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1
Global Winds
Wind current on a global scale.
Mr. Fetchs Earth Science Classroom
2
Global Temperature Patterns
The suns rays are weaker near the equator
causing less warming. The air here is cool.
The suns rays are stronger near the equator
causing more warming. The air here is warm.
Mr. Fetchs Earth Science Classroom
3
Global Winds
Hadley Cells.
Mr. Fetchs Earth Science Classroom
4
The Coriolis Effect
Mr. Fetchs Earth Science Classroom
5
Global Winds
NorthernHemisphere
SouthernHemisphere
Mr. Fetchs Earth Science Classroom
6
Global Winds
Remember, winds are named from where they come.
Polar Easterlies- From 90N to 60N- Deflected
to right
60N
Prevailing Westerlies- From 30N to 60N-
Deflected to right
30N
Easterly Trade Winds- From 30N to O-
Deflected to right
0
Doldrums
Easterly Trade Winds- From 30S to 0-
Deflected to left
30S
Prevailing Westerlies- From 30S to 60S-
Deflected to left
60S
Polar Easterlies- From 90S to 60S- Deflected
to left
Mr. Fetchs Earth Science Classroom