A lot of the storm mode being linear has just been down to deep layer shear vectors with a combination of trough geometry. All of our troughs have been disjointed and we’ve had to rely on surface features like warm fronts for CI vs classic subtle forcing over a N/S oriented boundary.
If you look at your classic, big time headlining outbreaks throughout history, not all of them had sky high parameters. Or 5500 k/j of cape paired with 600 SRH. They had adequate to great parameters over a large aerial expanse with a very cooperating storm mode. That cooperating storm mode is the hardest part to get, as you noted. That can come down to forcing, balance of dry air, vectors, and a stout cap.