The gravitational attraction between the
Earth, sun, and moon. It was not until Sir Isaac Newton (who lived from
1642-1727) discovered the law of gravity that the effect of the sun and the
moon on the tides was fully understood. All surfaces of the Earth are pulled
toward the moon and sun. This force has little effect on land masses, but it
does have a very great and obvious effect on the water of the Earth's oceans.
Twice each month the tidal range reaches a maximum and these large tides are
called the spring tides. Halfway through the monthly cycle the range is much
smaller, and these weak tides are called neap tides.
Neap tide: the sun and moon are at right
angles to the EarthAs the moon rotates around the Earth, it pulls the water on
the nearest side of the Earth outward into a bulge. A similar bulge on the
opposite side of the Earth is caused by the water being thrown outward by the
planet's spin. These two bulges travel around the globe, producing two high
tides each day. During time of the new moon and full moon, when the sun and
moon are in a straight line, their gravitational pulls combine and produce
spring tides; at this time the high tides are very high and the low tides are
very low. When sun and moon are at right angles from the Earth, during the
quarter phases of the moon, the gravitational pull on the oceans is less
producing a smaller difference between high and low tide known as a neap tide.
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