I tried to do it but I obtain parts like: $$\int _{-\infty }^{\infty }cos\left[2\left(nw_0+\theta \right)\right]dn$$, that I supposed it has no sense because $$cos[2(nw_0+\theta)]$$ is oscillant...
2026-03-28 05:01:14.1774674074
How to calculate the autocorrelation function
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Here is R code to simulate the first $m = 10\,000$ steps of a 2-state Markov chain for weather $W$ $(0=$sun, $1=$rain$)$ in a place where weather on any one day is heavily influenced by weather the previous day. Over the long run, it rains $b/(a+b) = 1/3$ of the time, (poorly) estimated by $0.28$ over the simulated $m$ days. [Runs of rainy and sunny days are so long that estimation is difficult.]
The panel at left below shows successive values of $W$ the panel at right shows the ACF function of the $W$'s.
Roughly speaking the autocorrelation of lag $1$ is the correlation of the sequences $(W_1, W_2, \dots, W_{m-1})$ and $(W_2, W_3, \dots, W_m).$ The exception is that sample mean and variance use the entire sequence, not just the $m-1$ overlapping values. Autocorrelations of other lags $\ell$ are defined analogously:
$$r_{\ell} =\frac{ \sum_{i=1}^{m-\ell}(W_i - \bar W)(W_{i+\ell} - \bar W)}{(n-1)S^2}.$$
The ACF of a observed values $(W_1, \dots W_m)$ gives the list of autocorrelations for lags $\ell = 0, 1, 2, \dots.$
The autocorrelation of lag $0$ is $1.$ Autocorrelations decrease with $\ell.$ Autocorrelations within the dotted horizontal bands are considered not significantly different from $0.$
So by the end of a month the weather on the first day of the month no longer affects the current weather. (In an ergodic Markov Chain, Markovian one-step dependence 'wears off' over time.)