The average daily temperature for an area can be approximated by the following function,

T = T _mean + (T _peak – T _mean) cos (ω (t – t _peak))

Where T _mean = the average annual temperature, T _peak = the peak temperature, ω = the frequency of the annual variation (= 2π/365), and t _peak = day of the peak temperature (≈ 205 d).Develop a program that computes the average temperature between two days of the year for a particular city. Test it for

(a) January – February (t = 0 to 59) in Miami, Florida (T mean = 22.1^o C; T _peak = 28.3^o C), and

(b) July–August (t = 180 to 242) in Boston, Massachusetts (T _mean = 10.7^o C; T _peak = 22.9^o C).