Lecture 6- Ocean Waves Flashcards
wavelength
crest to crest distance (top of wave)
speed
distance crest travels per unit time
period
time it takes a crest to travel one wavelength
freqency
number of crests passing a fixed location per time
constructive interference
occurs when two waves combine to make a wave with higher amplitude
destructive interference
occurs when two waves combine to make a wave with lower amplitude (cancel each other out)
What do waves propagate?
energy not mass
What determines wave speed?
wavelength and bottom depth
waves with longer wavelenth
travel faster than waves with shorter wavelength
waves traveling in deep water
travel faster than waves in shallow water
in very deep water, wave speed is aa function of – only
wavelength
in very shallow water, wave speed depends on — only
bottom depth
deep water waves
- bottom depth is more than 1/2 wavelength
- speed is a function of wavelength only
- longer wavelengths travel faster
shallow water waves
- bottom depth is less than 1/2 wavelength
- speed is a function of bottom depth only
- waves in shallow water travel slower
wave dispersion
- self sorting of deep water waves leaving a storm region
- occurs because longer wavelengths travel faster
wave refraction
bending of shallow water wave front due to change in bottom depth
longshore sediment transport
occurs when waves strike the beach at an angle
breaking waves
waves slow down as they feel the bottom depth but the waves behind are still traveling quickly so it causes crowding
summer beach conditions
gentle waves push offshore sandbar shoreward to create wide and gently sloping sandy beach
winter beach conditions
storm waves push sand off the beach into offshore sandbar resulting in rocky winter beach
rip currents
- accelerated jets of water
- narrow, seldom wider than 10 meters
What should you do if you’re caught in rip current?
swim parallel to shore for 10-20 meters
wave height of wind generated waves depends on
- wind speed
- duration of wind event
- fetch
wind speed
sets the upper possible limit on wave height
duration of wind event
modulates the upper possible limit on wave height
fetch
- depends on size of storm
- distance over which wind can blow without obstruction
internal waves
- travel along density discontinuities in the ocean interior
- atmosphere is low density fluid, ocean is high density
- slow motion