Starting to wonder if this starts building an inner core sooner rather than later. The surface circulation is already well defined and appears to be becoming stacked under the sprawling mid-level circulation. This process seems to be complicated only by dry entrainment off of Cuba’s higher terrain, with deep convection widespread in all 4 quadrants otherwise. I’m not seeing much reason why a quicker pace of intensification shouldn’t ensue once that gets mixed out, especially if convection continues to develop over the center.