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This jet stream brings cold weather conditions in the Northern Hemisphere.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
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.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
Winds that blow off the land onto the water. This is caused by temperatures over the water being warmer than temperatures over the land.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
Winds that blow over short distances.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
A quick moving band of air that moves west to east high up in the atmosphere.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
This is where water rises from deep in the bottom of the ocean up to the surface bringing nutrients up from the ocean floor.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
Winds that blow between 0 degrees and 30 degrees latitude. This is cool air that flows back to the equator and they blow from east to west.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
This area begins at 23 degrees and extends to 67 degrees. This area experiences many different temperatures throughout the year along with all 4 seasons.
Jet Stream
Trade Winds
Temperate Region
Upwelling
Local Winds
Polar Jet Stream
Land Breeze
Coriolis Effect
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