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Using a distributed lag non-linear model to identify impact of temperature variables on haemorrhagic fever with renal syndrome in Shandong Province

Published online by Cambridge University Press:  06 July 2018

Qinqin Xu
Affiliation:
Department of Biostatistics, School of Public Health, Shandong University, Jinan, Shandong, China
Runzi Li
Affiliation:
Department of Biostatistics, School of Public Health, Shandong University, Jinan, Shandong, China
Shannon Rutherford
Affiliation:
School of Medicine & Centre for Environment and Population Health, Griffith University, Bristol city, Queensland, Australia
Cheng Luo
Affiliation:
Department of Biostatistics, School of Public Health, Shandong University, Jinan, Shandong, China
Yafei Liu
Affiliation:
Department of Biostatistics, School of Public Health, Shandong University, Jinan, Shandong, China
Zhiqiang Wang
Affiliation:
Shandong Center for Disease Control and Prevention, Jinan, Shandong, China
Xiujun Li*
Affiliation:
Department of Biostatistics, School of Public Health, Shandong University, Jinan, Shandong, China
*
Author for correspondence: Xiujun Li, E-mail: xjli@sdu.edu.cn
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Abstract

Haemorrhagic fever with renal syndrome (HFRS) is transmitted to humans mainly by rodents and this transmission could be easily influenced by meteorological factors. Given the long-term changes in climate associated with global climate change, it is important to better identify the effects of meteorological factors of HFRS in epidemic areas. Shandong province is one of the most seriously suffered provinces of HFRS in China. Daily HFRS data and meteorological data from 2007 to 2012 in Shandong province were applied. Quasi-Poisson regression with the distributed lag non-linear model was used to estimate the influences of mean temperature and Diurnal temperature range (DTR) on HFRS by sex, adjusting for the effects of relative humidity, precipitation, day-of-the-week, long-term trends and seasonality. A total of 6707 HFRS cases were reported in our study. The two peaks of HFRS were from March to June and from October to December, particularly, the latter peak in 2012. The estimated effects of mean temperature and DTR on HFRS were non-linear. The immediate and strong effect of low temperature and high DTR on HFRS was found. The lowest temperature −8.86°C at lag 0 days indicated the largest related relative risk (RRs) with the reference (14.85 °C), respectively, 1.46 (95% CI 1.11–1.90) for total cases, 1.33 (95% CI 1.00–1.78) for the males and 1.76 (95% CI 1.12–2.79) for the females. Highest DTR was associated with a higher risk on HFRS, the largest RRs (95% CI) were obtained when DTR = 15.97 °C with a reference at 8.62 °C, with 1.26 (0.96–1.64) for total cases and 1.52 (0.97–2.38) for the female at lag 0 days, 1.22 (1.05–1.41) for the male at lag 5 days. Non-linear lag effects of mean temperature and DTR on HFRS were identified and there were slight differences for different sexes.

Information

Type
Original Paper
Copyright
Copyright © Cambridge University Press 2018 
Figure 0

Fig. 1. Age and gender distribution of HFRS cases in Shandong, 2007–2012.

Figure 1

Fig. 2. Monthly distribution of HFRS incidence in Shandong, 2007–2012.

Figure 2

Fig. 3. The sequence diagram of daily HFRS cases and meteorological variables (daily mean temperature, DTR (Diurnal temperature range)) in Shandong, 2007–2012.

Figure 3

Table 1. Summary statistics for daily HFRS cases and meteorological variables in Shandong, 2007–2012 (n = 6707)

Figure 4

Table 2. Spearman's correlation coefficients between meteorological factors and daily HFRS cases in Shandong, 2007–2012 (rs)

Figure 5

Fig. 4. Three-D plots of relative risk (RR) for HFRS along daily mean temperature and lags with reference at 14.83 °C for the total cases (a), male cases (b) and female cases (c) and DTR (Diurnal temperature range) with reference at 8.62 °C for the total cases (d), male cases (e) and female cases (f) by DLNM models.

Figure 6

Fig. 5. The relative risk (RR) of HFRS by the daily mean temperature at a specific lag day (0, 5, 10, 15, 20, 25 and 30 days) for total cases, controlling for relative humidity, precipitation, weekly effects and seasonality and long trends. The maximum likelihood estimate of RRs is shown as smooth red lines and the pointwise 95% confidence intervals are shown in the gray regions.

Figure 7

Fig. 6. The relative risk (RR) of HFRS by DTR at a specific lag day (0, 5, 10, 15, 20, 25 and 30 days) for total cases, controlling for relative humidity, precipitation, sunshine duration, weekend effects, seasonality and long trends. The maximum likelihood estimate of RRs is shown as smooth red lines and the pointwise 95% confidence intervals are shown in the gray regions.

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