The premise that southern Florida is uniformly hotter than northern Florida doesn't hold up under scrutiny. Florida's temperature patterns are shaped by multiple interacting factors.
Maritime Influence: Both coasts moderate temperatures. The Gulf Stream warms southeast Florida winters, while the Gulf of Mexico moderates the panhandle. Coastal areas stay cooler in summer and warmer in winter than inland locations.
Urban Heat Islands: Miami, Tampa, Orlando, and Jacksonville all create localized warming. Dense development, asphalt, and reduced vegetation elevate temperatures 2-5°F above surrounding areas.
Elevation and Topography: Northern Florida's slight elevation changes (up to 345 ft at Britton Hill) create minor but measurable temperature differences, especially on clear, calm nights when cold air drainage occurs.
Prevailing Winds and Weather Patterns: Summer seabreeze collisions trigger thunderstorms that cool some areas while others bake. Winter cold fronts affect the panhandle more severely than the Keys.
In winter, the Florida Keys often record the state's warmest temperatures. In summer, inland areas like Okeechobee or the I-4 corridor frequently exceed coastal highs. No single latitude rule applies year-round.
Think in terms of microclimates: coastal vs. inland, urban vs. rural, peninsula vs. panhandle—not simply north vs. south.