Abstract

The aim of the study was to establish to what extent extreme thermal conditions have changed and how they affected mortality, and what conditions favor lower mortality rates or conversely, higher mortality rates. Heat/cold exposure was measured with the Universal Thermal Climate Index (UTCI). Daily mortality and meteorological data for 8 large Polish cities (Białystok, Gdańsk, Kraków, Lublin, Łódź, Poznań, Warszawa, and Wrocław) in the period 1975–2014 were analyzed. Generalized additive models were used to investigate the relationship between UTCI and mortality, and TBATS models were used for the evaluation of time series UTCI data. Most of the cities experienced a clear and statistically significant at p ≤ 0.05 decrease in cold stress days of 0.8–3.3 days/year and an increase in the frequency of thermal heat stress days of 0.3–0.6 days/year until 1992–1994. There was a clear difference as regards the dependence of mortality on UTCI between cities located in the “cooler” eastern part of Poland and the “warmer” central and western parts. “Cool” cities were characterized by a clear thermal optimum, approx. in the range of 5–30 °C UTCI, changing slightly depending on cause of death, age, or sex. For UTCI over 32 °C, in most of the cities except Gdańsk and Lublin, the relative risk of death (RR) rose by 10 to 20%; for UTCI over 38 °C, RR rose to 25–30% in central Poland. An increase in mortality on cold stress days was noted mainly in the “cool” cities: RR of total mortality increased even by 9–19% under extreme cold stress.

Highlights

  • The atmospheric environment affects human beings constantly in a limited but clear way

  • This study has shown a significant decrease in the frequency of cold stress days over the whole 1975–2014 period, and a high increase in strong heat stress days until 1994 and a steady rise or stabilization afterwards

  • Cold stress days observed decreased from ca. 55 in 1975 to 38 in 2014, and the number of heat stress days grew from 3 to 7 in the same years

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Summary

Introduction

The atmospheric environment affects human beings constantly in a limited but clear way. As climate change has started manifesting itself, e.g., in the rise of air temperature and the frequency and intensity of heat periods (IPCC 2014, 2018), interest in analyses of mortality as dependent on thermal conditions has increased. This interest grew stronger after the record warm August of 2003: in this heat wave, approximately. These factors become the main risk factor, leading indirectly and sometimes directly to death, which is widely described in many books and papers (Tromp 1980; Guyton and Hall 2006; Cheshire 2016)

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