våtbulbstemperatur
Våtbulbstemperatur is a meteorological term that refers to the lowest temperature to which air can be cooled by the evaporation of water into it at a constant pressure. It is measured using a thermometer whose bulb is covered with a wet cloth or wick. As water evaporates from the wick, it cools the thermometer bulb, and the temperature reading will drop until it reaches a point where the rate of evaporation equals the rate of heat transfer from the surrounding air. The wet-bulb temperature is always lower than or equal to the dry-bulb temperature, which is the ambient air temperature measured by a standard thermometer.
The difference between the dry-bulb temperature and the wet-bulb temperature is an indicator of the humidity
Våtbulbstemperatur is an important parameter in various fields, including meteorology, agriculture, and human comfort studies. It