Pressure Gradient Force
Air traveling from a high pressure area to a low pressure area. Amount of difference determines strength of wind
Coriolis forces
Based on earth’s rotation. Moves air to the right in northern hemisphere, and left in southern
Buy- ballot’s law
In north hemi, air flows clockwise around a high and counter clock wise around a low
Friction
Surface of the earth exerts a frictional drag on the air flowing just above it and causes the wind to slow somewhat and change direction slightly
Veering
Wind change in a clockwise direction
Backing
Wind change in a counterclockwise direction
At 3000’
Fiction is not a factor
Wind speed doubles
Wind veers 30° to become parallel to isobars