What is Rainfall in Geography?
This article is entitled Explain What Is Rainfall in Geography? Definition: Rainfall is a measure of the amount of rain that falls in a particular season, for example, a week or a month. Rainfall is measured by the collection of rainwater at different times and times, as values may vary from place to place. Rainfall is a process in which local air becomes saturated and begins to flow as you can no longer maintain evaporation in the form of gases. There are different types of rain — Liquid, Cold and Ice. What is Cyclonic Rainfall in Geography? This type of rainfall occurs when warm and cold air meets. As warmer air is lighter, it rises above cold air. The rising air then cools over the overflow which leads to heavy rainfall. Such rain lasts only a few hours. Rain is very strong in hot storms is Cyclonic Rainfall Cyclonic activity creates storm eruptions and takes place near the edges of hurricanes. When two layers of air of different densities, temperature, and humidity meet the