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The amount of water vapor that air can hold depends on its temperature. Warmer air can hold more water vapor than cooler air. This relationship is described by the concept of relative humidity, which is the ratio of the amount of water vapor present in the air to the maximum amount the air could hold at that temperature.
Relative humidity is a measure of the amount of water vapor in the air. It represents the ratio of the amount of water vapor present in the air to the maximum amount of water vapor the air can hold at a specific temperature, expressed as a percentage.
no. humidity is the amount of water in the air.
Humidity is the measurement of the amount of water vapour in the air.
The amount of water in the air compared to the maximum amount of water vapor the air can hold at a given temperature is referred to as relative humidity. It is often expressed as a percentage.
relative humidity
The comparison of the actual amount of water vapor in the air to the amount of water vapor in the air if it were saturated is called relative humidity. It is expressed as a percentage and indicates how close the air is to being saturated with moisture.
The amount of water vapor in the air compared to the maximum amount it can hold at a specific temperature is called relative humidity.
Humidity is the amount of water vapor present in the air. It is a measure of the water content in the atmosphere, indicating how much moisture the air can hold. Low humidity means there is a lack of water vapor in the air, while high humidity means there is a higher amount of water vapor present.
"relative humidity"
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.