Lecture 14: Tides

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A set of vocabulary flashcards based on the lecture about tides, covering key terms and theories related to tides and their effects.

Last updated 6:33 PM on 4/16/26
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17 Terms

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Tides

Periodic, short-term changes in the height of the ocean surface caused by the gravitational force of the moon and sun and the motion of Earth.

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Equilibrium Theory of Tides

Explains tides based on the balance and effects of forces that maintain planetary orbits.

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Dynamic Theory of Tides

Accounts for depth, seabed contour, water viscosity, and tide wave inertia to predict tides.

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Inertia

The tendency of moving objects to continue in a straight line, which keeps them apart from gravitational forces.

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Lunar Tides

Tides caused by the gravitational attraction of the moon, creating bulges in the ocean.

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High Tide

Occurs when an area moves through the crest of a tidal bulge.

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Low Tide

Occurs when an area moves through the trough of a tidal bulge.

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Lunar Day

The time it takes for the moon to return to the highest point in the sky, approximately 24 hours and 50 minutes.

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Solar Tides

Tides influenced by the sun’s gravitational pull, which are smaller than lunar tides due to distance.

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Neap Tides

Tides that occur when the moon, Earth, and sun form a right angle, resulting in smaller high tides.

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Spring Tides

Tides that occur when the Earth, moon, and sun are in alignment, resulting in higher high tides and lower low tides.

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Diurnal Tides

Tides characterized by one high and one low tide each lunar day.

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Semidiurnal Tides

Tides characterized by two high tides and two low tides of nearly equal height each lunar day.

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Mixed Tides

Tides characterized by successive high tides and low tides of significantly different heights.

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Tidal Datum

Reference level for comparing tidal height, which could be mean sea surface level or mean of all low tides.

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Tidal Bore

A high wave generated by a tide crest that advances rapidly up an estuary or river.

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Coriolis Effect

The apparent deflection of moving objects caused by Earth's rotation, influencing tidal water movement around amphidromic points.