Plateau Atmosphere and Environment Key Laboratory of Sichuan Province, College of Atmospheric Science, Chengdu University of Information Technology, Chengdu, 610225, Sichuan, China.
Shenzhen National Climate Observatory, Shenzhen Meteorological Bureau, Shenzhen, 518000, China.
Int J Biometeorol. 2022 Jan;66(1):163-173. doi: 10.1007/s00484-021-02204-y. Epub 2021 Oct 25.
Under the variant climate conditions in the transitional regions between tropics and subtropics, the impacts of climate factors on influenza subtypes have rarely been evaluated. With the available influenza A (Flu-A) and influenza B (Flu-B) outbreak data in Shenzhen, China, which is an excellent example of a transitional marine climate, the associations of multiple climate variables with these outbreaks were explored in this study. Daily laboratory-confirmed influenza virus and climate data were collected from 2009 to 2015. Potential impacts of daily mean/maximum/minimum temperatures (T/T/T), relative humidity (RH), wind velocity (V), and diurnal temperature range (DTR) were analyzed using the distributed lag nonlinear model (DLNM) and generalized additive model (GAM). Under its local climate partitions, Flu-A mainly prevailed in summer months (May to June), and a second peak appeared in early winter (December to January). Flu-B outbreaks usually occurred in transitional seasons, especially in autumn. Although low temperature caused an instant increase in both Flu-A and Flu-B risks, its effect could persist for up to 10 days for Flu-B and peak at 17 C (relative risk (RR) = 14.16, 95% CI: 7.46-26.88). For both subtypes, moderate-high temperature (28 C) had a significant but delayed effect on influenza, especially for Flu-A (RR = 26.20, 95% CI: 13.22-51.20). The Flu-A virus was sensitive to RH higher than 76%, while higher Flu-B risks were observed at both low (< 65%) and high (> 83%) humidity. Flu-A was active for a short term after exposure to large DTR (e.g., DTR = 10 C, RR = 12.45, 95% CI: 6.50-23.87), whereas Flu-B mainly circulated under stable temperatures. Although the overall wind speed in Shenzhen was low, moderate wind (2-3 m/s) was found to favor the outbreaks of both subtypes. This study revealed the thresholds of various climatic variables promoting influenza outbreaks, as well as the distinctions between the flu subtypes. These data can be helpful in predicting seasonal influenza outbreaks and minimizing the impacts, based on integrated forecast systems coupled with short-term climate models.
在热带和亚热带过渡地区的变异气候条件下,气候因素对流感亚型的影响很少得到评估。本研究利用中国深圳作为海洋性过渡气候的典型范例,获得了可用的甲型流感(Flu-A)和乙型流感(Flu-B)爆发数据,探讨了多种气候变量与这些爆发的关联。本研究收集了 2009 年至 2015 年的每日实验室确诊流感病毒和气候数据。使用分布式滞后非线性模型(DLNM)和广义相加模型(GAM)分析日平均/最高/最低温度(T/T/T)、相对湿度(RH)、风速(V)和日较差(DTR)的潜在影响。在当地气候分区下,Flu-A 主要在夏季(5 月至 6 月)流行,初冬(12 月至 1 月)出现第二个高峰。Flu-B 爆发通常发生在过渡季节,尤其是秋季。尽管低温会立即增加 Flu-A 和 Flu-B 的风险,但这种影响可以持续 10 天,对于 Flu-B 来说,峰值出现在 17°C(相对风险(RR)=14.16,95%CI:7.46-26.88)。对于这两种亚型,中高温(28°C)对流感有显著但延迟的影响,特别是对于 Flu-A(RR=26.20,95%CI:13.22-51.20)。流感病毒 A 对高于 76%的相对湿度敏感,而在低湿度(<65%)和高湿度(>83%)时,流感病毒 B 的风险较高。Flu-A 在暴露于较大的日较差(例如,DTR=10°C,RR=12.45,95%CI:6.50-23.87)后会短期活跃,而 Flu-B 主要在稳定温度下循环。尽管深圳的整体风速较低,但发现中等风速(2-3m/s)有利于两种亚型的爆发。本研究揭示了促进流感爆发的各种气候变量的阈值,以及流感亚型之间的区别。这些数据可以通过结合短期气候模型的综合预测系统来帮助预测季节性流感爆发并将其影响降到最低。