The temperature at which air becomes saturated

The temperature at which air becomes saturated is referred to as the ‘dew point’.

the temperature at which water vapor in the air will condense on surfaces

Dew point is the temperature at which water vapor in the air will condense on surfaces.

The temperature

The temperature at which this happens is called the dew point.

the temperature at which a sample of moist air (or any other water vapour) at constant pressure reaches water vapour saturation

Dew point is the temperature at which a sample of moist air (or any other water vapour) at constant pressure reaches water vapour saturation

the temperature to which air must be cooled for saturation (ie 100% relative humidity) to occur

Dew Point is the temperature to which air must be cooled for saturation (ie 100% relative humidity) to occur, providing there is no change in water content.

the temperature to which a given parcel of humid air must be cooled

Wikipedia describes Dewpoint as ” The dew point is the temperature to which a given parcel of humid air must be cooled, at constant barometric pressure, for water vapour to condense into water.

the temperature to which the air would need to be cooled to reach maximum saturation

Dew point is the temperature to which the air would need to be cooled to reach maximum saturation.

the temperature , to which air must be cooled for saturation (100 relative humidity) to occurproviding there is no change in water vapor content

Dew point is the temperature to which air must be cooled for saturation (100% relative humidity) to occur, providing there is no change in water vapor content.

the temperature at which the air will condense at a given pressure

Dew point is the temperature at which the air will condense at a given pressure.

the temperature that will cause condensation

Dew point is the temperature that will cause condensation or when the RH is 100%.

The temperature at which the vapour begins to condense

The temperature at which the vapour begins to condense is called the dew point.

a measure of atmospheric moisture

Average dew points, a measure of atmospheric moisture, typically lie in the 60–70 °F (16–21 °C) range during July and August.

The temperature at which dew forms

The temperature at which dew forms, called the dew point, depends on the pressure and humidity of the air.

the temperature at which water will condense and form dew (or fog)

Dew point is the temperature at which water will condense and form dew (or fog),

The temperature at 2

The temperature at 2 is called the dew point.

the temperature below which the water vapor in a volume of humid air

The science-y definition of dew point is the temperature below which the water vapor in a volume of humid air at a constant barometric pressure will condense into liquid water.

The temperature at which droplets will form

The temperature at which droplets will form is called the dew point.

The temperature at which droplets can form

The temperature at which droplets can form is called the Dew Point.

the lowest the temperature can fall

The dew point is the lowest the temperature can fall.

the temperature that the metal surface will start to sweat

Dew Point is the temperature that the metal surface will start to sweat.