What is dew point temperature?

Dew point temperature refers to the temperature at which air becomes saturated with water vapor, leading to condensation and the formation of dew. This saturation occurs when the air temperature cools down to a point where it can no longer hold all the moisture it contains, resulting in the excess moisture condensing into liquid form. Understanding dew point is crucial in meteorology, as it helps predict humidity levels and the potential for precipitation.

The other options describe different concepts related to temperature but do not accurately define dew point. For instance, freezing temperature pertains to the phase change of water from liquid to solid, while the temperature of water in clouds can vary widely and is not specifically linked to saturation. Finally, the lowest humidity corresponds to dry air conditions, not to the point of saturation captured by the dew point.