downsouthman1 wrote:I think I kind of get that now after researching baroclinic zones. So, correct me if I'm wrong but, the system is essentially following a temperature gradient, for example 550 or so thickness layer, meaning that no matter where the storm goes along the baroclinic zone, the weather will be mainly constant, rain, then moisture being scoured as the cold, drier air intrudes.
You can't think of the different atmospheric features as being separate entities. There is a cause and effect for everything going on at any particular time. In this instance, it appears that the shortwave is riding along the low level baroclinic zone. This is generally to be expected as waves in the atmosphere tend to travel with the general flow of the jet stream. This jet usually forms above low level thermal gradients through the thermal wind relationship. This is highly simplified, of course.