Wave transformations Flashcards
wave shoaling
alteration of wave height and wave length/ celerity
wave refraction
change of wave celerity and direction
wave reflection
wave direction changes
from the beach or coastal structures
wave diffraction
waves bending round obstructions
wave attenuation
wave energy dissipation by sea bed friction and breaking
when waves move in shallower water (Shoaling)
- slow down (reduced celerity)
- become shorter (reduced wave length)
- become higher (increased wave height)
combining wave shoaling and refraction
wave refraction and shoaling occur simultaneously when a wave train travel from deep water to shallow water
Wave reflection (ideal)
if the solid boundary is smooth and vertical; the reflected wave has same phase and height travelling in the opposite direction
wave reflection coefficient
ratio between wave height and the incident wave height
Standing waves
form when reflected wave superimpose on incident wave
three regions can be defined when waves diffract
1) shadow region where diffraction takes place
2) short crested region where standing waves form due to wave reflection
3) undisturbed region of incident waves
in the shadow region - wave height dependant on:
incident wave height
incident wave length
incident wave angle
distance from the breakwater opening
gap between the breakwaters
length of the breakwaters
water level variations
- datum
- tide
- pressure surge
- wave set-up
- wind set-up
- long term trend