Rainfall

Rainfall refers to the amount of precipitation that falls from the atmosphere to the Earth’s surface in the form of rain. It is typically measured in millimeters or inches over a specific period of time, such as daily, monthly, or annually. Rainfall is a crucial component of the hydrological cycle, affecting water availability, agriculture, ecosystems, and climate. It can vary significantly by region and season, influenced by factors such as weather patterns, topography, and climatic conditions. Rainfall is essential for replenishing groundwater supplies, supporting plant growth, and maintaining the overall balance of natural environments.