The global monsoon system is a complex climatic phenomenon characterized by seasonal changes in wind patterns and precipitation over large regions of the world, primarily influenced by the differential heating of land and ocean surfaces. Monsoons are most prominent in South and Southeast Asia, parts of Africa, Australia, and North and South America. They are not limited to a single region but represent a global pattern of seasonal atmospheric circulation changes that bring distinct wet and dry periods. The monsoon system operates on the principle that land heats up and cools down faster than oceans. During the summer, the landmass warms more quickly than the surrounding seas, causing the air above the land to rise due to convection. This creates a low-pressure zone over the continent. In response, cooler, moisture-laden air from the adjacent oceans moves inland, resulting in heavy seasonal rainfall. In contrast, during the winter, the land cools faster