Ocean Currents. Two Types of Currents 1.Surface Currents 2.Deep water currents- very slow.

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Presentation transcript:

Ocean Currents

Two Types of Currents 1.Surface Currents 2.Deep water currents- very slow

Surface Currents Move huge amounts of water Affect the upper 10% of the worlds oceans Move the shallow warm, low density waters Driven by wind

Surface currents

Source of energy Prevailing Winds Tradewinds- blow from the East  West Westerlies- blow from the West  East ** trade winds converge at the equator

Coriolis effect Earth’s rotates (west to east) Water moves slower than wind causes the water to bend in a 45 angle to the direction of the wind

Ekman Transport Describes the phenomenon of the movement of water relative to the wind by in a 45 direction. Ekman - a result of both the prevailing winds and the Coriolis effect. Transports water to 100 m.

Ocean Gyres The circular motion of currents in the ocean basins. Initiated by the Ekman spiral

The Antarctic Circumpolar Current AKA- West wind drift Driven by westerlies Biggest winds & biggest storms on the planet.

Western Boundary Currents Fastest Deepest Move warm water from the tropics to the poles Tend to form eddies Largest and fastest= Gulf Stream 2 nd largest and source of tuna= Kurashio (Japan) Eddy= small, temorary loops of swirling water.

Eastern Boundary Currents: Shallow Broad Slow Name them:

Transverse Currents Link western and eastern currents Move water from east to west Move water from west to east Examples include:

Importance of Surface Currents 1.Distribute Tropical Heat 2. Influence Weather and Climate Water stores heat- moderates coastal climate

Wind Induced Vertical Circulation Upwelling- the movement of deep ocean water up to the ocean surface. An upwelling event occurs when: Winds blow water away from the coast outward When two currents diverge Identify upwelling sites:

Importance of an Upwelling Brings nutrient rich waters to the surface Increases primary productivity- surface Increases oxygen in the water Increase in heterotrophic populations

Downwelling The movement of surface waters downward to the deep waters. Carries oxygen rich water downward.

ENSO El Nino- an increase of temperatures in the surface waters of the tropical Western Pacific and of the coast of Equador and Peru. Caused by: Weak surface winds caused by a high pressure zone Effects: South America: Prevents the upwelling along the western coast of S. America Reduces fishing population Reduces guano production Destroys the economy World: Affects the tradewinds around the world Effects weather- droughts and torrential rains

Tides The rhythmic rising and falling of sea waters It is a Wave with the longest wave lengths Result from the gravitational pull of the moon and the sun.

Two high tides a day The earth completes a full rotation every 24 hrs The moon pulls upon the oceans creating a bulge( tide) Centrifical force causes the secon