Universidade Federal de Ouro Preto, Núcleo de Pesquisas em Ciências Biológicas - NUPEB, St. Três, 408-462, Bauxita, 35400-000 Ouro Preto, MG, Brazil.
Universidade Federal de Ouro Preto, Laboratory of Ecology of Diseases and Forests, Departamento de Biodiversidade, Evolução e Meio Ambiente, St. Quatro, 786, Bauxita, 35400-000 Ouro Preto, MG, Brazil.
An Acad Bras Cienc. 2021 Aug 9;93(suppl 3):e20210431. doi: 10.1590/0001-3765202120210431. eCollection 2021.
A second deadlier wave of COVID-19 and the causes of the recent public health collapse of Manaus are compared with the Spanish flu events in that city, and Brazil. Historic sanitarian problems, and its hub position in the Brazilian airway network are combined drivers of deadly events related to COVID-19. These drivers were amplified by misleading governance, highly transmissible variants, and relaxation of social distancing. Several of these same factors may also have contributed to the dramatically severe outbreak of H1N1 in 1918, which caused the death of 10% of the population in seven months. We modelled Manaus parameters for the present pandemic and confirmed that lack of a proper social distancing might select the most transmissible variants. We succeeded to reproduce a first severe wave followed by a second stronger wave. The model also predicted that outbreaks may last for up to five and half years, slowing down gradually before the disease disappear. We validated the model by adjusting it to the Spanish Flu data for the city, and confirmed the pattern experienced by that time, of a first stronger wave in October-November 1918, followed by a second less intense wave in February-March 1919.
第二波更致命的 COVID-19 浪潮与马瑙斯最近公共卫生崩溃的原因,与该市和巴西的西班牙流感事件进行了比较。历史上的卫生问题,以及其作为巴西气道网络中心的位置,是与 COVID-19 相关的致命事件的共同驱动因素。误导性的治理、高度传染性的变体以及社会隔离的放松加剧了这些驱动因素。这些相同的因素中的一些也可能导致 1918 年 H1N1 的爆发,这在七个月内导致了 10%的人口死亡。我们为当前的大流行模拟了马瑙斯的参数,并证实了缺乏适当的社会隔离可能会选择最具传染性的变体。我们成功地再现了第一波严重的浪潮,随后是第二波更强的浪潮。该模型还预测,疫情可能会持续长达五年半,在疾病消失之前逐渐放缓。我们通过调整模型来适应该城市的西班牙流感数据来验证模型,并确认了当时经历的模式,即 1918 年 10 月至 11 月的第一波更强的浪潮,随后是 1919 年 2 月至 3 月的第二波较弱的浪潮。