This study aims to examine the relationship between daily temperature and mortality in the Klang Valley, Malaysia over the period 2006 – 2015. A quasi-Poisson generalized linear model combined with a distributed lag non-linear model (DLNM) was used to estimate the association between mean temperature and mortality categories (natural, cardiovascular, and respiratory disease). Particulate matter with aerodynamic diameter below than 10 micrometer (PM10) and surface ozone (O3) has been adjusted as a potential confounding factor. Both cold and heat effects were associated with mortality categories. The relative risks of natural mortality associated with an extreme cold temperature (1st percentile of temperature, 25.2 °C) and an extreme hot temperature (99th percentile of temperature, 30.2 °C) relative to the minimum mortality temperature (28.2 °C) were 1.17 (95% confidence interval (CI): 0.97, 1.41) and 1.11 (95% CI: 0.93, 1.32) for lag 0-21, respectively. Heat effects were immediate whereas cold effects were delayed and lasted longer. People with respiratory diseases, the elderly and women were the most vulnerable groups when it came to the effects of extremely high temperatures. The extreme temperatures did not dramatically change the temperature-mortality risk estimates made before and after adjustments for air pollutant (PM10 and O3) levels.

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Posted 13 Apr, 2021
On 29 Apr, 2021
Invitations sent on 08 Apr, 2021
On 31 Mar, 2021
On 30 Mar, 2021
Posted 13 Apr, 2021
On 29 Apr, 2021
Invitations sent on 08 Apr, 2021
On 31 Mar, 2021
On 30 Mar, 2021
This study aims to examine the relationship between daily temperature and mortality in the Klang Valley, Malaysia over the period 2006 – 2015. A quasi-Poisson generalized linear model combined with a distributed lag non-linear model (DLNM) was used to estimate the association between mean temperature and mortality categories (natural, cardiovascular, and respiratory disease). Particulate matter with aerodynamic diameter below than 10 micrometer (PM10) and surface ozone (O3) has been adjusted as a potential confounding factor. Both cold and heat effects were associated with mortality categories. The relative risks of natural mortality associated with an extreme cold temperature (1st percentile of temperature, 25.2 °C) and an extreme hot temperature (99th percentile of temperature, 30.2 °C) relative to the minimum mortality temperature (28.2 °C) were 1.17 (95% confidence interval (CI): 0.97, 1.41) and 1.11 (95% CI: 0.93, 1.32) for lag 0-21, respectively. Heat effects were immediate whereas cold effects were delayed and lasted longer. People with respiratory diseases, the elderly and women were the most vulnerable groups when it came to the effects of extremely high temperatures. The extreme temperatures did not dramatically change the temperature-mortality risk estimates made before and after adjustments for air pollutant (PM10 and O3) levels.

Figure 1

Figure 2

Figure 3
This is a list of supplementary files associated with this preprint. Click to download.
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