👉 Humidity, often measured in percentage (%), is a crucial metric in meteorology that describes the amount of water vapor present in the air relative to its capacity to hold that water vapor at a given temperature. The formula to calculate relative humidity (RH) is RH = (Actual Humidity / Saturation Humidity)
100, where "Actual Humidity" is the current amount of water vapor in the air and "Saturation Humidity" is the maximum amount of water vapor the air can hold at that temperature. When RH equals 100%, the air is fully saturated, meaning it cannot hold any more water vapor, and condensation occurs. Lower RH values indicate drier air, while higher values suggest more moisture. This concept is vital for understanding weather patterns, predicting precipitation, and managing various environmental conditions.
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What is the definition of Humidity Math? 🙋
