wind chill

or wind·chill

[ wind-chil, win- ]
/ ˈwɪndˌtʃɪl, ˈwɪn- /

noun Meteorology.

the apparent temperature felt on the exposed human body owing to the combination of temperature and wind speed.
Also called wind·chill factor [wind-chil, win-,] /ˈwɪndˌtʃɪl ˌfæk tər, ˈwɪn-,/ wind·chill in·dex [wind-chil in-deks, win-] /ˈwɪndˌtʃɪl ˌɪn dɛks, ˈwɪn-/, chill factor.

Origin of wind chill

First recorded in 1945–50

Scientific definitions for wind-chill factor

wind-chill factor

The temperature of windless air that would have the same effect on exposed human skin as a particular combination of wind speed and air temperature. As the wind blows faster, heat is lost more quickly from exposed skin, making a person feel colder even though the air temperature remains the same. Also called chill factor