This calculator shows the inter-relationship of air temperature and moisture content with dew point and wet-bulb temperature as measured by a psychrometric thermometer or sling psychrometer.
The amount of moisture air can hold is dependent on its temperature and pressure. The warmer the air the greater the quantity of water vapor it can contain. The air temperature is measured with a normal thermometer this is the Dry-Bulb reading. The actual amount of moisture known as the mixing ratio is measured in grams of water per kilogram of dry air. When air at a certain temperature is saturated it cannot hold any more moisture. The relative humidity of the air is the ratio of the actual amount of moisture in the air to the saturated amount.
We can use evaporation to measure the amount of moisture in the air. A wet cloth is placed over the bulb of a thermometer and then air blown over the cloth until the water evaporates. Since evaporation takes up heat, the thermometer will cool to a lower temperature than a thermometer with a dry bulb at the same time and place. The depression in Wet-Bulb temperature allows the humidity to be calculated. If the air is fully saturated (100% relative humidity) the water cannot evaporate, so both the wet and dry bulb temperatures are the same. The calculator will show the saturation mixing ratio in grams of water per kilogram of dry air of a given temperature, if the dry and wet bulb temperatures are set to the same value.
If partly saturated air is cooled without changing its pressure or amount of water vapor, a point is reached when it becomes saturated. The moisture will be given up as dew or ice crystals. This temperature is the Dew Point. Condensation will form on a bottle of cold beer, if the air in its vicinity is cooled below its dew point. Meteorological reports usually quote the temperature and dew point as well as the station pressure, moisture content and relative humidity can be calculated from these figures.
Back to Weather Page