GEO 230 EXAM 3 Flashcards

1
Q

Waves are the manifestation of the translation of energy through a medium

A

The medium does not travel in the direction of the wave

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2
Q

Ocean waves are orbital waves and combine elements of 2 fundamental wave types

A

Longitudinal (push-pull)

Transverse (side to side)

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3
Q

Crest

A

High point of wave

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4
Q

Trough

A

Low point of wave

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5
Q

Stillwater (or mean water) level

A

Relaxed level of water surface

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6
Q

Wave height (H)

A

Crest to trough distance

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7
Q

Amplitude (A)

A

H/2

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8
Q

Wavelength (L)

A

Crest to crest distance

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9
Q

Wave steepness

A

H/L

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10
Q

Period (T)

A

Time it takes for one wavelength to pass a reference point in a given time (T= 1/F)

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11
Q

Frequency (F)

A

of wave crests to pass a reference point in a given time (F=1/T)

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12
Q

Wavespeed (C)

A

1/period = 1/T

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13
Q

Progressive waves

A

Moves across surface

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14
Q

Standing waves

A

Stay in one place

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15
Q

Wave motion

A

Path of water molecule

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16
Q

Deep water waves

A

If water depth (d) > L/2

Waves have no interference with ocean bottom

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17
Q

Wave Speed-C

A

For deeper waves, the longer the wavelength, the faster the wave C= 1.25 square root of L

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18
Q

Shallow-water waves

A

If water depth d

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19
Q

Transitional (intermediate) waves

A

If what we depth L/2

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20
Q

Light winds

A

Capillary waves
Max wavelength 1.7 cm
Rounded crests, v shaped troughs
Disappear quickly when wind stops

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21
Q

Increasing wind

A

Larger waves

22
Q

What causes waves?

A

Movement of air (wind)-ocean waves
Mass movement into ocean- splash waves
Sea floor movement (earthquake)-tsunami
Gravitational pull of the moon & sun- tides

23
Q

Smooth sine waves

A

Pointed crests; round troughs

24
Q

Breaking waves

A

Deep water waves

Waves form white caps (breaks) when they get too steep

25
When steepness H/L > 1:7 they
Break
26
Spray
Tops of waves get blown off completely due to wind When it gets heavy it's called... Spindrift
27
Factors affecting wave height
Wind speed Wind duration Fetch- uninterrupted distance over which wind blows
28
When a sea reaches equilibrium state
Energy gain = energy loss | Called "fully developed"
29
Largest wave recorded
34 meters = 100 feet
30
Wave dissipation
When a force creates a wave the wave is propagated through water
31
Rogue waves
Unusually large waves Super waves Freak waves Perfect storm wave
32
Surf zone
The zone of breaking waves
33
Sequence
``` Wave touches bottom Wavelength shortens Velocity decreases Wave height increases Breakers form ```
34
When wave steepness H/L > 1:7 waves
Break in surf
35
Local winds
Disorganized chaotic surf
36
Swells
Long wavelength More organized Orderly surf
37
Shallow---spilling breaker
When sea floor is almost flat and gentle, wave break progressively as they make their way in shore
38
Moderately steep---plunging breaker
When sea floor slope is moderately steep these produce the spectacular curling waves that surfers covet Produced when wave top get ahead of wave base that is slowed by sea floor
39
Steep---collapsing breaker
Occurs when sea floor is steep and leading edge of wave collapses before crest can develop
40
Very steep---surging breaker
Waves surge in and away from beach
41
Wave refraction
Waves coming in at angle Bending of waves as reaches shore Waves slow down as they feel bottom in surf zone Become more parallel to shoreline
42
Wave diffraction
Waves hitting irregular shoreline | Waves radiate from a point
43
Wave reflection
Reflection of waves off a breakwall
44
Tsu
Harbor
45
Nami
Wave
46
Tsunamis
Cause= sudden movement on sea floor from earthquakes, landslides, or underwater volcanic eruptions Referred to as seismic sea waves
47
Changes when waves hit shallow water
Wavelength shortens Velocity decreases Wave height increases
48
Shore
Between low tide and highest elevation affected by storm waves
49
Coast
From shore to farthest inland ocean-related features
50
Coastline
Boundary between shore and ocean