waves Flashcards
what is a wave?
a disturbance of the surface of water
what are the two forces that are involved in waves?
generating/disturbing force & restoring force (gravity/surface tension)
describe the wave anatomy?
Crest = top of the wave
Trough = bottom of the wave
Height (H) = vertical distance from trough to crest
Amplitude (α) = 1/2 height
Wavelength (L or λ) = horizontal distance crest to crest, or trough to
trough
Steepness = H / L
speed
Speed (celerity!) = wavelength / period = L/T
wave frequency
the number of wave crests passing point A each second
wave period
the time required for the wave crest at point A to reach point B
what’s wave motion?
a flow of ENERGY where particles, like a water molecule, travel in an orbital motion
Wave train indicates direction of energy movement
explain the depth effect
If the bottom is deeper than ½ L
(wavelength), then circular orbits = deep
water waves
If bottom is not deeper than ½ L, then
the orbits become ellipses (flattened
circles) = shallow water waves
Friction and compression of orbits
decreases forward speed of the wave
Wave speed decreases as depth
decreases
breaking waves
Wave height increases in shallow water
Bottom part of the wave moves more slowly than the top
of the wave (crest) 🡪 wave breaks
Wave breaks at critical steepness (H:L) > 1:7
what factors influence waves?
Depth of water – ✔
Wind speed & duration – the greater the wind speed and the duration, the larger the waves
- Beaufort scale
Fetch – the distance the wind can blow across the water unobstructed; The greater the fetch, the greater the wave potential
For wind generated waves, fetch is key to size – a longer fetch creates a higher energy wave
enumerate the types of waves
swells, standing waves (seiches), rogue waves, internal waves, tsunamis
describe the swells
waves that are no longer under the influence of the wind
The waves in a fully developed sea outrun the storm that creates them, lengthening and reducing in height in the process
Swells organize into groups smooth and regular in appearance
Able to travel 1000’s of km unchanged in height and period
describe the standing waves (seiches)
result from the combination of reflected waves interfering constructively with incident waves, they stay in one place instead of progressing, repeated crests/troughs in one place
e.g. at Race Rocks when the wind and tidal current are in opposition creates standing waves
describe the rogue waves
Larger than expected waves, usually associated with long period waves from distant storms (also called episodic waves, sneaker waves, extreme storm waves)
describe the internal waves
Waves that oscillate within rather than at
the surface, often found in stratified water at pycnoclines