The 12z HRRR, a derived sounding for Birmingham, AL at 5 pm tomorrow evening. Image from pivotalweather with annotations by Jacob Caddell.
Nearly 3000 J/kg of surface instability is more than enough to get strong upward motion from convection. Additionally the lowest 3km provide 120 J/kg of that, which is a significant amount at that level. With dew points near 70 and temperatures in the mid 70s and steep lapse rates (cooling with height) above, that’s a good recipe for an unstable airmass. So the low-levels have the juice but limitations start to show themselves as we rise into the column. It’s just really dry above 850 mb, which does lead to stronger lapse rates aloft but also will lead to evaporation of any rising air which would lead to updrafts not being able to sustain themselves and storms collapsing.
If storms try to get going and collapse, you could easily see some strong winds from this process as shown by the 819 J/kg of downdraft CAPE. That’s extra acceleration due to the buoyancy differences on top of gravity pulling on it.
Storms that do survive the dry air aloft will present potential for large hail with the instability in the -10 to -30 C temperature region. Assuming that instability can be realized.
The shear profile is not all that impressive for tornadoes, despite the strong instability from the surface and in the low-levels. Not much change in direction with height at all, and a critical angle of just 26 showing far more crosswise vorticity vs streamwise. This is just not supportive of tornadoes. Shear in general isn’t all that strong but there is increasing speed with height that would help tilt an updraft and why there is still some severe potential, even if the tornado risk does not look all that likely.
The tl;dr version:
Storms should fire in southern Alabama, Georgia, and the Panhandle by early afternoon as a shortwave brings dynamic support and whatever outflow boundaries left behind from today provide a focus for surface convergence. They will likely form a cluster of storms that will have ok shear and plenty of instability to work with. Would not be surprised to see the enhanced risk (3/5 risk) end up farther south by tomorrow’s update from the SPC. These storms could limit instability to the north of them and would further limit the severe potential toward Birmingham and Atlanta. Speaking of that northern end, shear profiles aren’t terribly impressive and would limit tornado risk even if more high heat content air ends up there than implied by the southern storms firing early. There will be some lifting coming due to an incoming cold front and there is substantial instability aloft due to cold mid-level air that cools quickly as you rise. The problem there is the environment will be dry above the surface and this would likely keep deep convection from happening.
Do remember though, if updrafts collapse, there will be high wind potential as the air rushes back toward the ground.
The super short version is to be aware of the severe potential, even though there are a few reasons why it won’t materialize especially in northern Alabama and Georgia. If you get a warning, take it seriously and keep an eye on the radar.
That’s all for today.