James Gustina
Supporter
This one kind of came out of left field and so far is all over the place in terms of the overall synoptic setup with relation to the fast moving cold front progged to come out of the Rockies/northern Plains.
Per the GFS, ECMWF and NAM12KM a rather deep, positively-tilted trough is progged to slowly dig out of the Four Corners region starting Wednesday morning. A lead impulse clears the Plains on Wednesday night with a second, stronger impulse and attendant jet streak huff onto the southern Plains late Thursday morning. The biggest concern as of right now is that the relative position of the trough is making it look very likely that low-level winds will be severely veered along the dryline in N TX/SW OK that extends from Hobart down through west of SPS, with modest surface winds out of the south/southeast at ~5 knots.
A strong fetch is already in place across the Plains currently, with dewpoints rising from the upper-40s to the low-60s across southern Oklahoma and northwest Texas as of this morning. While the SW 850s shouldn't notably hamper the moisture situation in the lowest 1km, the large amount of moisture combined with the meh shear profiles looks like it might be pointing to a more multicellular, messy precip convective mode should things stay the same.
With the unseasonably high moisture content going into Thursday, instability looks better than expected, excluding from the NAM4KM which places a very meager instability axis across SW OK. MLCAPE values between 1500 j/kg-2000 j/kg have been showing up consistently now with the GFS and NAM in NW TX near SPS.
The variability in dryline positioning/sharpness along with the cold front's motion is a rather notable problem along with the aforementioned VBV profile due to the trough's angle of approach. However, indications of rather sizable low-level shear have shown up in previous runs and depending on the trough's speed, I still think the possibility for a dryline supercell in N TX is very much alive.
Per the GFS, ECMWF and NAM12KM a rather deep, positively-tilted trough is progged to slowly dig out of the Four Corners region starting Wednesday morning. A lead impulse clears the Plains on Wednesday night with a second, stronger impulse and attendant jet streak huff onto the southern Plains late Thursday morning. The biggest concern as of right now is that the relative position of the trough is making it look very likely that low-level winds will be severely veered along the dryline in N TX/SW OK that extends from Hobart down through west of SPS, with modest surface winds out of the south/southeast at ~5 knots.
A strong fetch is already in place across the Plains currently, with dewpoints rising from the upper-40s to the low-60s across southern Oklahoma and northwest Texas as of this morning. While the SW 850s shouldn't notably hamper the moisture situation in the lowest 1km, the large amount of moisture combined with the meh shear profiles looks like it might be pointing to a more multicellular, messy precip convective mode should things stay the same.
With the unseasonably high moisture content going into Thursday, instability looks better than expected, excluding from the NAM4KM which places a very meager instability axis across SW OK. MLCAPE values between 1500 j/kg-2000 j/kg have been showing up consistently now with the GFS and NAM in NW TX near SPS.
The variability in dryline positioning/sharpness along with the cold front's motion is a rather notable problem along with the aforementioned VBV profile due to the trough's angle of approach. However, indications of rather sizable low-level shear have shown up in previous runs and depending on the trough's speed, I still think the possibility for a dryline supercell in N TX is very much alive.