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14.2 Ocean Movements Hydrosphere.

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Presentation on theme: "14.2 Ocean Movements Hydrosphere."— Presentation transcript:

1 14.2 Ocean Movements Hydrosphere

2 Learning Targets Define waves and explain their formation Describe what causes tides Describe how surface currents form and how they affect the world’s climate Describe the causes of deep currents Relate upwelling areas to the food chain

3 Surface Waves The largest surface waves form when the wind:
Is very strong Blows steadily for a long time Blows over a long distance How is wind formed? Waves on the ocean’s surface are caused by wind. What is the main cause of surface currents in the ocean? Wind What causes an ocean wave to break as it approaches the shore? The speed of the top of the wave is moving faster than the speed of the bottom of the wave.

4 Surface Waves Formed by wind Transfer energy from wind to water
Tsunamis are NOT formed by wind Transfer energy from wind to water Do not move much water Substances only bob up and down Waves break due to interactions with seafloor How is wind formed? Waves on the ocean’s surface are caused by wind. What is the main cause of surface currents in the ocean? Wind What causes an ocean wave to break as it approaches the shore? The speed of the top of the wave is moving faster than the speed of the bottom of the wave.

5 Parts of a wave

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7 Tides Daily rise and fall of sea level
Caused by gravitational pull of Moon and Sun High tide every 12 hours 25 minutes

8 Daily Tide Patterns High Tides – Two water bulges on opposite sides of the Earth aligned with the Moon Low Tides form between the two high tides Earth rotates beneath Moon where a single spot has 2 high & low tides What causes the daily changes in the tides? Gravitational pull form the moon and sun.

9 Monthly Tide Patterns Neap tide Spring tide Weak high and low tides
Moon, Sun, Earth NOT in a line Spring tide Strong high and low tides Moon, Sun, Earth in a line Has NOTHING to do with the seasons When the sun, moon, and earth are all aligned, the high tide will be higher than normal and called spring tide. When the sun, moon, and earth are not aligned but positioned at a 90 degree angle to each other, the high tide will be lower than normal and called neap tide.

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12 Surface Currents Surface currents created by three things:
Global wind patterns Rotation of the Earth Shape of the ocean basins Coriolis Effect Surface currents play a major role in regulating earth’s climate.

13 Surface Currents - Coriolis Effect
Blow in the same directions Unequal heating of Earth by the Sun More solar radiation strikes equator than polar regions Coriolis effect describes how Earth’s rotation steers winds and surface ocean currents. The objects are actually moving straight, but the Earth is rotating beneath them Surface currents play a major role in regulating earth’s climate.

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18 Surface Currents – Shape of Ocean Basins
When surface current collides with land, current must change directions Topography Landmasses and mid-ocean ridges Surface currents play a major role in regulating earth’s climate.

19 Surface Currents Huge effect on global climate patterns Gulf Stream
Sends warm water north and cold water south Gulf Stream Warm waters raise temperatures in North Sea, which raises temperatures in London Surface currents play a major role in regulating earth’s climate.

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22 Deep Currents Caused by density differences Regulates temperatures
Cold water sinks Salty water sinks Regulates temperatures Mixes water between oceans Giant ocean conveyor system Temperature & Salinity When compared to the rest of the ocean, the water at the bottom of the ocean is colder and more dense. What is the main cause of deep currents in the ocean? Differences in the density of ocean water.

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25 Downwelling Very Cold & High Salinity
Surface currents move water into the space vacated at the surface where dense water sank Cold nutrient rich waters can be brought to the surface in an upwelling.

26 Upwelling Deep water rises to the surface Promotes biodiversity
Brings nutrients up to surface Nutrient support the growth of plankton – base of food web Cold nutrient rich waters can be brought to the surface in an upwelling.

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