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Vocabulary flashcards about tides, lunar influence, and related concepts.
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Tides
Result from the gravitational pull of the moon and, to a lesser degree, the sun.
Tides
Very long-period waves that originate in the ocean and progress toward the coastlines where they appear as the regular rise and fall of the sea surface.
Equilibrium Theory
Proposed by Isaac Newton as an explanation for the tides, assuming a perfectly uniform Earth, very deep water, and no landmasses.
Dynamic Theory
Modified Newton’s model to account for tidal variations; it shows there are several tidal bulges, not just two.
High Tide
Occurs when the highest part of the tide (crest) reaches the coast.
Low Tide
Occurs when the lowest part of the wave, or its trough, reaches the coast.
Tidal Range
The difference in height between the high tide and the low tide.
Tidal Current
The horizontal movement of water that accompanies the rising and falling of the tide.
Flood Current
The incoming tide along the coast and into bays and estuaries.
Ebb Current
The outgoing tidal current.
Slack Current
The outflow of a tide.
Spring Tides
Highest and lowest tides that occur when the sun and moon are aligned on the same or opposite sides of the Earth (new or full moon).
Neap Tides
Weaker tides that occur when the moon is in a quarter moon phase, and the sun and moon are at a right angle to the Earth.
Declination of Moon
The angle of the Moon’s orbit with respect to the Earth’s equator.
Perihelion
Earth’s closest approach to the Sun.
Aphelion
Earth’s farthest distance from the Sun.
Perigee
Moon’s closest approach to the Earth.
Apogee
Moon’s farthest distance from the Earth.
Super Moon
When the Moon is at perigee, it appears ~14% larger when viewed from Earth.
King Tide
Common term to describe extra large high tides that occur when the Earth, Moon, and Sun are aligned at perigee and perihelion.
Underwater bathymetry
Shape of the seafloor
Diurnal Tide
Having a single low and high tide daily
Semidiurnal Tide
Having two roughly equal high and low tides daily.
Mixed Tide
Having two unequal high and low tides daily.
Tidal Bore
Forms when the incoming tide produces a wave that flows into a river or other narrow area.
Amphidromic points
Points where the water doesn’t rise and fall with the tides.
Tide Gauge
A device for measuring the change in sea level relative to a baseline such as mean sea level.