Condensation is indeed closely related to humidity. It occurs when air becomes saturated with moisture, meaning it contains as much water vapor as it can hold at a given temperature and pressure. When the air reaches its saturation point, any additional increase in humidity or decrease in temperature can lead to condensation.
Condensation occurs when warm, moist air comes into contact with a colder surface or encounters a colder air mass. As the air cools down, it loses its ability to hold as much moisture, and the excess water vapor transforms into tiny water droplets or ice crystals, depending on the temperature. This process is what creates dew on grass in the morning or forms clouds in the sky.
To make condensation happen, the air temperature needs to decrease to the point where it reaches its dew point temperature. The dew point is the temperature at which air becomes saturated with moisture and starts to condense. When the air temperature reaches or drops below the dew point, the excess water vapor in the air begins to condense into visible water droplets or frost, depending on the conditions.
In summary, condensation occurs when air reaches its saturation point due to high humidity and cools down to its dew point temperature, causing excess water vapor to change into visible water droplets or ice crystals
The relation between Humidity and Condensation is very prominent. Higher humidity helps to saturate the gaseous molecules of water. As a result, the density increases, and the molecules condense and become water droplets. Excessive humidity is the cause of most window condensation. As the outside temperature drops, the window glass temperature also drops. When moist air comes in contact with the cold glass pane, the moisture condenses and forms water droplets. When the air has high moisture content, as is the case in humid weather, this sweat cannot evaporate, leaving our bodies feeling hot and sticky. To cool off, our bodies must work even harder. This results in excessive sweating, increased rate and depth of blood circulation and increased respiration when the air has high moisture content, as is the case in humid weather, this sweat cannot evaporate, leaving our bodies feeling hot and sticky. To cool off, our bodies must work even harder. This results in excessive sweating, increased rate and depth of blood circulation and increased respiration. If the amount of water vapor in the air increases while the temperature remains the same, the relative humidity will increase. If it reaches 100%, condensation will occur. At which point it condenses and forms dew. So when the humidity level gets to 100% it doesn't matter what the air temperature is, as condensation will occur at any temperature once humidity levels reach 100% as the air can't physically hold any more moisture. All in all, a relative humidity of 30% should ideally be maintained in the home during the winter months in order to avoid health problems as well as condensation on windows and doors. Condensation happens one of two ways: Either the air is cooled to its dew point or it becomes so saturated with water vapor that it cannot hold any more water. Dew point is the temperature at which condensation happens. The amount of water vapor air can hold is directly related to the air temperature. Warmer air can hold more water vapor than cooler air. When warm air is cooled it loses its capacity to hold water vapor and, if it cools enough, it will begin to condensate. Dew Point is the temperature at which moisture will condense out of the air. If the temperature of any surface is at or below the dew point temperature then dew (condensation) will form. Here are some examples of Dew Point conditions: 85°C and 85% RH, the Dew Point is 80.9°C. At any temperature, evaporation and condensation are actually occurring at the same time. Faster molecules from the liquid evaporate while slower molecules from the gas condense. Depending on the conditions, one process will happen at a faster rate than the other resulting in net evaporation or net condensation.