Duan Yu, Huang Xiao-Lei, Wang Yu-Jie, Zhang Jun-Qing, Zhang Qi, Dang Yue-Wen, Wang Jing
Department of Epidemiology and Biostatistics, School of Public Health, Anhui Medical University, No. 81, Meishan Road, Hefei, Anhui, 230032, China.
Center for Disease Control and Prevention of Hefei City, Hefei, China.
Int J Biometeorol. 2016 Oct;60(10):1543-1550. doi: 10.1007/s00484-016-1145-8. Epub 2016 Mar 1.
Studies on scarlet fever with meteorological factors included were few. We aimed to illustrate meteorological factors' effects on monthly incidence of scarlet fever. Cases of scarlet fever were collected from the report of legal infectious disease in Hefei City from 1985 to 2006; the meteorological data were obtained from the weather bureau of Hefei City. Monthly incidence and corresponding meteorological data in these 22 years were used to develop the model. The model of auto regressive integrated moving average with covariates was used in statistical analyses. There was a highest peak from March to June and a small peak from November to January. The incidence of scarlet fever ranges from 0 to 0.71502 (per 10 population). SARIMAX (1,0,0)(1,0,0) model was fitted with monthly incidence and meteorological data optimally. It was shown that relative humidity (β = -0.002, p = 0.020), mean temperature (β = 0.006, p = 0.004), and 1 month lag minimum temperature (β = -0.007, p < 0.001) had effect on the incidence of scarlet fever in Hefei. Besides, the incidence in a previous month (AR(β) = 0.469, p < 0.001) and in 12 months before (SAR(β) = 0.255, p < 0.001) was positively associated with the incidence. This study shows that scarlet fever incidence was negatively associated with monthly minimum temperature and relative humidity while was positively associated with mean temperature in Hefei City, China. Besides, the ARIMA model could be useful not only for prediction but also for the analysis of multiple correlations.
关于猩红热与气象因素的研究较少。我们旨在阐明气象因素对猩红热月发病率的影响。从合肥市1985年至2006年法定传染病报告中收集猩红热病例;气象数据来自合肥市气象局。利用这22年的月发病率和相应气象数据建立模型。统计分析采用带协变量的自回归积分滑动平均模型。3月至6月有一个最高峰值,11月至1月有一个小峰值。猩红热发病率范围为0至0.71502(每10万人)。SARIMAX(1,0,0)(1,0,0)模型与月发病率和气象数据拟合最优。结果表明,相对湿度(β = -0.002,p = 0.020)、平均温度(β = 0.006,p = 0.004)和滞后1个月的最低温度(β = -0.007,p < 0.001)对合肥猩红热发病率有影响。此外,前一个月的发病率(AR(β) = 0.469,p < 0.001)和12个月前的发病率(SAR(β) = 0.255,p < 0.001)与发病率呈正相关。本研究表明,中国合肥市猩红热发病率与月最低温度和相对湿度呈负相关,与平均温度呈正相关。此外,ARIMA模型不仅可用于预测,还可用于多重相关性分析。