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(c) McGraw Hill Ryerson 2007 11.2 Ocean Currents There are more than 20 major currents which move large amounts of water predictably around the oceans.

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Presentation on theme: "(c) McGraw Hill Ryerson 2007 11.2 Ocean Currents There are more than 20 major currents which move large amounts of water predictably around the oceans."— Presentation transcript:

1 (c) McGraw Hill Ryerson 2007 11.2 Ocean Currents There are more than 20 major currents which move large amounts of water predictably around the oceans.  Currents move large quantities of water, minerals, solar energy, oxygen and carbon dioxide, plankton and fish.  Currents are caused and driven by water density and salt content, the wind, the spin of Earth, coastlines and the moon.  Largest current is the Antarctic Circumpolar Current in the Southern Ocean, at 24 000 km long See page 414 - 416

2 Ocean Currents Ocean currents are either  Surface currents (0 - 200 m)  Deep water currents (200 m and deeper) (c) McGraw Hill Ryerson 2007

3 What Makes Surface Currents Move? Wind  As air warms from solar energy, it rises, and cooler air rushes to replace it. This creates wind.  As the wind passes along the surface of the water, it bumps the water molecules and moves them along in the same direction. Spin of the Earth  Earth spins from West to East (counter clockwise)  The Coriolis effect deflects winds and currents to the right/East in the Northern hemisphere (opposite in the Southern hemisphere) Shape of continents  Currents move through the oceans and around the continents like rocks in a stream. See page 416 - 417

4 (c) McGraw Hill Ryerson 2007 What Makes Deep Currents Move? Water temperature  Like air, warm water rises, and cool water falls  Density current = cool, dense water moving on an ocean floor.  Three layers of water dependent on temperature:  Surface: 0 - 200 m, warmest  Thermocline: 200 m - 1 km, rapidly cools  Deep water: 1 km and deeper, just above freezing See page 418 - 420

5 What Makes Deep Currents Move? Water salinity  Adding fresh water decreases salinity  Evaporation and freezing increases salinity  Densest ocean waters at the poles  Upwelling occurs when nutrient-rich cold water finally moves up to the surface (c) McGraw Hill Ryerson 2007

6 Ocean Waves and Their Effect on Shaping Land Most waves are created by wind. In open ocean, waves are called swells.  Swells “break” in shallow water, show characteristic curl. The largest waves are tsunamis, caused by undersea earthquakes, landslides or volcanic eruptions. See page 421

7 Ocean Waves and Their Effect on Shaping Land Waves erode coastal areas based on the force of the waves, and the composition of the shoreline.  Headlands made up of harder rock, and erode less, but absorb most wave force.  Bays occur between headlands, are generally calm.  Sea stacks are extra-hard rock left behind from eroded headlands. (c) McGraw Hill Ryerson 2007

8 Tides Tides are caused by gravities of Earth and the Moon.  High tides occur where the Moon is closest to Earth (and opposite side)  Low tides occur at 90º to the high tides. (c) McGraw Hill Ryerson 2007

9 Tides Tidal range (difference between high and low) averages 3 m in BC. The Sun’s gravity, when lined up properly, can produce extreme tides.  These are called spring tides  When the Sun, Moon and Earth are not lined up, the tides are called neap tides. See page 423 - 424 Take the Section 11.2 Quiz


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