Models and ensembles have started to key in on the amplification of the shortwave, though it's worth noting that the disturbance responsible for it will only reach the Canadian coast on Saturday, after which it'll be sampled by upper-air balloons for the first time. An amplifying shortwave trough would serve to reinforce cold, especially in the mid-levels (500-700 hPa). That doesn't sound immediately like a big deal, but what it does is sharpen the temperature gradient between the interior Central US and the Gulf coast. Large gradients in temperature in the low to mid-levels means big increases in wind aloft, so that results in a strengthening of the northern stream jet over the Ohio River Valley.
Air accelerating off into the jet results in upper-air divergence, so air needs to be drawn up from the low-levels to replace it. The start of the jet, especially south and east of that area (i.e. the "right entrance region"), is a favored region for air to ascend into. Where this area is depends on the orientation and strength of the trough. The 12z GFS, pictured below, had a stronger, more emphatic jet than the 12z ECMWF, resulting in divergence extending farther north.

Details are yet to be worked out, but the general location of the shortwave is well-suited to draw moisture from the Gulf. We can represent this by plotting potential temperature (theta-E) like an topographical surface, since air tends to maintain constant potential temperature. In this case, the 295K potential temperature level is plotted like terrain, allowing us to visualize the ascent of humid air from the moist Gulf upwards over Texas to feed the jet stream. This translates into vertical motion over Texas, and, provided the air is sufficiently saturated aloft, precipitation:

Key questions determining precipitation location, type, and amount will be:
- How far inland will moisture be able to reach? The 12Z GFS showed the plume of moisture reaching the Red River. The 12Z Euro struggled to reach US-290.
- Will the plume of moisture sustain long enough to permit precipitation before drier low-level air associated with the shortwave trough arrives from the north? (Especially for North Texas)
- How cold will it be throughout the low-levels at the start of the event? Southerly flow inevitably causes warming. Will the resulting warm nose be well above freezing or marginal/below freezing?