community College, 874 Dillingham Blvd., Honolulu, HI 96817
or email to rickb@hcc.hawaii.edu
The Tides ©1995 Richard C. Brill