Abstract
Based on the total thermal resistance required by a human model to effect equilibrium, a scale is prepared showing apparent temperature for any combination of dry-bulb temperature, vapor pressure, wind speed and extra radiation likely to be encountered meteorologically. Application to normal midday climates of the United States shows that dry-bulb temperature is modified by the three other variables by from -5 to +7 K. -from Author
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CITATION STYLE
Steadman, R. G. (1984). A universal scale of apparent temperature. Journal of Climate & Applied Meteorology, 23(12), 1674–1687. https://doi.org/10.1175/1520-0450(1984)023<1674:AUSOAT>2.0.CO;2
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