Fast estimation of time-varying infectious disease transmission rates
Fig 8
Example of S(t) and β(t) reconstruction with an overestimate of S0 corrected by peak-to-peak iteration (PTPI).
[Panel A] Truncation step of PTPI (Box 5). Plotted is a reconstruction of true incidence Z(t) from a simulated reported incidence time series, before [Zk, black] and after [, yellow] smoothing with a 13-point central moving average. Vertical lines indicate peaks in
. The times of the first peak in
and the last peak occurring at the same phase of the cycle (in this case, the last peak) are denoted by ta and tb. [Panel B] Iteration step of PTPI (Box 6), where the initial estimates of both S0 = S(0) and S(ta) were taken to be 4 times the true (data-generating) value of S0. Plotted in grey are successive reconstructions of S(t) between times ta and tb, generated by updating the estimate of S(ta) with the estimate of S(tb) obtained in the previous iteration. Dashed continuations to the left of ta display estimation of S0 backwards in time from estimates of S(ta). Plotted in black is the result of reconstructing S(t) starting from the final estimate of S0, which was obtained after 25 iterations and had a relative error of roughly 1.4% (compared to 300% in the initial estimate). [Panel C] The sequence of reconstructions of β(t) corresponding to the estimates of S0 shown in Panel B. [Details] Twenty years of weekly reported incidence (Δt = 1 week, n = 1042) were simulated with environmental noise in transmission (ϵ = 0.5), demographic stochasticity, and random under-reporting of cases (prep = 0.25), using reference values (Table 1) for the remaining parameters. Z(t), S(t) and β(t) were reconstructed from reported incidence using the SI method without input error (apart from mis-specification of S0).