英文摘要: | It is widely assumed by policymakers and health professionals that the harmful health impacts of anthropogenic climate change1, 2, 3 will be partially offset by a decline in excess winter deaths (EWDs) in temperate countries, as winters warm4, 5, 6. Recent UK government reports state that winter warming will decrease EWDs7, 8. Over the past few decades, however, the UK and other temperate countries have simultaneously experienced better housing, improved health care, higher incomes and greater awareness of the risks of cold. The link between winter temperatures and EWDs may therefore no longer be as strong as before. Here we report on the key drivers that underlie year-to-year variations in EWDs. We found that the association of year-to-year variation in EWDs with the number of cold days in winter ( <5 °C), evident until the mid 1970s, has disappeared, leaving only the incidence of influenza-like illnesses to explain any of the year-to-year variation in EWDs in the past decade. Although EWDs evidently do exist, winter cold severity no longer predicts the numbers affected. We conclude that no evidence exists that EWDs in England and Wales will fall if winters warm with climate change. These findings have important implications for climate change health adaptation policies.
Seasonal variation in death rates in temperate countries has long been recognized. EWDs in the UK are defined as the number of deaths from December to March minus the average number of deaths in the preceding August to November, and the following April to July9. Despite fewer cases in northern than southern Europe10, EWDs are causally attributed to seasonal variations in temperature, with low temperatures thought to cause death directly (for example, through hypothermia or falls in icy conditions) and by altering vulnerability to communicable or non-communicable diseases, such as influenza and myocardial infarction, which are more common in winter11. We collated data from the past 60 years to identify key factors associated with the decreasing trend in EWDs in England and Wales, and its year-to-year variation. We deliberately considered a very broad set of factors to minimize the risk of erroneous conclusions. To clarify the thrust of this paper, we are interested in explaining the year-to-year variation in EWDs not the daily variation, and we are not saying that temperature does not play a role, if it did not there would be no EWDs. What we aim to demonstrate is that how harsh a winter is no longer predicts how many EWDs there will be. Fig. 1 presents relative EWDs and variables identified as possible mediating or causal factors. Between 1951 and 2011, both absolute and year-to-year variation in EWDs declined over time. Three distinct periods in EWD changes were apparent (Supplementary Fig. 1): 1951–1970, where EWDs exhibited very high year-to-year variation and a strongly decreasing overall trend; 1971–2000, where year-to-year variation EWDs halved compared with the preceding period and the decreasing trend continued, albeit less strongly; and 2001–2011, where year-to-year variation was very small and the EWD rate was flat.
| http://www.nature.com/nclimate/journal/v4/n3/full/nclimate2121.html
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