| Literature DB >> 33506154 |
Raúl Patricio Fernández-Naranjo1, Eduardo Vásconez-González1, Katherine Simbaña-Rivera1, Lenin Gómez-Barreno1, Juan S Izquierdo-Condoy1, Doménica Cevallos-Robalino2, Esteban Ortiz-Prado1.
Abstract
The growth of COVID-19 pandemic throughout more than 213 countries around the world have put a lot of pressures on governments and health services to try to stop the rapid expansion of the pandemic. During 2009, H1N1 Influenza pandemic, statistical and mathematical methods were used to track how the virus spreads around countries. Most of these models that were developed at the beginning of the XXI century are based on the classical susceptible-infected-recovered (SIR) model developed almost a hundred years ago. The evolution of this model allows us to forecast and compute basic and effective reproduction numbers (R t and R 0 ), measures that quantify the epidemic potential of a pathogen and estimates different scenarios. In this study, we present a traditional estimation technique for R 0 with statistical distributions by best fitting and a Bayesian approach based on continuous feed of prior distributions to obtain posterior distributions and computing real time R t . We use data from COVID-19 officially reported cases in Ecuador since the first confirmed case on February 29th. Because of the lack of data, in the case of R 0 we compare two methods for the estimation of these parameters below exponential growth and maximum likelihood estimation. We do not make any assumption about the evolution of cases due to limited information and we use previous methods to compare scenarios about R 0 and in the case of R t we used Bayesian inference to model uncertainty in contagious proposing a new modification to the well-known model of Bettencourt and Ribeiro based on a time window of m days to improve estimations. Ecuadorian R 0 with exponential growth criteria was 3.45 and with the maximum likelihood estimation method was 2.93. The results show that Guayas, Pichincha and Manabí were the provinces with the highest number of cases due to COVID-19. Some reasons explain the increased transmissibility in these localities: massive events, population density, cities dispersion patterns, and the delayed time of public health actions to contain pandemic. In conclusion, this is a novel approach that allow us to measure infection dynamics and outbreak distribution when not enough detailed data is available. The use of this model can be used to predict pandemic distribution and to implement data-based effective measures.Entities:
Keywords: Basic reproduction factor; Bayesian inference; COVID-19; Ecuador; R0; Real time reproduction factor
Year: 2021 PMID: 33506154 PMCID: PMC7811040 DOI: 10.1016/j.idm.2020.12.012
Source DB: PubMed Journal: Infect Dis Model ISSN: 2468-0427
Fig. 1Daily Rt estimation for Ecuador. a) Calcid Rt factor sequence using the Bettencourt’s model, from February 28th to May 5th, 2020, shows its highest peak on March 16 (Rt: 4.50, 95% HDI: 4.06–4.91). b) Rt factor sequence calculated using the proposed model from February 28th to May 5th, 2020, shows its highest peak on March 14 (Rt: 3.77, 95% HDI: 3.01–4.47). The trend followed by the daily recommendations in both models, represent a similar behaviour, however, the recommendations from the Bettencourt model are plotted with the most exaggerated main Rt values compared to those belonging to the proposed model.
Fig. 2Daily Rt estimation for Ecuadorian Provinces by proposed model.
R0 and Rt estimates for provinces in Ecuador.
| Province | R0 EG (95%CI) | R0 MLE (95%CI) | Max Rt proposed model (95%HDI) | Max Rt Bettencourt model (95%HDI) |
|---|---|---|---|---|
| Azuay | 1.08 (1.04–1.12) | 1.18 (1.05–1.33) | 2.62 (0–5.81) | 5.71 (3.24–7.63) |
| Bolivar | 1.02 (0.94–1.10) | 1.2 (0.95–1.49) | 1.76 (0.31–3.04) | 2.75 (1.2–4.01) |
| Cañar | 2.36 (2.03–2.74) | 2.25 (1.82–2.75) | 2.84 (0.95–4.45) | 4.05 (2.58–5.42) |
| Carchi | 1.36 (1.16–1.57) | 1.6 (1.1–2.25) | 2.15 (0.44–3.75) | 2.24 (0.24–3.91) |
| Chimborazo | 2.16 (1.44–3.1) | 2.45 (1.59–3.56) | 2.62 (0–5.81) | 2.88 (0.17–4.99) |
| Cotopaxi | 1.26 (1.1–1.44) | 1.49 (1.1–1.96) | 1.89 (0.02–3.41) | 2.52 (0.68–4.21) |
| El Oro | 3.16 (2.61–3.82) | 3.14 (2.5–3.89) | 2.01 (0–3.95) | 2.67 (1.93–3.36) |
| Esmeraldas | 3.5 (2.44–4.94) | 3.45 (2.28–4.97) | 3.77 (0–7.43) | 3.87 (2.6–4.97) |
| Galapagos | 2.12 (1.72–2.63) | 2.95 (1.93–4.27) | 2.81 (1.01–4.34) | 5.12 (3.85–6.25) |
| Guayas | 3.66 (3.55–3.77) | 3.08 (2.94–3.22) | 3.96 (3.11–4.76) | 4.91 (4.4–5.39) |
| Imbabura | 1.27 (1.12–1.44) | 1.39 (1.02–1.85) | 1.89 (0–4.49) | 2.62 (0–4.94) |
| Loja | 1.81 (1.55–2.11) | 1.9 (1.49–2.37) | 1.67 (0.4–2.83) | 5.39 (0.55–8.7) |
| Los Rios | 1.28 (1.24–1.33) | 1.2 (1.09–1.32) | 2.35 (0.61–3.88) | 2.36 (1.08–3.43) |
| Manabí | 1.33 (1.27–1.4) | 1.43 (1.28–1.6) | 3.77 (0–7.44) | 3.77 (0.87–6.22) |
| Morona Santiago | 1.57 (1.21–1.99) | 1.84 (1.13–2.8) | 2.15 (0–4.96) | 3.77 (0–7.45) |
| Napo | 1.86 (1.43–2.42) | 1.93 (1.09–3.13) | 1.89 (0–3.43) | 1.95 (0.22–3.46) |
| Orellana | 2.08 (1.63–2.68) | 2.25 (1.34–3.5) | 2.01 (0–3.96) | 2.62 (0–5.76) |
| Pastaza | 1.64 (1.34–2.01) | 2.08 (1.37–2.99) | 2.01 (0.12–3.48) | 3.04 (1.14–4.64) |
| Pichincha | 1.26 (1.23–1.29) | 1.32 (1.23–1.4) | 2.83 (1.27–4.14) | 3.04 (1.75–4.08) |
| Santa Elena | 1.44 (1.3–1.59) | 1.53 (1.31–1.78) | 2.43 (0.97–3.84) | 3.77 (2.33–5.05) |
| Santo Domingo | 1.5 (1.38–1.63) | 1.64 (1.37–1.94) | 1.6 (0.75–2.32) | 2.23 (1.22–3.18) |
| Sucumbíos | 3.44 (2.19–5.62) | 3.29 (1.5–6.13) | 2.15 (0–5.02) | 3.77 (0.48–6.3) |
| Tungurahua | 1.46 (1.26–1.67) | 1.61 (1.23–2.07) | 2.15 (0.11–3.92) | 2.62 (0.7–4.26) |
| Zamora Chinchipe | 3.95 (2.29–6.92) | 4.91 (2.11–9.49) | 3.04 (0.35–5.03) | 7.16 (4.89–9.1) |
MLE: Maximum likelihood estimation; EG: Exponential growth; Max: Maximum, CI: confidence interval; HDI: High density interval.