Re: Conclue - can you explain this please
Posted by
Conclue on 4/1/2011, 3:15 pm
Hey Jac-
I'm not quite sure that I can, however after reading the blog post and recalling what I remember from class is that they would prolly result in the midlevels from extreme instability where the air is clashing with different density functions with pressure.. We know barotroppic and baroclinic systems are different. I would imagine that these two clashing airmasses may have triggered them at the midlevels? it seems where they occurred would sit well with where density gradients would be the most different pressure gradients.
Also,I think of your note in the other thread about how we could get alot of early storm systems from frontocyclogensis (is that what we call it? LOL) with tropical systems. Maybe the current tropical airmass there isn't "unstable" enough yet to form storms this early on in the game, but yeild different things that may only occur sporadically. That MCV over Tallahasse was amazing on radar. Everyone at school was in there looking at it in the map room. I mean this thing had a line of storms that looked like a cold and warm front and was progogating as such.
Thanks for pointing this out. I've been *SO* busy with the school stuff theres little time for the "real time stuff". So annoying.
Man just talking about all this stuff reminds me of my passion for it. (I'm debating back in forth in my head if I want to puruse an Enviornmental MS to compete within job markets for climate related work.) |
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