This is the latest edition of Weather whys, a series of posts by Braniff Davis explaining the science behind weather phenomenon affecting Texas.
Now that we’ve enjoyed a few sunny days after an extremely wet May and early June, we wanted to tackle a few ‘weather whys’ questions people have asked, either on Facebook, Twitter, or in the blog comments. One reader asked why the weather system last week, which dumped so much rain on the region, was not considered a ‘tropical system.’ After all the system spun counter-clockwise, and had the satellite appearance of a tropical cyclone.

The answer has to do with how and where different low pressure cyclones form. Pressure, and how it influences weather systems, is vexing. Often, it was the most challenging concept for my students to grasp in my introduction to meteorology classes. We could probably do a 50-part series on the science behind it, called cyclogenesis. For now, we’ll spare you that and only focus on the large, synoptic scale cyclones that influence our weather.
EXTRATROPICAL VS. TROPICAL CYCLONES
