Tropical monsoon climate

Tropical monsoon climate is characterized by a distinct seasonal pattern of heavy rainfall and a dry period. Typically found near the equator, this climate sees abundant rain during the monsoon season, driven by changes in wind patterns and temperature, supporting lush vegetation and agriculture. The dry season occurs when winds shift, bringing less moisture. Temperatures remain warm year-round, but overall humidity and rainfall vary significantly between seasons. This climate is common in regions like South Asia, Southeast Asia, and parts of West Africa, influencing local ecosystems, agriculture, and daily life.