Andrew Herron
EF3
So you're saying the 34F along the coast isn't going to dramatically affect the storm? Why is that the case?
Hate to say it, but GFS has been trending worse and worse every run. Hope it's flat out wrong and NAM is more in the ballpark otherwise it may just turn into a typical cold front squall line, all too common around these parts.
Some facets of Thursday have the look of a classic severe weather outbreak for this region, especially if one goes with the NAM, although details are going to change over the next 84 hrs, so I'm not sure how this is going to evolve.
Thanks for your input, I know last night in chat we were discussing the probability that convection will be restricted to the cold front and pretty quickly forced into a line before making it's way to Illinois. I am not trying to "wishcast" only but I am looking for any signals of prefrontal convection, or even cells along the front keeping tornadic potential as they move across the Mississpi because I don't have a realistic shot of making it into Eastern Iowa by 1pm.I agree that there are still rather significant surface flow differences between the 00z/07 GFS and the 00z/07 and 12z/07 NAM. All of the major models are showing a more neutral orientation to the main upper-level energy, though they seem to be locking on to a solution whereby strong vort max approaches eastern IA/MO by peak heating, with sufficient destabilization and a deepening low.
I really believe, as mentioned yesterday, that the evolution of any convection Wednesday evening (or lack thereof) will be key to determining the extent of destabilization on Thursday across the warm sector, as well as the placement of residual boundaries and, ultimately, perhaps the northward extend of warm frontal placement.
There are some subtle differences on timing and placement of the surface low and cold front too. Surface flow on the 12z/07 NAM is somewhat anemic proximal to the warm front itself, and, although stronger, oriented more parallel to the forcing further down into SE MO, SW IL and points southward. Surface flow patterns on the NAM had been suggesting the possibility of a pre-frontal wind shift, which could ignite discrete convection in the warm sector before the main line of forcing ignites a linear mode prior to the main frontal passage, and this 'may' be what's being reflected in simulated reflectivity precip signatures on the recent runs. As of right now, if the NAM remains the more correct solution, discrete supercell and tornadic potential looks to be maximized in a narrow corridor from EC IA/NW or WC IL into S WI - I expect to see further changes over the next 48 hrs.