It’s now March which means we will soon begin the transition from winter weather to the stormy weather. We ran a story Monday on The Morning Show about a microburst that happened in Arizona. I gave a brief explanation of what it is. It’s basically a strong blast of wind from a thunderstorm that’s confined to a relatively small area. But here on Ken’s Korner, I want to give a bit more detail.
These things set up when thunderstorms are getting to their maturity state. The maturity stage is when storms are raining their hardest and at their strongest. In side the rain cloud, there is a lot of cooling taking place. As a note, cold air is more dense than warm air. So, with all those cooling, the air is getting heavier, so to speak. Eventually it gets too heavy and it “falls” out of the cloudy. It “falls” at a high rate of speed and can often be confused with a tornado. The “fall” is also part of the storm downdraft. When this air hits the surface, it spreads out in all directions. This lasts for several seconds. I have attached some pictures to illustrate.
There are two types of microbursts; wet and dry. Dry has no rain and wet is with rain. Microbursts will knock over trees and cause other damage. It’s also very dangerous to airplanes. If a plane gets caught in one, the microburst disrupts the flow over the wings which eliminates the lift. This causes the plan to go down and possibly crash.
![]()
They happen all the time, and could happen as we get into the summer season. Stay safe!
Posted under Uncategorized
This post was written by Ken on March 1, 2010
No Comments






Example of rotation.
Nor’easter Blizzard of 1978.

