The seasonal reversal of winds is the typical characteristic of

The Monsoon climate is defined by a complete seasonal reversal of wind direction—typically onshore in summer and offshore in winter—driven by the differential heating and cooling of land and sea. While the Mediterranean climate involves seasonal shifts in pressure belts, it lacks the distinct 180-degree reversal of winds that characterizes the Monsoon system. This question tests the core concept of atmospheric circulation and its influence on regional climatic patterns.