no it is not its preasure
Temperature and amount of water vapor.
Temperature and moisture content are the two main properties that characterize an air mass. Air masses are classified based on the temperature and humidity conditions they acquire from their source region.
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
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.
Relative humidity.
Relative humidity.
Relative humidity.
When the amount of water vapor increases, the temperature will generally increase because water vapor traps heat in the atmosphere. This phenomenon is known as the greenhouse effect.
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.
Temperature is the primary factor that affects the amount of water air can hold. Warmer air can hold more water vapor than cooler air. The relationship between temperature and water vapor capacity is known as the Clausius-Clapeyron equation.
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.
Because it is relative to temperature!