Forecast update!
Oklahoma's fucked.
Recent model runs have been consistently showing a virtually perfect environment on Monday into the overnight hours. When I mean virtually perfect, I really do mean virtually perfect.
The SPC has put out a Day 2 Moderate risk for parts of Oklahoma and Kansas, with a larger Enhanced risk around that, driven by a 15% risk for significant tornadoes and a 45% risk for large hail. The SPC outlines several interesting things in the discussion as well that makes it extremely concerning.
Additionally, forecast hodographs are quite long, with little
mid-level weakness. Mean storm motion is around 50 kt from 21 to
00Z, with Bunkers right motion around 30 kt. This should be more
than sufficient for storms to remain discrete and maintain supercell
characteristics. This also contributes to a greater potential for
long-track tornadoes. The tornado threat will persist pass sunset
and into the evening, supported by the persistence of ample
low-level moisture/buoyancy and a strengthening low-level jet. Most
current guidance maximizes the STP at 8-10 around 03Z over
south-central OK.
The environment is extremely favorable for discrete supercells across parts of Oklahoma into the overnight. How favorable, exactly? Well they mention a maximized STP (significant tornado parameter) of 8 to 10 throughout most parts of the area, which is INCREDIBLY high. However, some models show even higher numbers.
Yes. A significant tornado parameter of
SEVENTEEN. Some soundings have even shown STP values of up to 20 in some areas. Let's go into technical stuff to see why this is such a ridiculously favorable environment.
SRH values, or Storm Relative Helicity, are extremely high, with well over 400 m2/s2 of 0-1km SRH and over 600 m2/s2 of 0-3km SRH, which is an extreme amount. 150-200 m2/s2 of SRH is more than enough to produce strong tornadoes; the values seen here well exceed that requirement.
Alongside that, instability, measured in CAPE or Convective Potential Available Energy, is in excess of 3,000 to
4,000 j/kg. Again, only 1,000 j/kg of CAPE is more than enough to produce thunderstorms and tornadoes, and this much instability is extremely rare.
Combine the wind shear (SRH) and the extreme instability we have here, as well as smaller things such as subtle forcing to keep storms discrete, steep lapse rates (temperature falls with height) and extremely favorable moisture profiles, and you get one of the most volatile environments ever forecasted from models.
Keep in mind this environment will exist overnight so most tornadoes will be at the dead of night.
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And earlier in the day too, the forecasted environment is extremely similar to the one that produced the May 3rd, 1999 Bridge Creek-Moore F5. I'm honestly expecting a High Risk to be issued tomorrow for this area.
Further north, into Kansas and parts of Nebraska, a favorable environment, albeit not as extreme, will exist for tornadoes, however the mode will be more linear, so the risk for strong and long-tracked tornadoes is not as significant.
We'll have to see how models trend and what does happen, since models have been pretty inconsistent recently, but the sheer amount of consistency this time between models is very worrying.