In the context of water vapour, it is "relative humidity".
The symbol for relative humidity represents the amount of water vapor present in the air compared to the maximum amount the air can hold at a given temperature.
Relative humidity is the measure of the amount of water vapor present in the air compared to the maximum amount it could hold at a given temperature. It is expressed as a percentage, with 100% indicating that the air is holding the maximum amount of water vapor it can at that temperature.
Humidity refers to the amount of water vapor present in the air, while relative humidity is a measure of the amount of water vapor present in the air compared to the maximum amount the air can hold at a given temperature.
relative humidity
Relative humidity expresses the amount of water vapor present in the air as a percentage of the maximum amount of water vapor the air can hold at that temperature. For example, if the relative humidity is 50%, it means the air is holding half of the maximum water vapor it can hold at that temperature.
The term that defines this is relative humidity. It is expressed as a percentage and indicates the amount of water vapor present in the air compared to the maximum amount of water vapor that the air could hold at that specific temperature.
Humidity is a measure of the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. It is often expressed as a percentage with higher values indicating air that is closer to being saturated.
Relative humidity is a measure of the amount of water vapor present in the air compared to the maximum amount of water vapor that could be present at a given temperature. It is expressed as a percentage, with 100% relative humidity meaning the air is saturated with moisture.
Relative humidity.
relative humidity
The amount of water vapor in the air compared to the maximum amount it can hold at a specific temperature is called relative humidity.
Relative humidity is the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. It is calculated by dividing the actual water vapor pressure by the saturation water vapor pressure at that temperature, and then multiplying by 100 to get a percentage.