"WIND CHILL"
Piecewise defined functions in 2 variables
Many situations in every day life are modeled by these functions.
The number of variables Involved may be more than 1. Calculus of 2 or
more variables is studied in Calculus III. One popular everyday example
is a model for determining the WIND CHILL (how cold it
feels considering both the temperature & the velocity of the wind.
This is a complicated model. Other popular 1-variable models are for
postal & telephone rates. The latter are in a class called "step
functions." The following is a model used for Wind Chill. W(T,V) gives
the effective temperature taking into consideration the present
temperature, T and the velocity of the wind, V.
(Adapted from UMAP)
T
for V between 0 & 4 (inclusive)
W(T,V)= { 0.0817(5.81+3.71sqr(V) -0.25V)(T-91.4)+91.4 for 4 < V < 45
1.60T-55
for V = 45 or greater
Example: W(40,20) would represent the perceived temperature
(degrees F) with a present temperature of 40 degrees F and wind
velocity of 20 mph. V=20 will use the middle line in the above defined
function, since 20 falls between 4 & 45.
Substituting T=40 & V=20 in the above (use middle line), we would
get 18.3 degrees F. Needless to say, most people using the wind chill
temp would not use the formula (many do not know it or once they see
it, they would like to forget it quickly). Instead, charts are given
showing the results for a wide range of combinations of T & V.
NOTE: In the Fall of 2001, the National Weather Service revised the formula based on new research on how cold air affects people. Consequently, new charts have been used for wind chill and the numbers will not be consistent with the above formula. They will turn out to be significantly different.
The revised formula for all combinations of T & V is
W(T,V)= 91.4 - (0.474677 - 0.020425V + 0.303107sqr(V))(91.4 - T)
Not a piecewise defined function.