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It is easy to calculate the average value
of a finite set of numbers :

But how do we compute the average
temperature during a day if infinitely many temperatures readings are
possible? Figure 1 shows the graph of a temperature funtion T(t), where
t is mesured in hours and T in degrees Celcius, and a guess at the
average temperature, T(ave)
In general, let's try to compute the average value of a funtion , . We
start by dividing the interval [a,b] into n equal subintervals, each
with length . Then we choose points in
successive subintervals and calculate the average of the numbers :
(For example, if f represents a
temperature function and n=24, this means that we take temperature
readings every hour and then average them.) Since , we can write and
the average value becomes
If we let n increase, we would be
computing the average value of large nmber of closely spaced values.
(For example, we would be averaging temperature readings taken every
minute or even every second.) The limiting value is
by the definitiion of a definite
integral. Therefore, we define the average value of f on the interval
[a,b] as
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