Given gas prices and other extenuating factors, a modest jaunt toward southeast Kansas appears probable for myself and a fellow co-worker on Tuesday.
Excellent moisture return is forecasted by the 5/12 0z NAM, with mid-upper 60s surface dewpoints reaching the target area by Tuesday evening resulting in favorably low LCL heights. This seems attainable with moisture return well underway by early Monday morning, combined with upper 60s dewpoints already present at KBRO, and a few low-mid 60s values noted along the SE TX coastline.
A southwesterly mid-level speed max is evident from northern OK into eastern Kansas on Tuesday, beneath generally S or SSW surface flow, contributing to nearly 60kts of 0-6km shear. This magnitude of this cloud-layer shear combined with surface-based and mixed-layer parcels both yielding CAPE values > 2000 J/KG should be more than sufficient for supercells. Convective initiation would likely happen shortly after 21z as several subtle shortwaves eject northeastward from the Desert Southwest upper low, encroaching upon the unstable airmass and associated boundaries at play. The left exit region of a 90kt upper-level jet streak also positions itself across SE KS on Tuesday evening, and would provide an additional impetus for convective development.
Low-level speed shear is reasonable across SE KS given the presence of a better organized and significantly stronger LLJ than in areas further southwest. Surface winds out of the S or SSW are somewhat of a concern, however given the aforementioned strong speed shear, 0-1km SRH values still climb to above 200 m2/s2 by Tuesday evening. Forecasted hodographs across the area demonstrate a near 90 degree 'critical angle' as defined by Giuliano/Esterheld between the low-level storm inflow vector and the 0-0.5km shear vector. This certainly piques my interest as far as tornado potential goes, given the other parameters already discussed. See this hodograph:
http://beta.wxcaster.com/cgi-bin/parse_skewt_trace.cgi?model=NAM&fcsthr=048&STATIONID=KCNU
Another factor to like across SE KS is greater low-level instability as compared to SW OK/NW TX, likely owing to weaker boundary-layer mixing. Roughly 8-10% of the total surface based or mixed-layer CAPE is contained within the inflow region of the storm, co-located within a moderately sheared region.
One obvious downfall to the SE KS target will be 0-6km shear vectors only somewhat normal to the boundaries at play, as the cold front overtakes the dryline much faster in this area. I would hope that 10km storm-relative winds of around 50kts, as well as a backing wind profile above 650mb would tend to keep anvil seeding to a minimum, and lead to the likelihood of more discrete storms, especially given the relatively modest upper-level forcing.
This is the one day per month where my co-worker and I actually have the same day off and can chase together. Here's to hoping for a big 'Super Tuesday'!
-Chris