1b) Flashcards
Coastal landscape systems are influenced by a range of physical factors:
What are the 5 physical factors influencing coastal landscape systems?
- Winds
- Waves
- Tides
- Geology
- Global patterns of Ocean currents
1) What/ why are waves?
2) Name two types:
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
What three factors does the energy (kinetic and/or potential) of the waves depend upon?
- wind velocity
- duration (time over which wind blew over water)
- fetch (distance over which wind blew over water)
Why does SW of England experience the most destructive waves?
- larger stretch of open sea (more fetch) and due to direction of prevailing winds.
What are the characteristics of swell waves?
- As the swell wave advances, its crest becomes flattened and rounded and its surface smooth.
- Relatively long and regular periods.
What type of wave is more likely to form from Swell?
I dunno lemme check and get back to you bro.
Why/ how do waves break?
- 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
What are the 3 types of breaking waves?
- spilling
- plunging
- surging
What is the slope like for the following breaking wave types?:
1) spilling
2) plunging
3) surging
1 - gentle slope
2 - moderately steep beach
3 - very steep
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:
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.
Equation for power wave height and wave period:
Power = (wave height)^2 x wave period
kW/ m of wavefront
Crest
Highest surface part of a wave
Wave height
Vertical distance between the crest and trough
Wavelength
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
Still water level
Rest position of wave