If I'm being honest, even for a HSLC setup, this seems pretty poor. I have a feeling WAA advection will take place leading to multiple confluence attempts given heavily saturated profiles that would promote storm growth/perhaps mergers but how much CAPE we really get from this setup is the question. It's not a particularly extreme HSLC setup with around just 270 0-1km SRH. Any confluence band would heavily struggle. A lot of models seem to be struggling on timing imo though. If the QLCS moves thru this parameter space in W LA by 00z-03z, it's honestly the same chance lol as any confluence band in that environment. SPC doesn't seem too interested in this, but i imagine some slight uptrend in CAPE awaits us but we are getting in a pretty tight window. By heavily saturated profiles, that also may mean too much WAA advection over the vicinity resulting in showers limiting destabilization as the SPC says here.
"Furthermore, given the neutral to positive-tilt
trough and deep-layer flow parallel to the surface boundary,
training precipitation could further limit destabilization."
Plenty of failure modes for already a rather poor setup.