Waves & Tsunamis Flashcards

1
Q

All waves

A

T = period (S) one wave crest to the next
steepness = H / L
speed = L / T

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2
Q

Deep water wave speed

A

speed S = 1.25 * swrt(L)
S = 1.56 * T
Longer wavelengths travel faster

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3
Q

Shallow water wave speed

A

speed S = sqrt(gd)
S = 3.1 * swrt(d)
g = gravitational constant, d = water depth
waves travel faster in deeper water (no dependence on wave length)
examples: tides & tsunamis

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4
Q

Generation of wind-driven waves

A

Wave energy imparted to ocean depends:
- wind speed
- duration (longer the wind blows)
- fetch (area over which the wind blows)

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5
Q

Wave height plot

A
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6
Q

Beaufort scale

A

Relates wind energy and wind speed to appearance of sea surface

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7
Q

How do waves go from chop to swell?

A
  • storm puts more energy into ocean, waves move away from storm
    Wave dispersion:
  • waves with longer wavelengths travel faster
  • waves are sorted by wavelength/speed
  • longer wavelengths reach the shore first
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8
Q

Deep water wave train speed

A

Wave energy travels more slowly than each wave crest (for deep water waves)
- leading wave dies out, new wave forms behind
- wave train (and wave energy) travels at 1/2 speed of individual wave

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9
Q

Interference - what happens when two wave systems (swells) collide?

A

Destructive interference
Constructive interference

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10
Q

Mixed wave inteference

A

Patterns of small and tall eaves along coast

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11
Q

Non-linear affects

A
  • Linear: The combined height equals the sum of the individual waves
  • Non-linear: create rogue waves that are tller than the sum of the individual waves
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12
Q

Rogue waves

A
  • an anomalously large wave that is over twice as big as the significant wave height of the surrounding sea state
  • caused by a combination of multiple waves and non-linear effects
  • occur in open ocean with multiple swells
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13
Q

Onshore progression

A

Deep waves become shallow
- wave speed decreases as become shallow-water waves
- wavelength decreases
- wave height increases
- waves break when height: wavelength ratios exceeds ~1.7
- speed goes doen bc dependent on water depth

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14
Q

Types of breakers

A
  • spilling breakers: foam, not a dramatic break
  • plunging breakers: steeper beach, drmatic steepening of waves, depth changes fast = speed changes fast
  • surging breakers: too steep, lots of foam, not a clean break
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15
Q

What makes the world’s biggest waves surfable?

A

The underwater canyon focuses wave energy like a magnifying glass focuses light energy

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16
Q

Wave refraction

A
  • waves usually appraoch the coast at an angle
  • one end of the wave shoals before the other = refraction
17
Q

Tsunamis

A
  • long wavelength ocean waves generated by submarine earthquakes, landslides, volcanic eruptions, and meteor impacts
  • shallow water waves, wave orbitals smushes at the bottom (long wavelength and low wave period)
  • behaves as a shallow water wave (depth is <1/20 wavelength)
  • they can pass unoticed at sea (not very tall compared to its long wavelength)
18
Q

Which waves are the most deadly?

A
  • rogue waves: abnormally large waves in the open ocean observed by mariners
  • tidal waves: the wave that creates the twice-daily up and down motion of the tides (often incorrectly used to describe a rogue wave)
  • seiches: large-scale sloshing of water in lakes
  • tsunamis: large waves creates by earthquakes or landslides
  • sneaker waves: multiple waves crashing together on a beach
  • wind-driven waves: the most common type of wave ___
19
Q

Why are tsunamis so destructive?

A
  • energy compresses into smaller area, creating larger wave with steeper crest
  • small amplitudes in the deep ocean, but as they approach land they slow down and create waves up to 40 m
20
Q

Tsunami detection

A

Bottom pressure recorder: detects tsunamis with amplitudes as small as 30 mm in 6,000 m of water
-DART: record pressure

21
Q

How fast do tsunamis travel?

A

example:
propogation speed: 196

22
Q

Pacific ring of fire

A

80% of tsunamis occure in Pacififc ocean