Greg Blumberg
EF4
A few things. I don't trust the models right now because of their lack of good data regarding the shortwave trough south of Arizona, so I'm sticking to the 00 UTC observations for most of this discussion. I don't think CAPE will be a problem at all tomorrow. Looking at the Tucson, AZ 00 UTC 500 mb temperatures, (which I'd say the location well represent the temperatures of the shortwave trough), I see a -26 C. If this is representative of what kinds of temperatures will be aloft tomorrow, I'd say that the instability fears that we've seen in the past few days will vanish. With some surface heating and the moisture we already have, I believe that CAPE values in the 1,500 J/kg seems reasonable, maybe even more. This is new upper level data is probably the reasoning behind the 00 UTC NAM's CAPE solution Donovan mentioned.
I'll throw this into the mix. We've already got 70 F dewpoints just a bit off of the Texas coast. Advect those up to our target area (which I'll add doesn't seem too unreasonable given 40 knot 1.5 km winds out of the south per the current profilers in TX), and you've probably got somewhere in the 2,000 J/kg of CAPE near the Eastern border of OK. The 00 UTC NAM doesn't even have 70 F dewpoints anywhere near the TX Coast or have the 40 knot winds I was mentioning about. Keep in mind that I'm mostly estimating this, but my main point is that CAPE may be much larger that what we've been thinking. It's possible the 00 UTC NAM is underestimating CAPE.
It's really hard to track the vorticity max using water vapor right now. It's right between the division line between GOES-E and GOES-W on the composite maps. Just from my observations, it looks like it's lifting north ever so slightly. I'm watching the potential for a new surface low developing in southwest Kansas right now via the 3-hr pressure tendency maps and am hoping that the front over OK retreats a bit.
Just from looking at these observations, the MDT risk the SPC has put out seems very well warranted.
I'll throw this into the mix. We've already got 70 F dewpoints just a bit off of the Texas coast. Advect those up to our target area (which I'll add doesn't seem too unreasonable given 40 knot 1.5 km winds out of the south per the current profilers in TX), and you've probably got somewhere in the 2,000 J/kg of CAPE near the Eastern border of OK. The 00 UTC NAM doesn't even have 70 F dewpoints anywhere near the TX Coast or have the 40 knot winds I was mentioning about. Keep in mind that I'm mostly estimating this, but my main point is that CAPE may be much larger that what we've been thinking. It's possible the 00 UTC NAM is underestimating CAPE.
It's really hard to track the vorticity max using water vapor right now. It's right between the division line between GOES-E and GOES-W on the composite maps. Just from my observations, it looks like it's lifting north ever so slightly. I'm watching the potential for a new surface low developing in southwest Kansas right now via the 3-hr pressure tendency maps and am hoping that the front over OK retreats a bit.
Just from looking at these observations, the MDT risk the SPC has put out seems very well warranted.