Wave Generation + Characteristics Flashcards

1
Q

What is the crest of a wave?

A

Highest point

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2
Q

What is the trough of a wave?

A

Lowest point

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3
Q

What is the wave length?

A

Distance from crest to crest

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4
Q

What is the wave height?

A

Vertical distance between crest + trough

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5
Q

How do waves form?

A
  • winds move across the surface of the water = frictional drag, which creates small ripples + waves
  • this leads to a circular orbital motion of water particles in the ocean
  • as the seabed becomes shallower towards the coastline, the orbit of the water particles becomes more elliptical = causes more horizontal movement of waves
  • the wave height increases, but wave length + velocity both decrease
  • this causes water to back up from behind the wave until the wave breaks + surges up the beach
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6
Q

What influences the size of+ energy of waves?

A
  • strength of wind
  • duration of wind
  • size of the fetch
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7
Q

How does the strength of the wind influence the size + energy of a wave?

A
  • wind = movement of air from high to low pressure
  • the different pressure areas are caused by variations in surface heating by the sun
  • larger the difference in pressure between two areas = strong winds = stronger waves
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8
Q

How does the duration of the wind influence size + energy of waves?

A
  • if the wind is active for longer periods of time, the energy of the waves will build up + increase
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9
Q

How does the size of the fetch influence the size + energy of waves

A
  • fetch is the distance over which the wind blows
  • the larger it is, the more powerful the waves will be
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10
Q

How are shallow water waves formed?

A
  • waves approach the shore + the wave length is greater than depth
  • the wave touches the bottom + experiences friction
  • the wave starts to have an eleipitcal orbit + becomes a ‘wave of translation’
  • wave length starts to decrease + wave height increases
  • this is called shoaling + beaches begin to form
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11
Q

What is spilling?

A
  • steep waves
  • gentle beach gradient
  • gradual peaking
  • becomes unstable + spills forward
  • strong Swash
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12
Q

What is plunging?

A
  • steeper beaches
  • wave face becomes vertical + plunges
  • strong backwash
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13
Q

what is surging?

A
  • low steepness of waves
  • steep beach gradient
  • waves don’t break but surge gently up beach
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14
Q

What is Swash + backwash?

A
  • how waves move onto + off a beach
  • Swash = movement of the wave onto the beach after a wave breaks. Material being carried by waves is deposited onto the beach
  • backwash = movement of the wave back down the beach. Backwash drags any material off a beach
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15
Q

What are constructive waves?

A
  • tend to deposit material, creating deposition land forms + increase size of beaches
  • Swash is stronger than backwash
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16
Q

Characteristics of a constructive wave?

A
  • formed by weather systems that operate in the open water
  • elliptical orbit due to friction = long wave length
  • flat waves which spill over
  • strong Swash pushes material up the beach + weak backlash because water percolates into sand
  • occurs on gently sloped beaches
17
Q

What is a destructive wave?

A
  • removes depositional landforms through erosion, thereby decreasing the size of the beach
  • backwash is stronger than the Swash
18
Q

Characteristics of a destructive wave?

A
  • formed by localised storm events with strong winds
  • short wavelength
  • steep waves which plunge forward
  • weak Swash + strong backwash + little percolation meaning beach cliffs can form
  • occurs on steeply sloped beaches
19
Q

What are high energy coastlines?

A
  • associated with powerful waves so occur in areas where there is a large fetch
  • typically have rocky headlands + landforms
  • fairly frequent destructive waves
  • as a result these coastlines are often eroding as the the rate of erosion exceeds the rate of deposition
20
Q

What are low energy coastlines?

A
  • less powerful waves + occur in sheltered areas
  • constructive waves prevail = sandy beaches
  • there are landforms of deposition as the rate of deposition exceeds the rate of erosion
21
Q

What is wave refraction?

A
  • process by which waves turn + lose energy around a headland on uneven coastlines
  • the wave energy is focused on the headlands, creating erosive features in these areas
  • the energy is dissipated in bats leading to the formation of features associated with low energy environments such as beaches
22
Q

Why do waves break?

A
  • waves interact with the sea floor when they move into shallower water near the shore = friction between the wave + flow = wave slows down
  • wavelength decreases when the wave slows down, causing the wave to become steeper = shoaling
  • the shoaling process continues until the wave heigh can no longer be supported as it is too high = wave breaks