James Gustina
Supporter
The wild inconsistencies continue on the GFS further out, but a pretty deep, high-amplitude trough is progged to move out of the Four Corners and onto the Southern Plains on the 1st. A 90kt jet streak should eject through the northern Panhandle around 21Z with attendant diffluence region above it. A pretty sharp dryline has been shown to set up in the eastern panhandle and inch east during the day with one hell of a kinematic environment ahead of it. Deep-layer shear values have been looking to be around 45-50 knots with a solid 90 degree turn in the lowest levels of the atmosphere. A relatively broad sfc cyclone looks like it'll set up along the Oklahoma Panhandle/Kansas line and deepen throughout the day, with backed sfc winds wrapping towards the dryline. Really strong, southerly 850s across the warm sector throughout the day have been showing up pretty consistently which should help with the moisture issues to start.
Unfortunately, moisture still looks to be the biggest pitfall of this setup. "Just in time" moisture looks like a very good possibility, with 60F dews not reaching SW OK/SE TX PH until about 18Z which may in turn limit the thermodynamic environment if it's socked in with cloud cover. BUFKIT analysis has been showing a decent enlarging of the hodographs going between 18-21Z as the LLJ kicks up again towards the early evening with deep-layer shear ticking up as a result.
A lot of factors are still in free-fall such as the location of the instability axis and the overall quality of boundary layer moisture (mixing out is something to seriously worry about considering where it is).
Unfortunately, moisture still looks to be the biggest pitfall of this setup. "Just in time" moisture looks like a very good possibility, with 60F dews not reaching SW OK/SE TX PH until about 18Z which may in turn limit the thermodynamic environment if it's socked in with cloud cover. BUFKIT analysis has been showing a decent enlarging of the hodographs going between 18-21Z as the LLJ kicks up again towards the early evening with deep-layer shear ticking up as a result.
A lot of factors are still in free-fall such as the location of the instability axis and the overall quality of boundary layer moisture (mixing out is something to seriously worry about considering where it is).