Calculate wet-bulb temperature \(T_w\) (°C) from air temperature \(T\) (°C) and dewpoint temperature \(T_d\) (°C).
Details
Wet-bulb temperature \(T_w\) (°C) is the temperature at which air becomes saturated by evaporation at constant pressure. It is calculated using the formula:
$$T_w = T_d + 1/3 * (T - T_d)$$
where \(T\) is the air temperature and \(T_d\) is the dewpoint temperature, in degrees Celsius (°C).
The temperature input is converted to degree Celsius (°C) based on
the provided t_unit
before calculation.
References
Davis, Robert E., Glenn R. McGregor, and Kyle B. Enfield. “Humidity: A Review and Primer on Atmospheric Moisture and Human Health.” Environmental Research 144 (January 2016): 106–16. https://doi.org/10.1016/j.envres.2015.10.014.
Normand, Charles. “Energy in the Atmosphere.” Quarterly Journal of the Royal Meteorological Society 72, no. 312–313 (April 1946): 145–67. https://doi.org/10.1002/qj.49707231202.