194
14.19 In Chapter 11, we explained the concept of windchill factors. We said that the
heat transfer rates from your body to the surrounding increase on a cold, windy
day. Simply stated, you lose more body heat on the cold, windy day than you do
on a calm day. The windchill index accounts for the combined effect of wind
speed and the air temperature. It accounts for the additional body heat loss that
occurs on a cold, windy day. The old windchill values were determined
empirically, and a common correlation used to determine the windchill index was
)33)(1045.10( a
TVVWCI
where
WCI = Wind Chill Index (kcal/m2·h)
V = wind speed (m/s)
Ta = ambient air temperature (C)
and the value 33 is the body surface temperature in degree Celsius.
The more common equivalent wind chill temperature Tequivalent (C)
was given by
33)33)(28.045.1027.5(045.0 5.0 aequivalent TVVT
Note that V is expressed in km/h.
Create a table that shows the windchill temperatures for the range of ambient air
temperature -30 C < Ta < 10 C and wind speed of 20 km/h < V < 80 km/h as
shown in the accompanying spreadsheet.