Zusammenfassung der Ressource
Waves and Tides
- Waves
Anmerkungen:
- http://www.s-cool.co.uk/a-level/geography/coastal-processes/revise-it/wave-processes
- Constructive waves
Anmerkungen:
- Also known as Swell or Surging waves
- Depsitional
- Long wave length
Anmerkungen:
- Low Frequency
Anmerkungen:
- Elliptical orbit
- Swash is larger than Backwash
- Low Gradient
- Caused by distant storms
- Create Berms
- Destructive waves
Anmerkungen:
- Also known as surfing, storm, or plunging
- Erosional
- Short wave length
Anmerkungen:
- High Frequency
Anmerkungen:
- Circular orbit
- Larger backwash than Swash
- Steep graident
- Caused by local winds/storms
- Caused by:
- The surface of the sea
exerting frictional drag on the
lowest layer of wind
- The distance (fetch) travelled
before the wave reaches the
shoreline
- How long the wind had blown for
- How strong the wind is
- Wave refraction
- Occurs when waves approches a waveline
- Which is a irregular coastline
- As waves approach a coast they are
refracted so that their energy is
concentrated around headlands but
reduced around bays.
- Waves then tend to approach
coastline parallel to it, and their
energy decreases as water depth
decreases.
- Tides
- Caused by
- Controlled by the gravitational pull of
the moon (and to a lesser extent the
sun)
- High Tide
- The Moon pulls the water of the
earth towards it, creating a bulge
(High tide)
- The Moon pulls the Earth towards it,
creating a bulge of water on the otherside of
the earth to the high tide
- Spring tide
- Twice a month, the Earth, Moon and Sun
align
- Puts an extra gravitational
pull on the earth
- Producing an extra high tide
- Neap tide
- Lowest tidal range
- Occur when the Sun and Moon
are at right angles to each other