Abstract

Extreme temperature events have affected Chinese city residents more frequently and intensively since the early 2000s, but few studies have identified the impacts of extreme temperature on mortality in different city clusters of China. This study first used a distributed lag, nonlinear model to estimate the county/district-specific effects of extreme temperature on nonaccidental and cardiovascular mortality. The authors then applied a multivariate meta-analysis to pool the estimated effects in order to derive regional temperature–mortality relationship in three large city clusters—the Beijing-Tianjin-Hebei (BTH) region, the Yangtze River Delta (YRD), and the Pearl River Delta (PRD), which represent northern and southern regions. With 0–3 days’ lag, the strongest heat-related mortality effect was observed in the BTH region (with relative risk (RR) of 1.29; 95% confidence interval (CI): 1.13–1.47), followed by the YRD (RR = 1.25; 95% CI: 1.13–1.35) and the PRD (RR = 1.14; 95% CI: 1.01–1.28) areas. With 0–21 days’ lag, the cold effect was pronounced in all city clusters, with the highest extreme cold-related mortality risk found in the PRD area (RR = 2.27; 95% CI: 1.63–3.16), followed by the YRD area (RR = 1.85; 95% CI: 1.56–2.20) and BTH region (RR = 1.33; 95% CI: 0.96–1.83). People in the southern regions tended to be more vulnerable to cold stress, but the northern population was more sensitive to heat stress. By examining the effects of extreme temperature in city clusters of different regions, our findings underline the role of adaptation towards heat and cold, which has important implications for public health policy making and practice.

Highlights

  • According to the Fifth Report of the Intergovernmental Panel on Climate Change (IPCC), evidence of climate system warming is unequivocal, and the global mean surface temperatures in 2081–2100 will be up to 3.7 °C higher than those of 1986–2005 under the Representative Concentration Pathway (RCP) 8.5 scenario, with an uncertainty range from 2.6 to 4.8 °C (IPCC 2014)

  • With 0–3 days’ lag, the strongest heat-related mortality effect was observed in the BTH region (with relative risk (RR) of 1.29; 95% confidence interval (CI): 1.13–1.47), followed by the Yangtze River Delta (YRD) (RR = 1.25; 95% CI: 1.13–1.35) and the Pearl River Delta (PRD) (RR = 1.14; 95% CI: 1.01–1.28) areas

  • With 0–21 days’ lag, the cold effect was pronounced in all city clusters, with the highest extreme cold-related mortality risk found in the PRD area (RR = 2.27; 95% CI: 1.63–3.16), followed by the YRD area (RR = 1.85; 95% CI: 1.56–2.20) and BTH region (RR = 1.33; 95% CI: 0.96–1.83)

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Summary

Introduction

According to the Fifth Report of the Intergovernmental Panel on Climate Change (IPCC), evidence of climate system warming is unequivocal, and the global mean surface temperatures in 2081–2100 will be up to 3.7 °C higher than those of 1986–2005 under the Representative Concentration Pathway (RCP) 8.5 scenario, with an uncertainty range from 2.6 to 4.8 °C (IPCC 2014). There is increasing evidence that extreme climatic events are becoming more frequent, more intense, and longer-lasting (Guo et al 2013; Gao et al 2015). The IPCC report claims that in urban areas climate change is projected to increase risks for people, assets, economies, and ecosystems, including risks from heat stress. As the world is increasingly urbanized, the twentyfirst century agenda would have to focus on greatly reducing vulnerabilities of people and infrastructure in

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