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广州市气象因素对猩红热发病影响及交互作用分析:基于2014—2022年监测资料

Effects and interactions of meteorological factors on the incidence of scarlet fever in Guangzhou: an analysis based on surveillance data from 2014 to 2022

  • 摘要:
    目的  分析2014年—2022年广州市气象因素对猩红热发病的影响。
    方法  分析广州市猩红热发病情况。使用Spearman相关、分布滞后非线性模型和双变量响应模型,评估气象因素对猩红热发病风险的影响。
    结果  平均温度(rs= –0.255)、风速(rs=0.126)、气压(rs=0.116)和日照时长(rs= –0.177)与猩红热发病显著相关(P<0.05)。平均温度对猩红热发病呈低温危害效应和高温保护效应,当气温在12 ℃时,相对危险度(RR)达到峰值(1.41,95%CI=1.09~1.83)。风速和日照时长与猩红热发病的关系总体呈波浪形,风速在4.3 m/s时危害效应最强(RR=5.67,95%CI=1.61~19.84);当日照时长>8 h/d时,风险效应明显增强,但差异无统计学意义(95%CI=0.97~4.95)。气压对猩红热发病呈低气压的保护效应和高气压的危害效应;当气压为1 016.5 hPa时,RR达到峰值(2.26,95%CI=1.70~3.02)。低温、高风速、日照时间长、气压高等气象因素的联合交互作用会进一步提升广州市猩红热发病率。
    结论  平均温度、风速、气压和日照时长与猩红热发病呈非线性关系和滞后效应,且存在交互作用。因此,可以相应调整猩红热预防控制的工作重点。

     

    Abstract:
    Objective To analyze the effects of meteorological factors on the incidence of scarlet fever in Guangzhou from 2014 to 2022.
    Methods The epidemiological characteristics of scarlet fever in Guangzhou were described. The effects of meteorological factors on the risk of scarlet fever were evaluated via Spearman correlation analysis, distributed lag non-linear models, and bivariate response models.
    Results The incidence of scarlet fever had correlations (P < 0.05) with mean temperature (rs = −0.255), wind speed (rs = −0.126), air pressure (rs = 0.116), and sunshine duration (rs = −0.177). Mean temperature exhibited risk effects at lower temperatures and protective effects at higher temperatures, with the relative risk (RR) peaking at 1.41 (95%CI: 1.09–1.83) when the temperature was 12 ℃. The relationships of wind speed and sunshine duration with incidence of scarlet fever followed a wave-like pattern, with the strongest risk effect observed at a wind speed of 4.3 m/s (RR = 5.67, 95%CI: 1.61–19.84). When sunshine duration exceeded 8 h/d, the risk effect increased markedly, albeit not statistically significant (95%CI: 0.97–4.95). Air pressure demonstrated protective effects at low levels and risk effects at high levels on the incidence of scarlet fever, with the RR peaking at 2.26 (95%CI: 1.70–3.02) when the air pressure was 1 016.5 hPa. The interactions of meteorological factors such as low temperature, high wind speed, long sunshine duration, and high air pressure further contributed to an increase in scarlet fever incidence in Guangzhou.
    Conclusions Mean temperature, wind speed, air pressure, and sunshine duration demonstrate non-linear relationships and lag effects with the incidence of scarlet fever, with interactions among each other. Therefore, adjusting these meterological factors can be taken as a focus of prevention and control efforts for scarlet fever.

     

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