I thought a Miller B would always have an initial low that would transfer to a new developing low. This almost always results in CAD. I thought a Miller A had no hand off of one low to another. I didn’t think p-types had anything to do with whether it was a Miller A or B. For instance, couldn’t you have a Miller A in May that was rain only - or for that matter a Miller B with all rain? In sum, doesn’t miller A or Miller B have to do with atmospheric pressures and development, and nothing to do with p-types? Obviously, mixed Ptypes are more synonymous with Miller B’s and less so with Miller A’s. Thanks. TW