Which process occurs when a dew-point temperature that is above freezing is reached at a certain locality?

When the dew-point temperature that is above freezing is reached, condensation occurs because the air becomes saturated with moisture. As air cools or as the moisture content increases, the water vapor in the air condenses into liquid water droplets when it reaches its dew point. This process is essential in the formation of clouds, fog, and dew, as it is when the moisture in the air transforms from a gaseous state to a liquid state.

The conditions that lead to condensation often happen during cooling, such as at night when the temperature drops, or when warm, moist air rises and cools in the atmosphere. This transformation signifies an important aspect of atmospheric moisture as it relates to weather patterns and the hydrological cycle.