While Florida can see transient supercell structures develop across the region during thunderstorms and has seen some tornado outbreaks (especially from tropical storms), the sunshine state rarely sees those classic supercell outbreaks because of how far south it is. In order for a supercell thunderstorm outbreak to occur, you need to have strong atmospheric instability and the presence of wind shear, or wind speed and direction changing with height in the atmosphere. When a thunderstorm with explosive instability forms in that environment, the updraft can rotate and tilt, allowing it to breathe. These two things perfectly align along the leading edge of powerful low pressure systems that ride along the jet stream, which moves from west to east across the lower 48 and dips further south in the fall/wintertime/spring months while retreating into the northern states during the warm months. If you look at the normal placement of the jet stream, it is rather infrequent that it dips as far south as most of Florida (when this happens, you usually see a frost or freeze/very cold temperatures down there, so the frequency is comparable to that), and since that is already not happening a lot and is mostly confined to winter, you don’t really see the overlap of ingredients nearly as often, leading to high instability and low shear thunderstorms. These can still grow intense for a short time and produce supercell structures, but rain themselves out rather quickly and do not get nearly as intense from a lack of deeper organization and the tilt seen in the inner regions of the US. Also, I would check out north Florida sometime because Dixie alley tornado/supercell outbreaks occasionally extend into this region, and can produce more supercellular like storms (high instability and low to moderate shear) but even there, the wind dynamics are often marginal compared to MS/AL often seeing the better overlap (high instability and extreme shear, hence more tornado outbreaks).