DON'T PANIC!!!!! You don't have to understand the following charts. I will explain them to you.
Call me Bill Nye the Weather Guy, because I'm about to take you on a crash course in basic storm prediction. Feel free to take notes :-)
One of the first things meteorologists or "junior meteorologists" such as ourselves look for when determining the potential for severe weather is the upper level wind patterns. To put it simply, the best conditions for severe storms occur in the presence of an upper level trough, and this trough has nothing to do with horses [/dry science joke]. A trough is a kind of upper level flow that moves from the southwest to the northeast...or sometimes, even south to north. You can tell which way the wind is going by the wind barbs on the weather map, which consist of a line with diagonal extensions on the end. The wind direction is always FROM the small extensions at the end TO the center. For instance, the following barb...
...represents wind FROM the northeast TO the southwest. The speed of the wind is represented by the number and size of the little barb extensions at the end (but don't worry about that). So when meteorologists plot this information on an upper level map using colors to represent wind speed, the result looks like this...
Ooooo...pretty...
By the way, The lines on the map represent areas of constant barometric pressure, which almost always line up parallel to the wind direction. And which way is the wind going over the plains, class? GOOD! Southwest to Northeast! Cookies for everyone!
So now you know what you're looking at. A large trough/jetstream across the Rockies with some high speed wind making it's way as far as Texas, Kansas, and Nebraska. This is one forecast model's output for 00Z Monday (Z stands for Zulu Time. I heart the word "Zulu")
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