Yes, Beryl's problem with a partial core, despite deep convection aiding in regenerating an MLC, is that it's not yet shielded off from the stable airmass that still lingers within the southern half of the circulation. The ULL is still too close and feeding that stable air into the mid-levels. And any nascent core is very prone to downdrafts in this scenario. So even this convection and attempt at a new core could rapidly collapse. We'll just have to see if it's resilient. If anything, this kind of continued bursting will moisten and assist in future convection. Obviously, the modest environmental conditions will continue to improve and become more favorable.
I think this is where you just have to hedge and given the system's demonstrated resilience and tenacity, it has earned the benefit of doubt. May sound anecdotal, but at the end of the day it is these anecdotal hunches that usually distinguish between forecast success and failure.