Monsoon systems

Monsoon systems are seasonal weather patterns characterized by a significant shift in wind direction, typically bringing heavy rainfall. They occur mainly in tropical and subtropical regions, influenced by temperature differences between land and ocean. During warm months, land heats up faster than water, creating low pressure that draws moist air from oceans, leading to intense rainfall. The most famous example is the Indian monsoon, vital for agriculture. In the colder months, the winds reverse, often leading to dry conditions. Overall, monsoons play a crucial role in regional climates and ecosystems.