Precipitation

"In meteorology, precipitation (also known as hydrometeor) is any product of the condensation of atmospheric water vapor that is deposited on the earth's surface. It occurs when the atmosphere (being a large gaseous solution) becomes saturated with water vapors and the water condenses and falls out of solution (i.e., precipitates) Air becomes saturated via two processes, Cooling and Adding Moisture. Precipitation that reaches the surface of the earth can occur in many different forms, including rain, freezing rain, snow, sleet, and hail." (European Environmental Agency, 2019)

“Precipitation is a key hydrological and climate variable and includes both the liquid (rain) and solid (snow and ice) forms.  Precipitation occurs when a particle formed by the condensation of water vapor becomes heavy enough to fall under the force of gravity.  Precipitation can be measured at any vertical level in the atmosphere, but it is the amount that falls at Earth’s surface that is most relevant for people.” (“Rain Rate” 2025)

Sources

European Environmental Agency. "Water glossary". Accessed March 2, 2019. Available at: https://www.eea.europa.eu/themes/water/glossary

“Rain Rate.” 2025. Accessed September 22. https://www.remss.com/measurements/rain-rate/.
 

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