The temperature to which air can be cooled without causing condensation.

A measure of the amount of moisture in the air. It is the temperature to which air must be cooled in order to reach saturation.

The temperature at any given pressure at which liquid initially condenses from a gas or vapor. It is specifically applied to the temperature at which water vapor starts to condense from a gas mixture (water dew point) or at which hydrocarbons start to condense (hydrocarbon dew point).

The temperature to which air must be cooled such that it cannot hold any more water (saturated). When air at ground level reaches its dew point, dew forms on any exposed surface. Under certain conditions, air at its dew point forms a fog.

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 content. The dew-point is an important measurement used to predict the formation of dew, frost, and fog. If dew-point and temperature are close together in the late afternoon when the air begins to turn colder, fog is likely during the night. Dew point is also a good indicator of the air's actual water vapor content, unlike relative humidity, which takes the air's temperature into account. High dew point indicates high vapor content; low dew-point indicates low vapor content. In addition a high dew-point indicates a better chance of rain and severe thunderstorms. You can even use dew-point to predict the minimum overnight temperature. Provided no new fronts are expected overnight and the afternoon Relative Humidity ≥ 50%, the afternoon's dew point gives you an idea of what minimum temperature to expect overnight, since the air is not likely to get colder than the dew-point anytime during the night.

The temperature at which air must be cooled before dew can form, the temperature where secondary damages will start after a water loss. differing site conditions The occurring act (change) of a building component or contents item which changes conditions due to secondary damages, such as mold, absorption, corrosion, etc.

The dew point is the temperature the air must be cooled to for the air to become completely saturated. At that point the relative humidity is equal to 100%. The farther apart the air temperature is from the dew point, the drier the air and the lower the relative humidity. The closer the air is to the dew point, the damper or wetter the air, and the higher the relative humidity.

The temperature at which condensation begins to form as a gas is cooled.

Temperature at which a vapor begins to deposit as a liquid. Applies especially to water in the atmosphere.

The temperature at which water vapour present in the atmosphere is sufficient to saturate it. ( BCFT).

the temperature at which water would condense from the air if the air mass were cooled. In general, when the relative humidity is high, the dew point will be close to the air temperature. At 100% relative humidity, the dew point is equal to the air temperature. When the relative humidity is low, the dew point is much lower than the air temperature.

The temperature at which the current amount of water vapor would condense into fog.

As the surface of the earth cools at night, warm moist air near the ground is chilled and water vapour in the air condenses into droplets on the grass and other objects. Dew is particularly heavy on clear nights, when the earth cools rapidly. When a blanket of cloud insulates the earth, the cooling rate is slower. [Go to source

The temperature to which a certain amount of air must be cooled in order for saturation to occur (a cloud or fog to form); the drier the air the lower the dew point and the more air is needed to be cooled for a cloud or fog to form.

The temperature, referred to a specific pressure, at which water vapours condense.

Temperature of a surface at which condensation of moisture will occur (under ambient temperature and relative humidity).

the temperature at which droplets of water condense from air (dependent on the prevailing humidity)

The warmest temperature of an object in an environment where water condensation from the surrounding air would form on that object.

A TEMPERATURE AT WHICH CONDENSATION WILL FORM AT A CERTAIN AIR PRESSURE AND HUMIDITY.

The surface temperature at which moisture will condense out of the air onto a surface; varies with the relative humidity.

A measure of humidity given in terms of the temperature at which dew will start to form.

the temperature at which condensation from the vapor phase occurs

the temperature at which the water vapor in the air becomes saturated and condensation begins

the temperature at which the water vapour in the air condenses out into droplets of water forming precipitation.

The temperature at which dew or condensation begins to form.

The temperature to which air must be cooled for water vapor to condense (change to liquid).

the temperature at which water vapor turns to liquid

is the temperature that the air will no longer hold its entire moisture vapor. (Cold air holds less moisture vapor than warm air).

The temperature at which an air mixture is saturated with water vapor. If the temperature is at or below the dew point, condensation will occur.

The highest temperature of an object at which condensation will form on it.

The temperature at which water will condense out of a mixture of gasses. The dew point can be used as a means of identifying the humidity of a gas volume.

Temperature to which air must be cooled at constant pressure and water vapor content in order that it shall be saturated with respect to water.

The temperature to which the air must be cooled in order to have water vapor condense out of it.

The temperature at which water vapor condenses from the air. The dew point varies with the relative humidity.

Temperature at which vapor condenses from the atmosphere and forms water.

The temperature at which air becomes saturated when cooled without addition of moisture or change of pressure; any further cooling causes condensation.

The temperature to which the air must be cooled to condense. For example, if the air temperature was 65 degrees and the dew point was 65 degrees the humidity would be 100% and the air would be totally saturated. The larger the spread of temperature and dew point, the drier the air. This spread is called the dew point depression.

The temperature of which air must be cooled for it to be saturated.

Temperature at which water vapor condenses to a liquid

Temperature to which a specified parcel of air must cool, at constant pressure and water-vapor content, in order for saturation to occur. The dew point is always lower than the wet-bulb temperature, which is always lower than the dry- bulb temperature, except when the air is saturated and all three values are equal. Fog may form when temperature drops to equal the dew point.

When warm air comes in contact with a colder surface, such as a glass containing a drink with ice cubes or a cold window, water vapor from the air can start condensing on the glass or window. The temperature at which the condensation starts to happen for the relative humidity is called the dew point. If the relative humidity decreases or the temperature increases, the dew point raises to a higher temperature.

The temperature to which a sample of air must be cooled, while the mixing ratio and barometric pressure remain constant, in order to attain saturation by water vapor. When barometric pressure remain constant, in order to attain saturation by water vapor. When this temperature is below O°C, it is sometimes called the frost point.

The temperature at which the relative humidity is at 100 percent. In summer, most people are uncomfortable when the dew point goes above 65. Dew points above 70 cause very muggy conditions.

The temperature at which water molecules in a gas will begin to condense and form a liquid

The exact temperature at which moisture begins to form

Warm air can hold more moisture than cold air. When the air temperature drops low enough, the moisture in the air comes out and forms droplets on the ground. We call those droplets dew.

The point at which warm, moist air cools below a specific temperature and changes state from a vapor to a liquid.

The temperature at which water vapor begins to condense.

The temperature at which water vapour in the air begins to condense.

The temperature at which a vapor begins to condense.

the temperature at which the moisture in air condenses from a vapour back to a liquid. As in the condensation that forms on a cold surface relative to air temperature, i.e. glazing or un-insulated ducts or pipes.

Of a gas is the temperature at which the vapor in a space (at a given pressure) will start to condense (form dew). Dew point of a gas mixture is the temperature at which the highest boiling point constituent will start to condense. ( 030)

That temperature at which the weight of steam associated with a certain weight of dry air is adequate to saturate that weight of air. When air at less than 100% relative humidity is cooled to the temperature at which it becomes saturated, the air has reached the minimum temperature to which it can be cooled without precipitation of the moisture (dew).

Temperature at which air is saturated with moisture or, in general, the temperature at which a gas is saturated with respect to a condensable component.

The temperature at which a condensible component of a gas starts to condense into a liquid.

The temperature at which water vapor in air will condense at a given state of humidity and pressure.

the temperature at which the air becomes saturated with water vapor

The temperature to which air must be cooled to in order for dew (or frost) to form

The temperature at which dew would form.

The temperature at which air with a given amount of moisture is fully saturated, so that condensation occurs.

The temperature to which air must be cooled for saturation to occur, exclusive of air pressure or moisture content change. At that temperature dew begins to form, and water vapor condenses into liquid.

a measure of atmospheric moisture; the temperature to which air must be cooled for saturation to occur (given a constant pressure and constant water-vapor content)

is a measure of humidity, given in terms of the air temperature at which dew begins to form, as water vapor condenses into liquid.

The temperature to which a certain volume of air must be cooled to bring the relative humidity to 100 percent.

The temperature at which moisture in the air will begin to condense if the air is cooled at constant pressure. At this point the relative humidity is 100%.

The temperature of a surface, at a given ambient temperature and relative humidity, at which condensation of moisture will occur.

The temperature at which condensation or formation of a liquid phase begins. The term most commonly applies to condensation of moisture from water vapor in the atmosphere.

The temperature at which a vapour begins to condense.

The temperature at which the moisture in a gas commences to form droplets. The temperature varies according to the type of gas, and the moisture concentration.

The temperature at which condensation occurs for a given concentration of water vapor in the air.

The temperature to which air must be cooled to become saturated by the water vapour already present in the air.

The temperature at which liquid first condenses when a vapor is cooled .

A measure of the absolute amount of water in the air. As air is circulated into and around a building, its absolute moisture content - and therefore its dew point - does not change unless it is humidified or dehumidified. Dew point is the temperature at which water will begin to condense out of the air, expressed in degrees F or C.

A measure of atmosphere purity, it is the temperature where moisture condenses out of a process atmosphere.

The temperature and pressure at which a gas begins to condense to a liquid.

temperature at which water vapor condenses into cloud droplets

The temperature below which condensation of vapor begins to occur as the atmosphere is cooled (pressure dependent).

The temperature and pressure at which the liquefaction of a vapor begins.

The temperature at which relative humidity reaches 100% and water vapor is able to condense into water droplets. The dew point varies depending on the absolute water vapor content of the air.

the point at which water vapor condenses into droplets of water

upon cooling a vapour mixture, this is the point at which droplets of liquid first appear.

is a temperature level which indicates the temperature of the air at which condensation takes place

The temperature to which a given parcel of air must be cooled at constant pressure and constant water-vapor content in order for saturation to occur.

temperature (Td) - The temperature to which air must cool at constant pressure in order for air to reach saturation (commonly dew to form); indicates moisture content.

The temperature and pressure at which a liquid begins to condense out of a gas.

The temperature to which air must be cooled to become saturated with water vapor. Further cooling leads to the formation of fog or cloud droplets in the atmosphere or the deposit of dew on the surface.

The temperature to which air must be cooled to cause condensation of the water vapor it contains.

The temperature at which water starts to condense out of a particular air mass.

the temperature at visible moisture would form if you cooled a parcel of air. At this temperature there would be 100% humidity and any further cooling and water vapour would condense.

The temperature at which components of a gas material starts to condense into liquid.

Temperature to which air must be cooled to reach saturation at a constant atmospheric pressure. The dew point is always lower than the wet-bulb temperature, which in turn is always lower than the dry-bulb temperature. The only exception to this is when the air is saturated (i.e., relative humidity is 100 percent), in which case all three values are equal.

The temperature to which air must be cooled at a constant pressure to become saturated.

the temperature at which water vapor starts to condense in cooling air at the existing atmospheric pressure and vapor content.

The temperature at which air, by cooling, becomes saturated with vapor, and droplets begin to form.

Temperature at which dew starts to form or vapor to condense into liquid.

The temperature at which moist air will become saturated and condensation of water vapor will take place.

The dew point or dewpoint of a given parcel of air is the temperature to which the parcel must be cooled, at constant barometric pressure, for the water vapor component to condense into water, called dew. When the dew point temperature falls below freezing it is called the frost point as the water vapor no longer creates dew but instead creates frost or hoarfrost by deposition.