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Chapter 14 Waves, Beaches, and Coasts

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Wave height: Vertical distance between the crest and trough of the wave. ... in bays. Continued evolution results in coastal straightening. ... – PowerPoint PPT presentation

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Title: Chapter 14 Waves, Beaches, and Coasts


1
Chapter 14Waves, Beaches, and Coasts
Photo credit G. Mattioli
2
Water Waves
  • Surf

Nearshore Circulation
  • Wave Refraction
  • Longshore Currents
  • Rip Currents

3
Wave Characteristics
4
Wave Features
  • Wave height Vertical distance between the crest
    and trough of the wave.
  • Wave crest Highest point on the wave.
  • Wave trough Lowest point on the wave.
  • Ocean waves range 0.3 to 5 m can be as high as
    15 m.
  • Wavelength Horizontal distance between two wave
    crests or troughs.
  • Ocean waves range from 40 to 400 m.
  • Wave period Time for one wavelength to pass.
    This is inversely related to frequency P 1/f.
  • Ocean wave velocities range from 25 to 90 km/hr.

5
Orbital Motion Animation
6
Wave Particle Motion
7
Wave Interaction with Sea Floor
8
Oblique Waves
Wind and wave direction
Normal component
Beach parallel component
9
Longshore Current
10
Rip Currents
Rip currents water that flows straight out to
sea from the surf zone. Travel at the surface
and die out at depth. Carry fine grained
particles out of surf zone to deeper water.
11
Beach Terminology
12
Beach Features, CA
13
Seasons and Beach Development
14
Beach Seasonal Cycle Animation
15
Longshore Sand Movement
16
Longshore Drift Animation
17
Baymouth Bar - Russian River, CA
18
Spit and Bar Development Animation
19
Tombolo Development
20
Tombolo - Santa Cruz, CA
21
Beaches
  • Longshore Drift of Sediment
  • Human Interference with Sand Drift
  • Jetties
  • Breakwaters
  • Groins
  • Sources of Sand on Beaches
  • Deposition from rivers
  • Erosion of local rocks in cliffs and headlands
  • Transport from offshore regions
  • Bioclastics

22
Sand Erosion and Deposition Jetties
23
Sand Erosion and Deposition Groins
24
Wave Refraction Along Irregular Coast
Focusing of wave energy causes erosion of
headlands and deposition in bays. Continued
evolution results in coastal straightening.
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