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wind
warm, less dense air rises
cool, dense air sinks
large circular patterns of moving air
movement of air cause by differences in air pressure
convection cells
warm, less dense air rises
cool, dense air sinks
large, circular patterns of moving air
movement of air caused by differences in air pressure
Coriolis Effect
bands of high and low pressure found about every 30 degrees of latitude
the curving of a path of a moving object from an otherwise straight path due to Earths rotation
winds that blow from east to west between 60 and 90 degrees latitude in both hemispheres
narrow belts of strong winds that blow in the upper troposphere
Polar Easterlies
bands of high and low pressure found about every 30 degrees of latitude
the curving of a path of a moving object from an otherwise straight path due to Earth's rotation
winds that blow from east to west between 60 and 90 degrees latitude
narrow belts of strong winds that blow in the upper troposphere
westerlies
winds that blow from west to east between 30 and 60 degrees latitude in both hemishpheres
winds that blow from 30 degrees latitude almost to the equator in both hemispheres
area around the equator where there is very little wind ("dull", "sluggish")
area around 30 degrees latitude in both hemispheres where there is very little wind
horse latitudes
winds that blow from west to east between 30 and 60 degrees latitude in both hemispheres
winds that blow from 30 degrees latitude almost to the equator in both hemispheres
area around the equator where there is very little wind ("dull", "sluggish")
area around 30 degrees latitude in both hemispheres where there is very little wind
trade winds
winds that blow from west to east between 30 and 60 degrees latitude in both hemispheres
winds that blow from 30 degrees latitude almost to the equator in both hemispheres
area around the equator where there is very little wind ("dull", "sluggish")
area around 30 degrees where there is very little wind
doldrums
winds that blow from west to east between 30 and 60 degrees latitude in both hemispheres
winds that blow from 30 degrees latitude almost to the equator in both hemishperes
area around the equator where there is very little wind ("dull", "sluggish")
area around 30 degrees latitude where there is very little wind
Bands of pressure found every 30 degrees latitude
Coriolis Effect
Pressure Belts
Convection Cells
Winds
Which is NOT a type of global wind?
Polar Easterlies
Prevailing Westerlies
Doldrums
Antarctic Winds
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