
You may need to reread this part a couple of times to make sense of it all. This is a bit of a mind-bender, and it takes a while to wrap your head around it. The change from 50% relative humidity to 100% however, did not reflect the reality that the discomfort level (even at a 100% humidity), may not be as uncomfortable as the figures may imply. This simply shows that the higher temperature in Container B allows the air to contain a greater amount of water vapor, which is clearly reflected by the higher dew point temperatures in the illustration above. If the air were to be cooled even more, water vapor would have to come out of the atmosphere in the liquid form, usually as fog or precipitation. At this point the air cannot hold more water in the gas form.

This is evident as the relative humidity of Container A, even at a 100% in Figure 2, is still below the higher the dew point level of Container B. The dew point is the temperature the air needs to be cooled to (at constant pressure) in order to achieve a relative humidity (RH) of 100. This means in both cases, the level of discomfort in Container B is higher than that of Container A. Even if the relative humidity is raised to 100% in Container A, and the air is fully saturated at a dew point of 21° Celsius, it is still below that of Container B, where nothing has changed, and the dew point remains at 26° Celsius as a result. This is clearly indicated by the much higher dew point temperature of 26° Celsius (compared to the much lower dew point of 10 ° Celsius in Container A). If you want to know whether (or weather, heh) it's comfortable or not to have a morning jog or go on a weekend hiking trip stick with that term. The higher the dew point is, the more moisture that is in the air. In this experiment, you will determine the dew point temperature in two different ways and learn more about what dew point actually means.Since the temperature in Container B is much higher, allowing the air to hold more moisture, the discomfort level is substantially higher than that in Container A. Dew point is an accurate measurement of the moisture content in the air. This liquid forms by the condensation of water vapor that is near the surface of the glass.

Farmers and gardeners use the dew point to estimate how much water they need to give plants.Meteorologists use dew point to predict the potential for storms as well as nighttime temperatures.Dew point is also a fascinating exercise. Water vapor in the air condenses at the dew point. The dew point temperature will never be higher than the air temperature dew point temperature will always be equal to or less than air temperature. By definition DEW POINT is a temperature that represents humidity. Warmer air is able to store more water vapor than cooler air, so warmer air has a higher dew point temperature than cooler air. When the air temperature drops below the dew point temperature, condensation occurs, resulting in the formation of dew, fog, and/or clouds.

In other words, the temperature at which relative humidity is 100%. Dew point is a value that is often included in a weather forecast, but what is it? Dew point is defined as the temperature at which air is fully saturated with water vapor.
