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中欧长时间热浪对热应激和死亡率的影响——以 2019 年 6 月波兰为例。

Heat strain and mortality effects of prolonged central European heat wave-an example of June 2019 in Poland.

机构信息

Climate Impacts Laboratory, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Twarda 51/55, 00-818, Warszawa, Poland.

Faculty of Geography and Geology, Jagiellonian University in Cracow, Gronostajowa 7, 30-387, Kraków, Poland.

出版信息

Int J Biometeorol. 2022 Jan;66(1):149-161. doi: 10.1007/s00484-021-02202-0. Epub 2021 Oct 26.

Abstract

The occurrence of long-lasting severe heat stress, such as in July-August 2003, July 2010, or in April-May 2018 has been one of the biggest meteorological threats in Europe in recent years. The paper focuses on the biometeorological and mortality effects of the hot June that was observed in Central Europe in 2019. The basis of the study was hourly and daily Universal Thermal Climate Index (UTCI) values at meteorological stations in Poland for June 2019. The average monthly air temperature and UTCI values from 1951 to 2018 were analysed as background. Grosswetterlagen calendar of atmospheric circulation was used to assess synoptic conditions of heat wave. Several heat strain measures were applied : net heat storage (S), modelled heart rate (HR), sultriness (HSI), and UTCI index. Actual total mortality (TM) and modelled strong heat-related mortality (SHRM) were taken as indicators of biometeorological consequences of the hot June in 2019. The results indicate that prolonged persistence of unusually warm weather in June 2019 was determined by the synoptic conditions occurring over the European region and causing advection of tropical air. They led to the emergence of heat waves causing 10% increase in TM and 5 times bigger SHRM then in preceding 10 years. Such increase in SHRM was an effect of overheating and overload of circulatory system of human organism.

摘要

长时间严重的热应激的发生,如 2003 年 7 月至 8 月、2010 年 7 月或 2018 年 4 月至 5 月,是近年来欧洲最大的气象威胁之一。本文重点研究了 2019 年中欧观察到的炎热 6 月的生物气象学和死亡率影响。该研究的基础是波兰气象站每小时和每日的通用热气候指数(UTCI)值,用于 2019 年 6 月。分析了 1951 年至 2018 年的平均月气温和 UTCI 值作为背景。总天气状况日历的大气环流用于评估热浪的天气条件。应用了几种热应激指标:净热储存(S)、模拟心率(HR)、闷热指数(HSI)和 UTCI 指数。实际总死亡率(TM)和模拟强烈与热相关的死亡率(SHRM)被用作 2019 年炎热 6 月生物气象后果的指标。结果表明,2019 年 6 月异常温暖天气的长时间持续是由影响欧洲地区的天气条件决定的,这些条件导致热带空气的平流。它们引发了热浪,导致 TM 增加了 10%,而 SHRM 则比前 10 年增加了 5 倍。SHRM 的这种增加是人体循环系统过热和过载的结果。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87a9/8727406/581be5ed416d/484_2021_2202_Fig1_HTML.jpg

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