LP supercell near Pampa completely gone now. Was gorgeous, don't know why it didn't produce
Disclaimer: this is a WAG. It seems to me that a lot of storms don't produce on days like today because their storm motion is too slow. The "Pampa" storm today was a slow mover. It's not just the lack of SRH that can result from slow storm motion.
I can't come up with a good analogy, so I offer a crappy one:
Picture a boat moving over water slowly. The wake it creates spreads out behind the boat at a wide, or obtuse, angle. A boat speeding along the water leaves a wake with an acute angle. In fact, the slow boat pushes the water ahead of it a bit; the fast boat does not. Well, much less so.
Same thing with a storm, sort of. All thunderstorms will generate a low pressure area near their base as the updraft does its thing. That explains non-synoptic strong inflow winds near the RFB. A fast mover will leave a "wake" of low pressure behind it (*boat analogy*) , and as a bonus to the fast-moving storm, ingests PBL more readily as it clips along at its brisk pace.
Here's another ridiculous analogy to illustrate that: Lets say you have a vaccuum cleaner that ingests air at 30mph. It creates a vaccuum *duh* at the end of the hose. Well, what if you got in your car and drove at 30 mph holding the hose facing forward out the window with it turned on? Would there still be an area of low pressure created at the hose's opening? Of course not. Drive at 60mph, and there would actually be high pressure there relative to the ambient air, as the onrushing air would be blocked by the hose, even though the vaccuum cleaner was running.
A fast moving storm is like that hose held out the window. It gets fed lots of air. Sort of turbocharged.
Back to the boat wake: A fast moving storm creates little low pressure area in front of it. The low pressure wake is left behind more. It would be oval/elongated in shape, with most of the oval trailing the storm. A slow moving storm creates a rounder low around it, with the leading edge a greater distance in advance of the storm.
A storm struggling to mature can be choked by slow storm motion in this way. We saw the Pampa storm pulse as the updraft would first suffocate from low pressure at 360 degrees surrounding its base, then regenerate after the updraft weakened, which allowed synoptic/meso inflow to resume, and over and over until the updraft died on a cycle of storm-fatal inflow suffocation.
*edit I guess I should have waited for the "4-23 DISC thread...."