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The average daily temperature, $T,$ for an area can be approximated by the following formula:

$T=T_{\text{m}\text{e}\text{a}\text{n}}+(T_{\text{p}\text{e}\text{a}\text{k}}-T_{\text{m}\text{e}\text{a}\text{n}})cos((t-t_{\text{p}\text{e}\text{a}\text{k}}))$

where $t=$ day of the year from $0$ to $364,T_{\text{m}\text{e}\text{a}\text{n}}=$ the average annual temperature, $T_{\text{p}\text{e}\text{a}\text{k}}=$ the peak temperature, $=$ the

frequency of the annual variation $(2\frac{}{365}),$ and $t_{\text{p}\text{e}\text{a}\text{k}}=$ the day of the peak temperature $($~~$205d).$ Parameters for some

U$.$S$.$ cities are listed here.

Develop a Python function that computes the average temperature between two days of the year for a particular city.

Test it for January$-$February in Yuma $(t=0$ to $59).$

The average temperature is

$C.$