Johnsen Morten Guldborg, Christiansen Lasse Engbo, Græsbøll Kaare
DTU Compute, Technical University of Denmark, Building 324, Richard Petersens Plads, 2800 Kgs. Lyngby, Denmark.
Statens Serum Institut, Artillerivej 5, 2300 Kbh S., Denmark.
Microb Risk Anal. 2022 Dec;22:100235. doi: 10.1016/j.mran.2022.100235. Epub 2022 Oct 8.
From march 2020 to march 2022 covid-19 has shown a consistent pattern of increasing infections during the Winter and low infection numbers during the Summer. Understanding the effects of seasonal variation on covid-19 spread is crucial for future epidemic modelling and management. In this study, seasonal variation in the transmission rate of covid-19, was estimated based on an epidemic population model of covid-19 in Denmark, which included changes in national restrictions and introduction of the -variant covid-19 strain, in the period March 2020 - March 2021. Seasonal variation was implemented as a logistic temperature dependent scaling of the transmission rate, and parameters for the logistic relationship was estimated through rejection-based approximate bayesian computation (ABC). The likelihoods used in the ABC were based on national hospital admission data and seroprevalence data stratified into nine and two age groups, respectively. The seasonally induced reduction in the transmission rate of covid-19 in Denmark was estimated to be , (95% CI [ ; ]), when moving from peak Winter to peak Summer. The reducing effect of seasonality on transmission rate per C in daily average temperature were shown to vary based on temperature, and were estimated to be pr. 1 C around C; pr. 1 C around C; and pr. 1 C around a daily average temperature of 11 C.
从2020年3月到2022年3月,新冠病毒感染呈现出冬季感染人数持续增加、夏季感染人数较低的一致模式。了解季节变化对新冠病毒传播的影响对于未来的疫情建模和管理至关重要。在本研究中,基于丹麦的新冠病毒疫情人口模型估计了新冠病毒传播率的季节变化,该模型包括2020年3月至2021年3月期间国家限制措施的变化以及新冠病毒变异株的引入。季节变化通过对传播率进行与温度相关的逻辑缩放来实现,并且通过基于拒绝的近似贝叶斯计算(ABC)估计逻辑关系的参数。ABC中使用的似然性分别基于分为九个年龄组和两个年龄组的国家医院入院数据和血清阳性率数据。从冬季高峰到夏季高峰时,丹麦新冠病毒传播率因季节导致的下降估计为 ,(95%置信区间[ ; ])。结果表明,季节性对每日平均温度每升高1摄氏度时传播率的降低作用会因温度而异,在约 摄氏度时估计为每1摄氏度 ;在约 摄氏度时为每1摄氏度 ;在每日平均温度为11摄氏度左右时为每1摄氏度 。