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42 Cards in this Set

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  • Back
  • 3rd side (hint)
Surface and ocean currents
Surface- set In motion by atmos winds, have speeds 1/100th of winds, 5 years for surface water to cross ocean basin
Ocean-deflected by Coriolis effect, slower than winds
Gyres
Centered at 30° lat
NH rotates clockwise
SH rotates counter clockwise
Shan
Windrows
Series of parallel rows of debris lining up in the direction of the wind
Langmuir cells
Common wave generating forces
Wind, atmos storms, ocean currents
Most common restoring forces
Surface tension, gravity
Deep water waves
Wave depth exceeds half of the wavelength, long deep water waves are faster, progressive wind waves
Forced waves
Generated by varying wind speed and direction in storms, forced waves far from the storm are called free waves
In phase waves
Out of in phase waves
When the crest of one wave is equal to the crest of another
When the crest of one wave is equal to the trough of another
Limits of max wave height
Wind speed, wind duration, fetch (distance over which wind blows)
Wave energy
Wave steepness
Wave energy is directly proportional to wave height

Steepness is the ratio of wave height to wavelength
Surf zone
Shallow coastal regions, waves slow down, steepen and break and dissipate as turbulence and spray
Breakers
Plungers
Spillers
Breakers are classified as plungers and spillers
Plungers- curling crest outruns the rest of the wave and spills over
Spillers- gradually move up the shallow bottom
Internal waves
Generated by low pressure, change of ocean currents, currents moving over sea bottom
Single node standing wave
Two node standing wave
Node is in the middle, antinodes are at the end

Nodes are 1/4 and 3/4 distance, antinodes are in the middle and at the end
Tsunami
Causes by earthquakes, volcanic eruptions, landslides, meteors, comets or asteroid impacts, shallow water waves, low steepness, slows down and shortens in shallow water, sea recedes if trough is leading edge, flooding occurs if crest is leading edge
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
New moon
Spring tide
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
New moon
Spring tide
First quarter moon
Neap tide
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
New moon
Spring tide
First quarter moon
Neap tide
Full moon
Spring tide
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
New moon
Spring tide
First quarter moon
Neap tide
Full moon
Spring tide
Last quarter
Neap tide
Diurnal tides
Semi-diurnal
Mixed tides
One high and one low tide per day

Two high and low tides per day

Two high and low tides of unequal water levels per day
Rising tides
Falling tides
Called flood tides

Called ebb tides
New moon
Spring tide
First quarter moon
Neap tide
Full moon
Spring tide
Last quarter
Neap tide
Tidal bores
Bay of fundy in Nova Scotia