some rather glaring organizational problems here.
1) The convective bursts at present have been rather singular (as in singular updraft), asymmetric and transient.
2) These bursts are having a hard time really consolidating over the center probably because they're having trouble persisting.
3) The RMW is very broad and there isn't an inner core structure at all, despite the rather intense convective burst ongoing.
4) The large area of 50kt winds on the northern side likely indicates this storm will have trouble building an inner core in short order, at least having a hard time doing it prior to yucatan landfall.
As is, I don't really see this intensifying very quickly with rather significant organizational flaws working against it. I think this makes landfall as a weak cane as it stands now. It may be a strong TS now, but it is still *very* disorganized relatively speaking. Not all 70mph TSs are created equal.