A pressure gradient is how fast atmospheric pressure changes over distance. So, when pressure changes rapidly over a small distance, the pressure gradient force is large. Strong winds almost always result from large pressure gradients. Recently, southern Wisconsin has been under the influence of a weather pattern that has strong pressure gradients and strong winds.
The Coriolis force pulls the wind to the right so that in the Northern Hemisphere winds blow counterclockwise around low pressure systems and clockwise around high pressure ones. With your back to the wind, lower pressure is to the left.
What the wind is blowing over can also influence the wind speed. Over the open lakes, the wind will be faster than through a stand of trees, where it will be slowed by friction. In the presence of buildings, the air can be funneled between buildings and pick up speed.
During this time of the year, thunderstorms also can cause strong winds. Rain falling from a thunderstorm evaporates underneath the cloud, cooling the air beneath it. This cold heavy air plunges to the surface and “splashes” against the ground like a bucket of cold water. The air then rushes sideways resulting in strong winds.
These “microbursts” are capable of producing winds of more than 100 mph, causing significant damage while lasting for only five to 15 minutes.