A tropical monsoon is a climate characterized by distinct wet and dry seasons, primarily found in regions like South Asia and Southeast Asia. During the wet season, heavy rainfall occurs due to the southwest monsoon winds, which bring moisture from the ocean. This period typically lasts several months and is crucial for agriculture. In contrast, the dry season features significantly less rainfall and higher temperatures. The transition between these seasons is marked by a rapid change in weather patterns. Tropical monsoons support diverse ecosystems and are vital for the livelihoods of millions, particularly in farming communities reliant on seasonal rains.