Ocean Surface Currents (Slides 1 &2
Nemo (Slides 3 &4
currents patterns (slides 5&6)
deep currents slide 7
waves slides 8&9
100

streamlike movements near the surface of a ocean is called..

surface currents 

100

The East Australian Current does flow along 

the East coast of 

austrailia

100

If Earth's surface were covered only with        , currents would travel in a fixed pattern across the Earth, but Earth’s surface is not covered only with     .

water

100

                                  are stream-like movements of ocean water far below the ocean surface.

deep currents

100

Waves are made of two main components -      and    

crests, troughs

200

surface currents are controlled by four factors

water temperture,global winds,the colioris effect,conential defections.

200

And it 

does flow     from the Great Barrier 

Reef.

southward

200

When currents meet landforms, they change        .

direction

200

Deep currents are not controlled by wind or                

the coriolis effect

200

A       is the highest point

crest 

300

global winds blowing across the earths surface create 

surface currents 

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Speeds in the core of the EAC are 

among the strongest in the South Pacific, up 

to 4.5 mph an hour.

4.5 mph

300

This is known as continental          .

deflection

300

Deep currents are mainly controlled by increases in water          .

density 

300

the      is the lowest point.

trough

400

the rotation of the earth causes 

surface currents

400

But actually the real East Australian Current is much                    than in the movie

bigger and much wilder

400

Warm water currents begin near the             and carry warm water to the other parts of the ocean.                                                                                      

equator

400

                     and salinity affect the density of ocean water.

temperture

400

A           is the distance between two adjust crests or troughs

wavelength 

500

Because of the Coriolis Effect, currents in the Northern                                 Hemisphere turn clockwise 

 Coriolis Effect

500

just not so conducive to

surfing.

500

Cold water currents begin closer to the         and carry cool water to other parts of the ocean.                                                                                            

poles

500

Ocean water gets           when it becomes saltier or gets colder.

denser

500

Wave height is the         distance between a waves crest and its trough.

vertical

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