We start with water vapor imagery early this afternoon. The blues, greens, and whites indicate copious amounts of mid-level moisture, originating from the southeastern Pacific/Gulf of California. An area of enhanced moisture associated with a fort max is seen over eastern parts of Texas, and is likely contributing to the veil of high-level cirrus that is blanketing us here in the GTR and all across central and northern Mississippi.
Severe Weather Discussion
The Storm Prediction Center maintains a slight risk of severe weather for much of the state of Mississippi for Thursday and Thursday night, and an enhanced area of severe weather probabilities are defined for north Mississippi up through western Tennessee and Kentucky.
Synoptically, this system remains impressive with a significant dynamic wind field. A strong negatively tilted shortwave trough will be ejecting out of the southern Plains northeastward, and PVA associated with this feature will be abundant.
In the upper levels, an area of enhanced diffluence will coincide with downstream PVA and result in widespread and significant dynamic uplift. In fact, some of the wind fields are very potent, including a 50-70 kt low-level jet and a 120+ kt upper-level jet streak.
Moisture will be far from meager with this event thanks to the aforementioned strong low-level jet transporting Gulf moisture northward in advance of the approaching frontal boundary. Additionally, southwesterly flow in the mid-levels (as shown in the water vapor imagery) is also supplying copious amounts of moisture in the mid-levels of the atmosphere as well. PWAT values will exceed 2" for most locations as well, so heavy rainfall is also a hazard.
However, thermodynamically speaking, this system is just lacking. With all of the moisture in the air, lapse rates are barely moist adiabatic, if that. Given that we have relatively warmer air in the 700-500mb layer, mid-level lapse rates remain poor (< 6 C). This greatly inhibits instability and the ability for storms to be sustained into the mid-levels of the atmosphere. Therefore, these showers and embedded storms will most likely be low-topped with very low cloud bases with LCL heights likely lower than 1km AGL in some cases.
That being said, with such incredible dynamic uplift, it is likely that at least some of the thermodynamic insufficiencies will be overcome. As SPC's enhanced risk shows, this is more likely to the north of the GTR as mid-level temperatures/heights are a little bit lower relative to what they are here in central MS.
Here's the modeled lapse rates from the 12z NAM. As discussed, this graphically depicts the relatively higher lapse rates (6 - 6.5 C/km) well to our north, and values < 6 down this way.
Given all of this information, sustained WAA will steadily increase our dew point temperatures and despite widespread cloud cover expected tomorrow, surface air temperatures should manage to achieve the mid 70s. However, as the mid-level ridge 'battles' with the approaching trough (700mb temps/heights warmer/higher), appreciable CAPE is not able to be realized in the warm sector, at least here in MS. Still, models can underdo instability even this short in advance, but the prospects of achieving CAPE over 250 J/kg is very unlikely at this point.
However, even with very marginal CAPE/instability, the dynamic forcing cannot be ignored. With that said, I'm still expecting a strongly forced line of convective showers with a few lightning strikes embedded to prelude the cold front tomorrow late afternoon through tomorrow night. Within this line, provided the boundary layer remains well mixed (which it should given very strong low-level winds prevailing and even increasing nocturnally), some of those stronger winds located just a couple thousand feet off the ground could be transferred downward. Behind this forced line, moderate rains will likely continue right along the front and some of it being post-frontal as well.
Additionally, winds remain relatively backed around to at least southerly as a weakening meso-low moves northeast out of Arkansas. This combined with the aforementioned very strong low-level jet winds is creating helicity in the lowest 2km AGL of over 300-400 m^2/s^2, favorable for tornadogensis. However, because the instability is so low, the excessive shear in the atmosphere may act to 'shear out' the showers and embedded storms that try to grow vertically. Nonetheless, very quick, spin-up tornadoes are possible down this way, but not likely, within the leading, strongly forced line of showers and embedded storms.
The highest isolated tornado and potentially gusty wind threat should be located north of us here in the GTR, basically where the SPC has defined a 30% chance of severe weather (in the graphic above). The thermodynamics down this way are severely lacking, and the best wind field seems to be out of phase with the extra uplift associated with the approaching front. Details on the mesoscale tomorrow will be important to this event's evolution, so stay tuned!
IW