Rich Thompson
EF3
I know Monday looks interesting in a conditional sense (i.e., given storms), but I think the "dry" model forecasts could be legitimate. The moist layer looks to be a little on the shallow side E of the dryline Monday in OK, and the mixed layer W of the dryline extends only up to 700-600 mb. This doesn't look like a strong dryline circulation setup to me, and since the ascent along the dryline tends to peak near the height of the moist layer depth on the moist side of the dryline, that peak ascent will be well below the LFC height. The rather quick veering of winds to SW-WSW above 850 mb also suggests that parcels will "detrain" from the narrow dryline updraft zone before the parcels can rise enough to reach the LFC. This problem is reflected in the NAM not triggering convection, likely because there's not quite enough moistening for the BMJ scheme. The same argument could also apply to Tuesday along the dryline.
All of the nifty sounding analogs from SHARPpy won't mean squat without an actual storm. This one may require some sort of ejecting wave that hasn't been identified yet, or a little stronger mesoscale ascent than is currently expected. Still 48-72 hrs to go, so much can change...
All of the nifty sounding analogs from SHARPpy won't mean squat without an actual storm. This one may require some sort of ejecting wave that hasn't been identified yet, or a little stronger mesoscale ascent than is currently expected. Still 48-72 hrs to go, so much can change...