INTRODUCTION
Respiratory syncytial virus (RSV) is the leading cause of lower respiratory tract infections and hospitalizations in infants and young children worldwide [Reference Iwane1]. The incidence of RSV follows a seasonal pattern in temperate areas, with marked peaks in the winter season in the northern and southern hemispheres [Reference Hall2]. Despite this regular occurrence, differences exist in the region, duration, and magnitude of transmission periods [Reference Mullins3]. New information regarding the regional dynamics of RSV epidemics would broaden our understanding of RSV transmission, thus helping to predict or prevent these epidemics.
The incidence of RSV has been reported to exhibit seasonal variation in a number of different areas. For example, ambient temperature was found to be inversely associated with RSV activity in China and Tunisia [Reference Li4, Reference Fodha5]. In Malaysia, RSV cases were found to be directly correlated with rainy days and inversely correlated with temperature and humidity [Reference Khor6]. In the USA, it was found that RSV activity (1) peaked in summer and early autumn at sites with persistently warm temperatures and high humidity; (2) was maximal during winter, correlating with lower temperatures in temperate climates; and (3) was nearly continuous in areas where temperatures remained cold throughout the year [Reference Yusuf7]. In Germany and Italy, RSV infections were found to be correlated with decreasing temperature [Reference du Prel8, Reference Vandini9]. In Mexico and Turkey, an increase in RSV activity was found to be significantly associated with lower temperature and higher humidity [Reference Noyola and Mandeville10, Reference Turkish11]. In Hong Kong, RSV epidemics are more frequent during the rainy season when temperatures are high [Reference Sung12], while RSV cases in other studies showed a significant positive correlation with temperature and humidity [Reference Chan13]. In Singapore, the daily viral detection rates of RSV were found to be associated with higher temperatures, lower humidity, and higher diurnal temperature variation [Reference Chew14]. In Indonesia, it has been suggested that a significant increase in the risk of RSV is associated with an increase in temperature, humidity, and rainfall [Reference Omer15]. The observed seasonality of RSV both suggests that its incidence may be influenced by weather factors. Despite this speculation, the impact of diurnal temperature range (DTR) on the incidence of RSV, with adjustment for the mutual confounding between weather and other seasonal factors, has not been investigated in previous studies.
The present study examines the possible relationship between DTR and the incidence of RSV cases using surveillance data collected in Fukuoka, Japan, during the period of 2006–2012.
METHODS
Data sources
In Fukuoka Prefecture, which is located in the southwest of Japan, the number of RSV patients is reported to the Fukuoka Prefectural Government on a weekly basis from 120 sentinel medical institutions [Reference Onozuka, Hashizume and Hagihara16]. Cases are defined by clinical factors and laboratory tests. Clinical manifestations include a variety of respiratory illnesses, from cold-like symptoms to bronchitis, croup, and lower respiratory infections like bronchiolitis and pneumonia, according to the Act on Prevention of Infectious Diseases and Medical Care for Patients Suffering Infectious Diseases [17]. We obtained data that were reported by sentinel clinics and hospitals to the Fukuoka Institute of Health and Environmental Sciences, the municipal public health institute of the Fukuoka Prefectural Government. In addition, we also obtained data on daily minimum temperature, maximum temperature, average temperature, relative humidity and rainfall in Fukuoka Prefecture from the Japan Meteorological Agency. Weekly DTR was calculated as the weekly means for DTR. DTR was calculated as the daily maximum temperature minus the daily minimum temperature. Weekly means for temperature, relative humidity and rainfall were calculated from the daily records.
Statistical analysis
We used negative binomial generalized linear models with robust error variances to examine the relationship between the number of weekly RSV cases and DTR [Reference McCullagh and Nelder18]. We also included mean temperature, humidity, and rainfall in the model to control for the effects of weather factors. To account for the seasonality of RSV cases that were not directly due to the weather, the model included Fourier terms up to the sixth harmonic. Fourier terms can be used to re-create any periodic signal, such as a consistent seasonal pattern, using a linear combination of sine and cosine waves of varying wavelengths [Reference Stolwijk, Straatman and Zielhuis19]. The number of harmonics defines the lowest wavelength reproduced (i.e. the level of seasonal adjustment), with six harmonics corresponding to a wavelength of 9 weeks (i.e. one-sixth of a year). Indicator variables for the years under study were incorporated into the model to allow for long-term trends and inter-annual variations. To allow for autocorrelations, an autoregressive term of order 1 was incorporated into the models [Reference Brumback20]. Plots of model residuals, predicted and observed time-series plots, and the partial autocorrelation function of the residuals (Supplementary online data, Fig. S1) suggested that this adjustment for seasonal trends was adequate.
Based on the results of exploratory analyses with the lowest deviance of the above-described models, we considered lags (delays in effect) of up to 16 weeks when analysing the influence of DTR on the number of RSV cases. In initial analyses designed to identify the broad shape of any association, we fitted a natural cubic spline (3 d.f. ) [Reference Durrleman and Simon21] to the average DTR over lags of 0–16 weeks. We then fitted the data to linear models to quantify the change in disease risk associated with DTR. The choice of model (i.e. linear or threshold) [Reference Armstrong22] was based on our comparison of deviance in the models derived from likelihood ratio tests [Reference Daniels23]; models with lower deviance are preferred. When the difference in the values of deviance between the linear and best-fit threshold models was <3·84 (χ 2 value for 1 d.f. at the P = 0·05 level), the linear model was selected for simplicity. The observed values of deviances suggested that there was little change in the deviance between the linear and threshold models; thus, we assumed that linear models without a threshold were appropriate for assessing the associations between DTR and the incidence of RSV cases (the model is described in Protocol S1, online).
We also examined DTR–morbidity curves and lag effects in more detail using a quasi-likelihood Poisson regression model with distributed lag nonlinear model [Reference Gasparrini, Armstrong and Kenward24] adjusted for the confounding factors of temperature, humidity, rainfall, year, and seasonality. A distributed lag nonlinear model was developed on the basis of cross-basis function, which allows for the simultaneous estimation of possible nonlinear associations across lag periods [Reference Gasparrini, Armstrong and Kenward24]. Regarding the space of lags, we defined cubic spline with the natural constraint for the lag dimension of DTR. The knots for the spline for lags were placed at equally spaced values in the log scale of lags. Lag stratification was defined as 3 d.f. for the average DTR. We examined the possible nonlinear effect of DTR using a 3 d.f. natural cubic spline. As in the negative binomial generalized linear models, the maximum lag period of DTR was set at 16 weeks. Confounding factors of temperature, humidity, and rainfall using a 3 d.f. natural cubic spline with the maximum lag period of 16 weeks were also included in the model. Distributed lag nonlinear models are illustrated in Figure 3 (the model is described in Protocol S1, online).
As a sensitivity analysis, we also estimated DTR–morbidity relationships using different degrees of seasonal control (3rd and 12th harmonics). All statistical analyses were conducted using Stata v. 11.2 (Stata Corp., USA) and R statistical software (version 3.0.2) [25], using the dlnm package (version 2.0.6) [Reference Gasparrini, Armstrong and Kenward24].
Ethics approval
The ethics committee of the Fukuoka Prefectural Government Health and Environmental Research Advancement Committee approved this study on 27 December 2006 (reference no. 18-3515). Patients' records and other patients' information were anonymized and de-identified prior to analysis.
RESULTS
A total of 30 215 RSV cases from 2006 to 2012 were included in our analyses. Of these patients, 29 592(97·9%) were children aged 0–4 years, while the remaining 623 (2·1%) were aged ⩾5 years. Descriptive statistics for the number of patients based on age and weather variables are summarized in Table 1. In the analysis of the weekly reported number of RSV cases, the seasonal peak in cases was found to differ from year to year, although it typically occurred during the autumn or winter season (Fig. 1). The 7-year data were then analysed to identify relationships between the incidence of RSV and DTR.
The relationship between the relative risk (RR) of RSV and DTR using negative binomial generalized linear models is shown in Figure 2. Analysis of the crude relationship showed no clear relationship between the risk of RSV and DTR (Supplementary data, Fig. S2). After adjusting for seasonal, inter-year, temperature, humidity and rainfall variations, it was confirmed that a significant increase in the risk of RSV was associated with an increase in DTR. Notably, the time between DTR increase and the occurrence of RSV involved lag periods of 0–16 weeks, as indicated by the positive linear slope with increasing temperature (Fig. 2). Our analysis revealed that an increase of 1°C in DTR resulted in a significant increase in the number of RSV cases, with a RR of 3·30 [95% confidence interval (CI) 1·65–6·60]. We also found evidence for an association with mean temperature and the number of cases of RSV (RR 0·51, 95% CI 0·39–0·68) (Supplementary data, Fig. S3); however, a substantially nonlinear relationship was indicated between the RR of RSV cases and mean temperatures during a lag of 0–16 weeks (Fig. S3).
We also identified the RR of RSV by DTR using distributed lag nonlinear models at specific lag periods (4, 8, 12 weeks) and by lag at specific DTRs (5 °C, 7°C, 10°C), which corresponded to approximately the 5th, 50th, and 95th percentiles of DTR distribution, respectively (Fig. 3). The effects of high DTR were more prominent and persistent over longer lag periods.
To investigate whether the results were sensitive to the levels of control for seasonal patterns, the analyses were repeated using different degrees of seasonal control. Halving (three harmonics) or doubling (12 harmonics) the degree of seasonal control in sensitivity analyses only minimally changed the estimated effects of temperature and humidity. Specifically, the DTR model yielded a RR of 2·99 (95% CI 1·51–5·93) with three harmonics and 3·03 (95% CI 1·53–6·03) with 12 harmonics with respect to the incidence of RSV.
DISCUSSION
Our analysis of the effects of DTR on the incidence of RSV in Fukuoka, Japan, has yielded several notable findings. After adjustment for potential confounding by seasonal, inter-year, temperature, humidity and rainfall variations, we detected that the number of RSV cases increased with increasing DTR. This association appeared to have a major influence on the incidence of RSV infections. These findings indicate that these patterns should be considered when planning for early warnings of epidemics regarding the association between RSV cases and DTR.
Using negative binomial generalized linear models and distributed lag nonlinear models, we found that the number of RSV cases increased with higher DTR and was strongly positive at longer lag period lengths. The findings of the present study highlight the need to consider the weather effect of not only absolute temperature but also changes in DTR, particularly higher DTR. We speculate that this finding might be related to the failure of thermoregulation. The median incubation period of RSV is 4·4 days (95% CI 3·9–4·9) [Reference Lessler26], and infected persons are most contagious for 3–8 days following signs of illness [27]; however, some infants, young children, and people with weakened immune systems could be contagious for as long as 4 weeks [27]. In addition, recent research has suggested that it might be possible to be a carrier of the virus for ⩾3 months, because parts of the virus have been found present in some people long after symptoms have disappeared [Reference Schwarze28]. This fact is of significance as asymptomatic carriers are capable of spreading the causative viruses. These characteristics of RSV infections also highlight the need for more precise modelling of lag effects of weather on disease risk.
The results of this study support the notion that there is a significant relationship between DTR and RSV infections. While the exact mechanism remains unclear, a previous study suggested that sudden changes in weather conditions may affect humoral or cellular immunity [Reference Bull29]. Very young children have a relatively immature immune system [Reference Gerba, Rose and Haas30] and less self-care capacity [Reference Xu31], which might cause them to be more vulnerable to temperature change. Other studies have found that sudden changes in the temperature of inhaled air are associated with the release of inflammatory mediators by mast cells and thus cause more inflammatory nasal responses [Reference Graudenz32], which might also be related to higher RSV incidence. These findings might explain some of the mechanisms associated with the effect of DTR on RSV infections, and further study is needed to determine how the immune system is affected by DTR.
Although we did not have access to individual data of RSV cases in this study, a previous study suggested that the sharing of toys and other items in childcare centres or kindergartens might contribute to viral infections [Reference Ooi33]. Another study found that parents do not dress children appropriately for weather and active play [Reference Copeland34], which might be associated with the higher susceptibility of RSV infections. A recent study has also shown that children's opportunities for physical activities in childcare centres might often be curtailed because of inclement weather are often highly influenced by weather, outdoor play policies, and caregiver behaviours related to weather [Reference Copeland35]. Further investigation into these factors in the spread of epidemic foci may have implications for the control of RSV infections.
A few limitations of this study should be mentioned. First, surveillance data for RSV do not capture all cases in the community. The under-reporting of infections can occur anywhere in the reporting chain, from the initial tendency of a patient to seek health care to the recording of the case in the disease registry. The degree of under-reporting may also vary between epidemic and non-epidemic periods. Second, the participating sentinel medical institutions were recruited on a voluntary basis; however, this is not expected to significantly influence the validity of the comparisons over time, which is the subject of this study. Third, we did not control for air pollution; however, a previous study on the potential role of air pollutants on the pattern of RSV-related illness in infancy was unable to identify a clear link between a variety of air pollutants and the timing of the RSV epidemic [Reference Bhatt and Everard36].
The present study suggests that DTR might have a potentially significant role in pediatric infectious diseases. Recent studies have suggested that DTR might be an independent risk factor for childhood asthma and diarrhoea [Reference Xu37, Reference Xu38]. Infectious pathogens such as viruses, parasites and bacteria are devoid of thermostatic mechanisms, and reproduction and survival rates are strongly affected by fluctuations in temperature [Reference Meerburg and Kijlstra39, Reference Patz40]. Thus, clarification of the effects of weather variability on infectious disease epidemics is important for disease control and prevention by public health officials. In this study, the effects increased with higher DTR, highlighting that parents, medical staff, and public health officials would be made aware of the particularly high risk posed by high DTR and RSV-related morbidity in infants and young children. The results of this study may aid in the prediction of epidemics and in preparation for the effects of DTR on the epidemiology of RSV through implementation of preventive public health interventions, such as frequent hand washing, wiping of hard surfaces with soap and water or disinfectant, and the use of campaigns to encourage such preventative activities. It is expected that such activities might be practically useful for preventing or limiting the spread of RSV infections.
In conclusion, our study provides quantitative evidence that the number of RSV cases in Fukuoka, Japan, increased significantly with increased DTR over the study period. To our knowledge, this is the first report to quantify the impact of DTR on the number of RSV cases using time-series analysis. We therefore suggest that preventive measures for limiting the spread of RSV should be considered during extended periods of high DTR.
SUPPLEMENTARY MATERIAL
For supplementary material accompanying this paper visit http://dx.doi.org/10.1017/S0950268814001575.
ACKNOWLEDGEMENTS
We thank the Fukuoka Prefectural Government, Department of Public Health and Medical Affairs, Division of Public Health for their painstaking efforts in infectious disease surveillance in Fukuoka, Japan. The study was supported in part by a Grant-in-Aid for Scientific Research from the Ministry of Health, Labour and Welfare, Japan. The funder had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
DECLARATION OF INTEREST
None.