A tropical climate is characterized by consistently high average temperatures throughout the year and distinct periods of wet and dry conditions. These climates are typically found near the equator, receiving intense solar radiation that drives predictable atmospheric circulation patterns. The warm moisture content often results in high humidity levels and can support dense biodiversity. The seasonal variation is generally defined by the movement of the Intertropical Convergence Zone (ITCZ), which dictates whether the region experiences monsoon-like rainfall or a drier dry season. Due to the consistent heating and moisture sources, tropical regions are vital areas of global atmospheric energy exchange.