Traditional Culture Encyclopedia - The 24 Solar Terms - Humidity adjustment of climate box
Humidity adjustment of climate box
Humidity, also known as "relative humidity", refers to the content of water vapor in the atmosphere, expressed by the percentage of the maximum water vapor that air can hold. This content varies with temperature. Warm air can contain more water vapor while cold air contains less water vapor. Completely dry air contains no water vapor, and the relative humidity is 0%, while saturated air cannot absorb more water vapor, and the relative humidity is 100%.
Temperature and humidity are not the same concept, so when the temperature is set to 55 degrees in the artificial climate box, the relative humidity can't reach the highest value of 95% and only 75%; When the temperature drops to more than 40 degrees, the humidity can reach the highest value.
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