Land and sea breezes (local winds) are typical of such winds. Because water heats up and cools down more slowly than does dry land, the air along a shoreline is alternately warmer over the water and cooler over the land, and vice versa. These differences account for the fact that winds tend to blow offshore during the evening and on-shore during the day.
pressure.
Local winds
doldrums
Local geographic features.
Globally.
Atmospheric pressure differences!
Winds are produced when there is a difference in atmospheric pressure. Air moves from areas of high pressure in the atmosphere to areas of low pressure. This movement of air is experienced as wind.
100 Tradewinds Cheetah 594 were produced in 1968
yes
lateral loading. such as the forces produced by high winds
dustbowl
The differing air temperatures cause the winds.