Abstract

The objective of the paper was to characterize the occurrence of cold days and cold waves in Poznań in the years 1966/67–2015/16, as well as to characterize thermal conditions in the city during selected cold waves in the years 2008/09–2015/16. The study was based on daily data on maximum and minimum air temperature for station Poznań-Ławica from the years 1966/67–2015/16 and daily air temperature values from eight measurement points located in the territory of the city in different types of land use from the years 2008/08–2015/16. In addition, to characterize thermal conditions during selected days forming cold waves, satellite images were used, on the basis of which the land surface temperature (LST) was calculated. A cold day was defined as a day with daily maximum temperature (Tmax) below the value of 5th annual percentile of Tmax, and a cold wave was defined as at least five consecutive cold days. The study showed an increase in Tmax in winter, which translated to a decrease in the number of cold days over the last 50 years, although the changes were not statistically significant. Thermal conditions in the city showed high variability in the winter season and during the analyzed cold waves.

Highlights

  • The currently observed climate warming is unquestionable and evident among others through an increase in mean global air temperature [1]

  • Current research conducted in Poland points to a decrease in the number of cold days [2,3,4], more evident changes are observed in the case of frequency of occurrence of days with strong frosts [5,6]

  • An increase in The first set covered daily maximum (Tmax) at a level of 0.36 ◦ C was recorded in the analyzed years, the changes were not statistically significant

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Summary

Introduction

The currently observed climate warming is unquestionable and evident among others through an increase in mean global air temperature [1]. Current research conducted in Poland points to a decrease in the number of cold days [2,3,4], more evident changes are observed in the case of frequency of occurrence of days with strong frosts [5,6]. Due to a small contribution of natural plant surfaces, numerous vertical surfaces, as well as human activity, substantial amounts of heat are accumulated within the city during the day. They are released to the atmosphere causing their slower cooling than in the surrounding areas [10]. Air temperature in the city is usually higher than in suburban areas

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