Waves Flashcards
A disturbance or oscillation that travels to a matter or space accompanies by a transfer of energy. Can carry energy from one place to another, as a medium they are like a harmonic oscillator, they require a “restoring force” and inertia.
Waves
Propagate along a surface or interface
Surface Waves
Caused by energy passing through the water, causing the water to move in a circular motion. A progression of energy from one point to another and does no move forward, only the energy in it progresses.
Waves
Visual proof of the transmission of energy across the surface of the ocean.
Ocean Waves
Anatomy of a Wave:
- Highest point in the wave
- Lowest point in the wave
- Vertical distance between the wave crest and the wave trough
- Water displacement from its undisturbed state. Always one-half the wave height (at least for a symmetric wave).
- Distance from one crest to the next crest or from one trough to the next trough.
- Crest
- Trough
- Wave Height
- Wave Amplitude
- Wavelength
Defined as wave height divided by wavelength (S = H/L). Therefore, the same wave height will result in high steepness if the wavelength becomes smaller.
Wave Steepness
Number of wave crests passing point A, each second.
Wave Frequency
Time Required for the wave crest at point A to reach point B
Wave Period
Half of the wave height
Amplitude
Waveheight divided by wavelength (H/L)
Steepness
Causes waves to form
Disturbing Force
Interface of Fluids with Different Densities:
- Air-ocean interface
- Air-air interface
- Water-water interface
- Ocean Waves
- Atmospheric Waves
- Internal Waves
Acts on a water particle displaced from its equilibrium position
Restoring Force
Type of Wave:
- <1 Second, <2 Cm
- 1-10 Sec, 1-10 m
- 10-30 Sec, up to 100 m
- 5-90 minutes, 20 km to 300+ km
- Capillary or Ripple
- Chop
- Swell
- Tsunami
Source of Types of Waves:
- Winds
- Gravity (Tides)
- Discontinuity in Ocean Surface
*Earthquake (Tsunamis)
*Landslides
*Rain Drops
Most Ocean Waves Generated by Winds:
- Ripples, Wind generates initial stress on sea surface
- More energy transferred to ocean, Trochoidal waveform as crests become pointed
- Any wave that has moved out of its wind generation source region
- Capillary Waves
- Gravity Waves
- Swell
Wave size depends on the:
- The area over which the wind is blowing
- The speed at which the wind is blowing
- How long the wind has been blowing
- Fetch
- Wind Velocity
- Duration
Equilibrium Condition, waves can grow no further
Fully Developed Sea
Uniform, symmetrical waves that travel outward from storm area, long crests, transport energy long distances
Swell
As waves move beyond ___, wind speed ____ and waves move ____ than wind. Wave Steepness ____ and waves become ______ waves.
Fetch, Decreases, Faster, Decreases, Long-Crested
Factors Affecting Wave Energy:
*
*
* Distance over which wind blows
- Wind Speed
- Wind Duration
- Fetch
Waves:
Stage 1: ?
Stage 2: ?
Stage 3: ?
Capillary Waves (CM Scale)
Wind Waves
Mature Sea - Swell
Directly related to wave energy and is usually less than 2 meters.
Wave Height
Breakers called ____ form when wave reaches critical steepness.
Whitecaps
Describes appearance of sea surface
Beaufort Wind Scale
A standing wave that oscillates back and forth within a water body. Water sloshes back and forth, and the wave decreases in size due to friction as its oscillation tries to reach equilibrium. Most often, generated by a persistent strong wind blowing down the long axis of a large water body. When the wind subsides, the water is released as a _____ wave. Can also be generated by a disturbance such as an earthquake, landslide, wave interaction, changes in air pressure, or changes of wind.
Seiche