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热浪对死亡率的影响。

The impact of heat waves on mortality.

机构信息

Department of Social and Environmental Health Research, London School of Hygiene and Tropical Medicine, London, United Kingdom.

出版信息

Epidemiology. 2011 Jan;22(1):68-73. doi: 10.1097/EDE.0b013e3181fdcd99.

DOI:10.1097/EDE.0b013e3181fdcd99
PMID:21150355
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3324776/
Abstract

BACKGROUND

Heat waves have been linked with an increase in mortality, but the associated risk has been only partly characterized.

METHODS

We examined this association by decomposing the risk for temperature into a "main effect" due to independent effects of daily high temperatures, and an "added" effect due to sustained duration of heat during waves, using data from 108 communities in the United States during 1987-2000. We adopted different definitions of heat-wave days on the basis of combinations of temperature thresholds and days of duration. The main effect was estimated through distributed lag nonlinear functions of temperature, which account for nonlinear delayed effects and short-time harvesting. We defined the main effect as the relative risk between the median city-specific temperature during heat-wave days and the 75th percentile of the year-round distribution. The added effect was defined first using a simple indicator, and then a function of consecutive heat-wave days. City-specific main and added effects were pooled through univariate and multivariate meta-analytic techniques.

RESULTS

The added wave effect was small (0.2%-2.8% excess relative risk, depending on wave definition) compared with the main effect (4.9%-8.0%), and was apparent only after 4 consecutive heat-wave days.

CONCLUSIONS

Most of the excess risk with heat waves in the United States can be simply summarized as the independent effects of individual days' temperatures. A smaller added effect arises in heat waves lasting more than 4 days.

摘要

背景

热浪与死亡率的上升有关,但相关风险仅部分得到描述。

方法

我们通过将温度风险分解为由于每日高温的独立影响的“主要效应”,以及由于热浪期间持续时间延长的“附加效应”,在美国 1987-2000 年的 108 个社区中使用数据来研究这种关联。我们根据温度阈值和持续天数的组合,采用不同的热浪日定义。主要效应通过温度的分布式滞后非线性函数来估计,这些函数考虑了非线性延迟效应和短期收获。我们将主要效应定义为热浪日期间中值城市特定温度与全年分布的第 75 百分位数之间的相对风险。附加效应首先使用简单指标定义,然后使用连续热浪日的函数定义。通过单变量和多变量荟萃分析技术汇总特定城市的主要和附加效应。

结果

与主要效应(4.9%-8.0%)相比,附加波效应较小(取决于波定义,超额相对风险为 0.2%-2.8%),仅在连续 4 天热浪后才明显。

结论

美国热浪的大部分超额风险可以简单地概括为个别日子温度的独立影响。在持续超过 4 天的热浪中,会产生较小的附加效应。

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