While we are looking for signs of cold wintry weather (or, in wxman57's case, pleasant warm outdoors weather) in the long-run model guidance, a more immediate concern presents itself Wednesday evening into Thursday morning. A trough is expected to move eastward from the Rockies and produce a surface low over the state Wednesday night. As its doing that, we could see an influx of Gulf moisture and CAPE ahead of a developing frontal boundary, and some storms developing Wednesday evening could become severe. Might be a dreary, cloudy, and rainy day in the leadup to more feisty storms in the evening. NAM and GFS so far show a stout squall developing Wednesday night and Thursday morning sweeping east across the state.
NWS Austin/San Antonio AFD wrote:Tuesday a mid-level low will dig down into the southwestern states and
turn the flow over Texas to the southwest. This feature will move toward
the east and into Texas by Wednesday. The trough axis will
swing across our CWA with a negative tilt Wednesday night. This will
bring a complex frontal boundary through the area during this time.
Tuesday night the boundary will move northward as a warm front and
continue through our CWA Wednesday. Then Wednesday night the cold
front portion of the boundary will move through from west to east.
Models show the best timing for precipitation to be Tuesday night
through Wednesday night. There will be a chance for thunderstorms
Wednesday afternoon and evening. Model soundings are showing good
instability and vertical wind shear and there could be some strong to
severe storms Wednesday afternoon and evening.
NWS Dallas/Fort Worth had a lot more to say about the system... a lot of good discussion here so I've reproduced much of it below:
NWS Dallas/Fort Worth AFD wrote:This upper level system will be one to watch for a potential severe weather event across North and Central Texas late Wednesday afternoon into Wednesday night. Model guidance is in excellent agreement that there will be strong and organized wind shear ahead of the system, strong dynamic forcing for ascent, and widespread convection Wednesday afternoon and night as the Pacific cold front sweeps through the area. PoPs will be high and QPF of 1 to 2 inches is currently forecast across the entire forecast area.
The question still remains whether surface instability will be available for surface based storms - which would increase the risk for severe weather and tornadoes. While the December 26th 2015 tornado event is fresh on many people`s mind, there are a few notable differences with this setup. The first and most important being that the December 26th event was characterized by extremely anomalous surface based instability with dewpoints in the 70s and an afternoon of sunshine that pushed temperatures to near 80 degrees. There are currently no indications in any of the model guidance that the surface airmass will look anything like those values with the models all clustering both temperatures and dewpoints in the mid to upper 60s.
If there is an analog to this setup that we are mindful of it is the December 29th 2006 event that produced over 20 tornadoes, but most were F0 and F1. Both that event and the one upcoming had similar thermodynamic variables, but the 06 event had a well defined warm front and a surface low/triple point that moved into the western CWA and created strongly backed winds near and just north of the warm front where most of the tornadic activity occurred. While we can`t rule out that this mesoscale feature won`t occur this time around, there aren`t any indications of it in the model guidance at the present time. The upper low in the 06 event was also noteworthy in its slow movement through the Sonora Desert, which likely led to a deeper layer of moisture and higher low level instability than is forecast to occur for this event.
Model guidance has slowed the progression of the system slightly which means there will be more time for richer moisture from the Gulf to return to the region, but also puts the window for severe weather more into the evening or nighttime hours. As is often the case ahead of strong cool-season systems, the strong moisture advection will result in cloud cover and limited potential for sunshine and warmer surface temperatures. Thus, it takes away the uncertainty of: "what if the clouds break up in the afternoon" and allows us to trust forecast surface instability more. Model soundings also depict the impacts of the strong dynamic forcing and lift and show the layer just above the surface will become convectively unstable. This slightly elevated convection may tend to keep the surface cooler and more stable, and limit the ability for storms to become surface based and thus lower the tornado potential.
So having said all that, we will be watching this event closely, but there`s nothing to warrant sounding the alarms for an outbreak due to the concerns about surface instability. The region we`re presently most concerned about right now is south of a Cisco to Hillsboro to Centerville line in the late afternoon into the evening hours for possible severe cellular convection ahead of the front. For most of the region a squall line along the Pacific front looks to be in play, which could result in wind damage and possibly a few brief tornadoes IF the surface isn`t too disrupted by widespread convection ahead of the front during the day.