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Wind Energy Resources: Global Winds

How the Coriolis Force Affects Global Winds
Global Circulation
The wind rises from the equator and moves north and south in the higher layers of the atmosphere.
Around 30° latitude in both hemispheres the Coriolis force prevents the air from moving much farther. At this latitude there is a high pressure area, as the air begins sinking down again.
As the wind rises from the equator there will be a low pressure area close to ground level attracting winds from the North and South.
At the Poles, there will be high pressure due to the cooling of the air.
Keeping in mind the bending force of the Coriolis force, we thus have the following general results for the prevailing wind direction:

Prevailing Wind Directions














The size of the atmosphere is grossly exaggerated in the picture above (which was made on a photograph from the NASA GOES-8 satellite). In reality the atmosphere is only 10 km thick, i.e. 1/1200 of the diameter of the globe. That part of the atmosphere is more accurately known as the troposphere. This is where all of our weather (and the greenhouse effect) occurs.

The prevailing wind directions are important when siting wind turbines, since we obviously want to place them in the areas with least obstacles from the prevailing wind directions. Local geography, however, may influence the general results in the table above, cf. the following pages.



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© Copyright 2000 Soren Krohn. All rights reserved.
Updated 6 August 2000