GEO 230 EXAM 3 Flashcards
Waves are the manifestation of the translation of energy through a medium
The medium does not travel in the direction of the wave
Ocean waves are orbital waves and combine elements of 2 fundamental wave types
Longitudinal (push-pull)
Transverse (side to side)
Crest
High point of wave
Trough
Low point of wave
Stillwater (or mean water) level
Relaxed level of water surface
Wave height (H)
Crest to trough distance
Amplitude (A)
H/2
Wavelength (L)
Crest to crest distance
Wave steepness
H/L
Period (T)
Time it takes for one wavelength to pass a reference point in a given time (T= 1/F)
Frequency (F)
of wave crests to pass a reference point in a given time (F=1/T)
Wavespeed (C)
1/period = 1/T
Progressive waves
Moves across surface
Standing waves
Stay in one place
Wave motion
Path of water molecule
Deep water waves
If water depth (d) > L/2
Waves have no interference with ocean bottom
Wave Speed-C
For deeper waves, the longer the wavelength, the faster the wave C= 1.25 square root of L
Shallow-water waves
If water depth d
Transitional (intermediate) waves
If what we depth L/2
Light winds
Capillary waves
Max wavelength 1.7 cm
Rounded crests, v shaped troughs
Disappear quickly when wind stops
Increasing wind
Larger waves
What causes waves?
Movement of air (wind)-ocean waves
Mass movement into ocean- splash waves
Sea floor movement (earthquake)-tsunami
Gravitational pull of the moon & sun- tides
Smooth sine waves
Pointed crests; round troughs
Breaking waves
Deep water waves
Waves form white caps (breaks) when they get too steep