Ocean Surface Current Slides 1&2
Nemo Slides 3&4
Currents Patterns Slides 5&6
Deep Currents Slide 7
Waves Slides 8&9
100

Streamlike movements of water that occur at or near the surface of the ocean are called

Surface Currents.

100

does flow along 

the East Coast of Australia, obviously

The East Australian Current

100

 When currents meet landforms, they change direction.

 continental deflection.

100

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

Deep

100

can travel through air, water, or solids, but it can't travel through a vacuum.

Sound

200

flow like rivers in distinct patterns around the Earth. 



Surface currents

200

transports a staggering 40 million cubic meters of water southward each second.

The East Australian Current

200

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

Warm water currents

200

Ocean water gets denser when it becomes saltier or gets 

colder.

200

is defined as a transfer of energy.

A wave

300

Surface currents are controlled by four 

factors: 

global winds, the Coriolis effect, 

continental deflections, and the water 

temperature.

300

The current is almost

100 km wide, and more than 1.5 km deep

300

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

 Coldwater

300

 and some cool coastal areas year-round.

Some surface currents warm

300

waves form because of friction between the wind and the surface of the water. Waves move in a circular pattern.

Ocean

400

is one of the 

longest surface currents transport 25 

times more water than all of the rivers in 

the world and flows from Florida to Iceland!

The Gulf Stream

400

The East Australian Current does flow

southward from the Great Barrier 

Reef.

400

currents greatly affect the climate in many parts of the world.

Surface

400

currents create cooler climates in coastal areas that would be much warmer (San Francisco).

Cold-water

400

is the distance between two adjust crests or troughs.

A wavelength

500

currents in the Northern Hemisphere turn clockwise while currents in the Southern Hemisphere turn counterclockwise.

Coriolis Effect

500

 Speeds in the core of the EAC are among the strongest in the South Pacific,

up to 4.5 mph an hour.

500

currents create warmer climates in coastal areas that would otherwise be much cooler

Warm-water

500

Deep currents are mainly controlled by

 increases in water density.

500

are waves that require a medium

Mechanical waves