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Waves, Beaches and Coastal Erosion. 1. Tidal forces associated with Moon. Tidal forces associated with Sun and Moon. High tide stays aligned with moon but Earth rotates, yielding 2 high and 2 low tides each day. Tidal forces associated with Sun and Moon.
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1 Tidal forces associated with Moon
Tidal forces associated with Sun and Moon High tide stays aligned with moon but Earth rotates, yielding 2 high and 2 low tides each day.
Tidal forces associated with Sun and Moon Neap tides: Sun and Moon tides are out of phase Spring tides: Two tides are in phase-- High tide will be higher than usual Tides are cyclical floods
Tidal Ranges influenced by local conditions and bathymetry Bays tend to focus the water and create larger ranges Organisms are stratified based on tidal zone
Mean sea level is the average height of the sea… Relative to what? When? High or low tide? Measured with tide gauges 2) Sea Level: What and When?
Eustatic Sea Level Changes “Eustatic” refers to changes related to amount of water in the oceans
Wave Energy Doubling wave height quadruples energy: Ew = 0.125rgH2L where: Ew = energy of wave r = water density (g/cm3; close to 1) g = acceleration of gravity (9.8 m/sec2) H = wave height (m) L = wavelength (m)
Passive continental margin Submarine canyons Deep-sea fan Coastal plain Abyssal plain Continental shelf Continental slope Continental crust Oceanic crust Mantle Continental rise
5) Waves approaching the shore at an angle cause a longshore current. Path of sand particles Rip current Path of water particles Longshore current Longshore drift results from movement of sand particles by swash and backwash.
The beach is a “river of sand” Sand will move in this direction
Offshore sand bars migrate to beach during summer Winter storms remove beach sand to deeper water Hurricanes result in summer beach sand loss 8) Sand Supply/Loss
Chandeleur Islands Before (above) and after (below) Hurricane Katrina
Headlands erode from wave action Creates caves, arches, sea stacks 10) Sea Cliff Erosion
Coastal Erosion