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Tide creation
| Морской словарь |
All surfaces of the earth are pulled toward the moon and sun by gravitational attraction. this has minor effect on solid land masses, but exerts great and obvious influence on the fluid oceans. moon gravity pulls upwards on the water, while the stronger force of earth gravity simultaneously pulls downward. the sun’s gravity also has an impact, but its gravitational force on the earth is less than half that of the moon, making the latter the predominant factor in tide creation. as 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 centrifugal force of the planet’s spin. these two bulges travel around the globe as tidal waves, producing diurnal high tides (two each day). when the sun>earth>moon line is straight (at new moon and full moon) their gravitational pulls combine to produce higher high tides and lower low tides, known as spring tides. 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 range between high and low water, known as neap tides. there is about a seven day interval between springs and neaps. tides also occur at slightly different times from one day to another, due to shifts in the relative orbits of earth, moon, and sun. northern california has two unequal tides each day, while the gulf of mexico experiences only one high and one low tide each day.
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Tide gate, английский
[1] a restricted passage which produces a tide race. [2] a tidal gate.
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A ball-shaped signal hoisted when the depth of water allows a vessel to enter a bar-restricted harbor.
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