Fronts as described in the “Bergen school” by Vilhelm Bjerknes are early conceptual models. Parameters typical for the changing of air masses were named and used by forecasters to recognize transition zones (fronts) between air masses. For nearly a century the method from the Bergen school is applied in the majority of weather rooms all over the world. Satellite information expressed how right Bjerknes was in his CM thinking, but this information showed also that fronts can have a much more complicated structure and live cycle Bjerknes could imagine.
In SatManu eight different types of warm- and cold fronts were recognized and described.
In this lecture we concentrate on warm- and cold fronts and show how we can analyze them with help of CM thinking.Go to Webcast...
Filed under Keywords:
fronts, cold front, warm front, frontal theory