BIOL 331
Lecture 4
Waves
Wave Terminology
- Crest
- Trough
- Wave length
- Wave height
- Wave Period
Types of Waves and Relative Energy
- Ripples
- Chop
- Sea
- Swell
- Surf Beat
- Tsunamis
- Tides
Historical Studies on Ideal Waves
1802: Franz Gerstner
- Water particles in waves move in circles
- Surface trace of a wave is approximately a trochoid
- (like sine waves).
1825: Ernst & Wilhelm Weber
- Used a wave channel to study waves
- Filled it with variety of liquids (brandy, mercury,
- water, etc.)
- Three important discoveries:
- Waves reflected with no energy loss
- Suspended particles trace circles
- Near bottom orbits are nearly flat
Fundamental Properties of Waves
I. Wave Length, Period & Velocity
- Wave length depends upon period
The following hold true for deep water waves (d/L > 1/2)

L = length in feet, T = period in seconds, g = acceleration of gravity
- Wave velocity depends on wave length

C = velocity in feet per second
- For shallow water the velocity equation must be modified
For d/L between 0.05 and 0.5:

For d/L < 0.05:

II. Wave Height
- Appears at first to be independent of wave period & length
- Holding wave length constant (e.g. 5.12 feet) and increasing wave height results in
waves over 8 inches (0.75 feet) "breaking"
- Repeated experiments show that wave crest angle cannot be more than 120o
- Steepness (ratio of H/L) cannot exceed 1:7
- Waves at 1:7 move 10% faster than predicted.
III. Orbital Motion
- Movement of water molecules studied using "gunk" (xylol & butyl phthalate
whitened and weighted with zinc oxide
- Surface particles make an orbit = the wave height, deeper orbits are progressively
smaller
- Repeated observations show that at D = L/9 the diameter of the orbit is halved
- Deeper orbits become more and more flattened
- At bottom the particles simply move back and forth
IV. Mass Transit
- If particles are watched over time, the orbits gradually move toward direction of waves.
- Movement of particles is small, but significant given time
Waves Caused by Wind
Factors Determining Wave Development:
- Wind velocity
- Length of time wind blows
- Length of fetch
Other Considerations
- Wind is never constant
- Direction of wind often shifts erratically
- Wave size and direction therefore highly variable
- Waves of 75 to over 100 feet have been documented
Characteristics of Shallow Water Waves

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