Then, the wind changes. The air grows heavy, thick enough to chew. The first drops of rain are rarely gentle; they are often explosive, heralding the arrival of the monsoon or the tropical storm.
The transition between these two states is a delicate balance. Climate change has begun to disrupt this equilibrium, making dry seasons longer and more severe, while making wet seasons more unpredictable and intense.
In equatorial and tropical regions (approximately 23.5° N to 23.5° S), temperature remains relatively high and consistent year-round. Consequently, local inhabitants and ecosystems do not prepare for cold but for water scarcity (dry season) or flooding (wet season). Understanding these cycles is critical for water resource management, crop planting schedules, and disease control. This paper aims to define, compare, and analyze the distinct characteristics of dry and wet seasons.