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46 Cards in this Set
- Front
- Back
Breaker
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Sea surface water wave has become too steep to be stable and collapses
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Capillary Wave
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Wave with wavelength less than 1.5 cm in which the primary restoring force is surface tension
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Centrifugal Force
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outward-directed force acting on a body moving along a curved path or rotating about an axis; an internal force
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Centripetal force
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inward-directed force necessary to keep an object moving in a curved oath or rotating about an axis
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Deep-water wave
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wave in water; the depth of which is greater than one-half the wavelength
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diffraction
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process that transmits energy laterally along a wave crest
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dispersion (sorting)
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sorting of waves as they move out from a storm center; occurs because long-period waves travel faster in deep water than short period waves
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diurnal tide (declinational tide)
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tide with one high water and one low water each tidal day
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dynamic equilibrium
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state in which the sums of all changes are balanced and there is no net change
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episodic wave
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abnormally high wave unrelated to local storm conditions
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equilibrium tide
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theoretical tide formed by the tide-producing forces of the moon and sun on a nonrotating, water-covered earth
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fetch
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continuous area of water over which the wind blows in essentially a constant direction
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forced wave
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wave generated by a continuously acting force and caused to move at a speed faster than it freely travels
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free wave
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wave that continues to move at its natural speed after its generation by a force
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generating force
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disturbing force that creates a wave, such as wind or a landslide entering water
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gravity wave
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water wave form in which gravity acts as the restoring force; a wave with wavelength greater than 2 cm
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group speed
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speed at which a group of waves travels (in deep water, group speed equals one-half the speed of an individual wave); the speed at which the wave energy is propagated
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internal wave
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wave created below the sea surface at the boundary between two density layers
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mixed tide
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type of tide in which large inequalities between the two high waters and two low waters occur in a tidal day
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moon tide
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portion of the tide generated solely by the moon's tide-raising force, as distinguished from that of the sun
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neap tides
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tides occurring near the times of the first and last quarters of the moon, when them range of the tide is least
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progressive wind wave
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wave that moves, or progresses, in a certain direction
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restoring force
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force that returns a disturbed water surface to the equilibrium level, such as surface tension and gravity
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rip current
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strong surface current flowing seaward from shore; the return movement of water piled up on the shore by incoming waves and wind
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semi-diurnal tide
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tide with two high waters and two low waters each tidal day
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shallow water wave
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wave in water whose depth is less than one twentieth the average wavelength
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slack water
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state of tidal current when its velocity is near zero; occurs when the tidal current changes direction
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spring tides
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tides occurring near the times of the new and full moon, when the range of the tide is greatest
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standing wave
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type of wave in which the surface of the water oscillates vertically between fixed points called nodes, without progression; the points of maximum vertical rise and fall called antinodes
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storm center
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area of origin for surface waves generated by the wind; an intense atmospheric low-pressure system
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sun tide
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portion of the tide generated solely by the sun's tide-raising force, as distinguished from that of the moon
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swell
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long and relatively uniform wind-generated ocean waves that have traveled out of their generating area
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tidal bore
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high-tide crest that advances rapidly up an estuary or river as a breaking wave
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tidal current
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alternating horizontal movement of water associated with the rise and fall of the tide
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tidal datum
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reference level from which ocean depths and tide heights are measured; the zero tide level
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tidal day
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time interval between two successive passes of the moon over a meridian, approximately twenty-four house and fifty minutes
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tide wave
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long-period gravity wave that has ts origin in the tide-producing force and is observed as the rise and fall of the tide
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tsunami (seismic sea wave)
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long-period sea wave produced by a submarine earthquake, volcanic eruption, sediment slide, or seafloor faulting. It may travel across the ocean for thousands of miles unnoticed from its point of origin and build up to great heights over shallow water at the shore
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wave crest
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highest part of a wave
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wave height
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vertical distance between a wave crest and the adjacent trough
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wave length
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horizontal distance between two successive wave crests or two successive wave troughs
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wave period
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time required for two successive wave crests or troughs to pass a fixed point
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wave ray
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line indicating the direction waves travel; drawn at right angles to the wave crests
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wave steepness
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ratio of wave height to wavelength
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wave train
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series of similar waves from the same direction
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wave trough
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lowest part of the wave
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