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Published byTamsin Thompson Modified over 9 years ago
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Chapter 21- 2,3 OCEAN WAVES
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Wave Disturbance of energy transmitted through a medium Medium- solid- liquid-gas Crest-highest point in a wave Trough-lowest point in a wave
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waves Wave height- vertical distance between crest and trough Wavelength-horizontal distance between two crests
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Wave Energy Wind- caused by the uneven heating of earths surface Wind transfers energy to the ocean and forms waves
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Water movement Waves move over the ocean-only the energy of the wave moves-NOT the water.
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Wave size Three factors Speed of wind Length of time wind blows Fetch – distance wind blows across the water
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swell Group of long rolling waves similar in size
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whitecaps When the wind blows the crest off waves whitecaps form
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Waves and the coastline Breakers- foamy masses of water that wash onto the coast Refraction-bending of waves toward the coast Undertow-water carried to the beach by breaking waves is pulled back by gravity
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Rip current Form when water from large breakers returns to the ocean through channels that cut through underwater sandbars
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Longshore currents Form when waves approach the beach at an angle
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Tsunami Most destructive wave Not powered by wind Cause Earthquakes underwater Volcanic eruptions
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Tides- lesson 3 Cause of tides The gravitational pull between the moon and earth Two high and two low tides per day in most areas
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Tide Behavior Spring tides- new and full moon Earth-sun-moon are lined up RESULT- higher high tides and lower low tides
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Neap Tides First and third quarter, moon and sun at right angles to earth Daily tides are small
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Tidal variation Tidal patterns are influenced by: Size Shape Depth Location OF the OCEAN BASIN
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Tidal Oscillations Slow rocking motions of the ocean water that occur as the tidal bulges move around ocean basins.
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Tidal currents Flowing water toward the coast is called flood tide Ebb tides flow toward the ocean
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