Why do waves not approach a straight uniform coastline
It is very rare for waves to approach a straight uniform coastkunr, as most coastlines have a variety of bays, beaches and headlands
Because of these features along the coastline what happens the sea water
Because of these features, the depth of sea water sound a coast varies and as a wave approaches a coast its progress is modified due to friction from the sea bed
When does the base of the wave start to feel friction
When sea depth is 1/2 the approaching waves wavelength, shown in s2 on my diagram
What happens the wave around the shallower headland
The base of this wave around the shallower headland slows down whilst the other sections of the wave continue undisturbed
What is the result of different sections of the wave flowing at different speeds
The wavefront has now been modified and it no longer runs parallel to the coastline
What then happens when the wave continues to approach the coast
As the wave continues to approach the coast, shown in s3 on my diagram the wave starts to become refracted around the headland and this results in the wave energy being concentrated around the headland
What happens the wave right along at the headland
At s4 in my diagram the wave section along the headland has reached the crustal point of depth
What is the critical point of depth
The critical point of depth is less than 1/20th of the wavelength and as such has ‘broke’ onto the headland and released its energy there
What happens the remaining section of the same wave
The remaining section of the same wave continues onto the Bay Area
What helps show how energy released is not uniform along a coast
Orthogonals
What are orthoganals
Lines drain at right angles to the wave crests that help show how energy released is not uniform along a coast
What does wave refraction result in
Results in concentrated wave energy on headlands and energy dissipation into bay areas, creating local differences and making Hugh energy and low energy sections on the same coastline
What are local examples of wave refraction
Portrush, NI
Here the prevailing westerly winds drive the waves to refraction around Ramore Head and dissipate their energy into the East and West strand areas on either side