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This is where water rises from deep in the bottom of the ocean up to the surface bringing nutrients up from the ocean floor.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
Winds that blow steadily from specific directions over long distances.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
Winds that blow off the land onto the water. This is caused by temperatures over the water being warmer than temperatures over the land.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
A place where there is little to no wind near the equator.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
The mixing motion of liquids and gases that are different temperatures.The primary way that energy is transferred in the ocean and atmosphere.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
Winds that blow over short distances.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
This jet stream brings cold weather conditions in the Northern Hemisphere.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
Winds do not travel in a straight line. Winds curve from East to West as they travel from the North Pole to the Equator. They curve or twist as a result of Earth's daily rotation.
Polar Jet Stream
Local Winds
Convection
Coriolis Effect
Global Winds
Doldrums
Land Breeze
Upwelling
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