orangeblood wrote:Ntxw wrote:TeamPlayersBlue wrote:What are the dynamics behind the wintry weather for tuesday? I see an 850 low on the coast but thats it. Not really seeing it. Dont want to be bamboozled like the last time! I didnt think it would happen but i let the models convince me!
Something to note, i think the high will come into the Southern plains much quicker than the last NY big high we had. The GFS wants to hang onto it a bit too much in the N Plains i think.
Frontal upglide with some STJ noise. Set up you see more of the central and northern plains. Bubba notes it well. Race between how much moisture we see return and how quickly cold can undercut it
This front is what is referred to as an Ana Front. An ana front is a frontal boundary in which the main shield of clouds and precipitation is located behind the actual frontal boundary.This is because cold air located behind the front moves rapidly, pushing against the warm air out ahead of the front. Because cold air is more dense than warm air, the surging cold air causes the warm air to lift upward along the front - Upglide as Ntxw just mentioned. Therefore, clouds and precipitation that form end up inclined rearward with height due to the advancing cold air at the surface. And the more moisture we have out in front of this Ana Front, the better chances we have to see more precip
Here is a decent illustration
Beautiful. Exactly what i was looking for. So the dense air rushing in the main proponent here. So, for us Texas folk, we REALLY need the trough shift west for us. Especially SE Tx, the Ouachita shadow will be terrorizing us again.
Thanks so much guys!