Weather Notebook
Bryan Yeaton
 


 
Why Spring?
Thu May 06, 2004

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Have you ever wondered why all the really severe weather in the Midwest United States seems to occur in the spring? Why not the summer? The answer has to do with a clashing of the Titans. Hi, I'm Bryan Yeaton, and this is The Weather Notebook.

In the summer, air masses rolling out of Canada have warmed sufficiently that, for the most part, they are not all that different from the air they run into in the United States. Same thing in the winter.

But in the spring, the air over the plains states is starting to warm as the suns creeps northward on its trek into summer. This air can also be pretty humid, as influenced by the Gulf of Mexico. But up in Canada, summer is still a distant dream -- winter retains its cold hold on our northern neighbor. The bigger the difference between the two, the bigger the clash.

Cold air is denser than warm air, so a charging cold front will burrow underneath the warm air, and force it upwards -- sometimes at great velocity. As this air drives higher, it cools and eventually reaches its dewpoint where it condenses into cloud. If the upward push fizzles out, the clouds will appear as puffy, fair-weather cumulus clouds. But if the energy keeps cranking, these friendly clouds will build through cumulus congestus and cumulus castellanus, and into cumulonimbus -- the towering thunderheads.

During tornado formation, powerful updrafts and downdrafts set spinning in a horizontal column of air. Eventually, this column gets lifted upright and becomes the mesocyclone. If conditions are right, a concentrated circulation reaches from the middle of the "meso" to the ground -- the tornado.

There are other related atmospheric conditions and air masses that can produce severe weather, but it seems that the most violent storms occur when giant weather systems collide.

You can revisit any of our shows online at www.weathernotebook.org. We are supported by the National Science Foundation and Subaru -- Driven By What's Inside. We are produced by the Mount Washington Observatory.




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