Monsoon climates are characterized by distinct wet and dry seasons, primarily influenced by seasonal wind patterns. These climates typically occur in regions like South Asia, Southeast Asia, and parts of Africa. The wet season brings heavy rainfall, often resulting from the southwest monsoon winds, while the dry season experiences significantly less precipitation.
The monsoon season is crucial for agriculture, as it provides the necessary water for crops. However, it can also lead to challenges such as flooding and landslides. Understanding monsoon climates is essential for managing water resources and preparing for potential natural disasters in affected areas.