1b) Flashcards

Coastal landscape systems are influenced by a range of physical factors:

1
Q

What are the 5 physical factors influencing coastal landscape systems?

A
  • Winds
  • Waves
  • Tides
  • Geology
  • Global patterns of Ocean currents
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2
Q

1) What/ why are waves?

2) Name two types:

A

1 - Created by the frictional drag of wind on the surface of the sea.

2 - local wind’s waves = sea waves
- distant storm’s waves = swell waves

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3
Q

What three factors does the energy (kinetic and/or potential) of the waves depend upon?

A
  • wind velocity
  • duration (time over which wind blew over water)
  • fetch (distance over which wind blew over water)
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4
Q

Why does SW of England experience the most destructive waves?

A
  • larger stretch of open sea (more fetch) and due to direction of prevailing winds.
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5
Q

What are the characteristics of swell waves?

A
  • As the swell wave advances, its crest becomes flattened and rounded and its surface smooth.
  • Relatively long and regular periods.
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6
Q

What type of wave is more likely to form from Swell?

A

I dunno lemme check and get back to you bro.

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7
Q

Why/ how do waves break?

A
  • waves move into shallower water
  • friction between deepest circling water molecules and the seafloor increases
  • bottom of wave slows down
  • waves bunch up and wavelength decreases
  • once water depth is less than 1.3×s the wave height, the wave breaks
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8
Q

What are the 3 types of breaking waves?

A
  • spilling
  • plunging
  • surging
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9
Q

What is the slope like for the following breaking wave types?:

1) spilling
2) plunging
3) surging

A

1 - gentle slope

2 - moderately steep beach

3 - very steep

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10
Q

Characteristics of constructive vs destructive waves:

1) Height:
2) Wavelength:
3) Frequency:
4) usually break as?:
5) why do they break as they do (more detail basically)?:
6) effect on beaches/sediment:

A

1) low VS tall.
2) long VS shorter.
3) low (6-8/minute) VS high (8-14/minute).
4) spilling (strong swash travels along way up the gently sloping beach)

VS

plunging (little forward energy transfer small swash; friction also slows the swash).

5) long-wavelength; backwash returns to the sea before the next week breaks so swash is uninterrupted and retains energy.

VS

short-wavelength; incoming swash is often slowed by the backwash as the backwash reaches at the same time.

6) tend to build up beaches and make them steeper.

VS

tend to transport sediment offshore thus decreasing the sediment.

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11
Q

Equation for power wave height and wave period:

A

Power = (wave height)^2 x wave period

kW/ m of wavefront

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12
Q

Crest

A

Highest surface part of a wave

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13
Q

Wave height

A

Vertical distance between the crest and trough

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14
Q

Wavelength

A

Horizontal distance between two adjacent crests/ troughs

Swell wave period = 20 seconds and long wavelength

Local storm wave period = shorter
Also short wavelength and greater height

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15
Q

Still water level

A

Rest position of wave

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16
Q

Trough length region

A

Length that wave travels below the still water level

17
Q

Crest length region

A

Length that wave travels above the still water level

18
Q

Depth

A

Distance between the still water level and the ocean bottom

19
Q

Trough

A

Lowest point of a wave

20
Q

What are Tides?

A

The regular rising and falling movements of the surface of the sea.

21
Q

How are tides formed?

A
  • caused by gravitational pull of moon and sun on oceans
  • moon has greatest influence lower gravitational pull but much closer
  • creates outward bulge in oceans closest to moon and on other side of earth away from moon
  • area between high tides = low tides
  • When the moon is between earth and sun combined gravitational pull create biggest bulge of water cold spring tide
  • When earth moon and sun form right angles gravitational pulls interfere with each other and produce the lowest high tides and the highest low tides; the smallest tidal range - these are called neap tides
22
Q

When do spring tides occur?

A

Shortly after new and full moon when the gravitational forces of sun and moon reinforce each other resulting in a higher than normal tidal range.

23
Q

When do neap tides occur?

A

After the moon is in its 1st and 3rd quarters when the gravitational forces are at right angles to each other in a lower than normal tidal range.

24
Q

What are tidal ranges like in enclosed seas?

A

Tidal ranges are low and so wave action is restricted to a narrow area of land i e Mediterranean.

25
Q

What are tidal ranges like in funnel coasts?

A

The tidal range can be as high as 14m, i.e. in the Severn estuary.

26
Q

Yeh

A

Chonglong