The weight of the air above an object exerts a force per unit
area upon that object and this force is called pressure. Variations
in pressure lead to the development of winds, which in turn
influence our daily weather.
The purpose of this module is to introduce pressure, how it
changes with height and the importance of high and low pressure
systems. In addition, this module introduces the pressure gradient
and Coriolis forces and their role in generating wind.
Local wind systems such as land breezes and sea breezes will
also be introduced. The Forces and Winds module has been organized
into the following sections:
Introduces pressure, associated characteristics, and high and
low pressure centers. Pressure Gradient Force
A net force that is directed from high to low pressure.
Coriolis Force
The apparent deflection of objects due to the earth's rotation.
Geostrophic Wind
Winds that result from a balance of Coriolis and pressure gradient
forces.
Gradient Wind
Winds that blow parallel to isobars, but are not geostrophic.
Friction
How friction near the surface affects geostrophic and gradient
wind.
Boundary Layer Wind
More on how friction affects low level winds.
Sea Breezes
Atmospheric conditions that lead to the development of sea breezes.
Land Breezes
Atmospheric conditions that lead to the development of land
breezes.
Acknowledgments
Those who contributed to the development of this module
