Abstract

We investigated the spatial characteristics of heat extremes in South Korea from the climatological mean perspective. A heat extreme was defined as a day when the daily maximum temperature was higher than 33 °C. According to our analyses, the eastern area of the Sobaek and Taebaek mountain ranges (hereafter called the eastern district) is significantly more exposed to heat extremes compared to other areas. The onset date and total number of days of annual heat extremes in the eastern district are approximately 13 days earlier and 3 days higher than those in the western district on average, respectively. Likewise, the annual mean of daily maximum temperatures during heat extreme days are approximately 0.25 °C higher. This larger exposure to heat extremes in the eastern district appears to be attributable to the Föhn phenomenon, which is likely induced by the dominant southwesterly monsoon during the early-to-peak summer. In contrast, differences in the ending dates of annual heat extremes are not noticeable between the eastern and western districts, when the southerly winds are dominant. Our analyses suggest that heat extremes in South Korea cannot be understood by a simple function of latitude, but in conjunction with atmospheric physical processes.

Highlights

  • Heat extremes bring extremely hot air into midlatitude and subtropical regions

  • To confirm whether heat extremes are more severe in the southern region of South Korea or not, the regression coefficients between latitudes and four climatological heat-related indicators of weather stations were calculated (Table 1)

  • Our results suggest that heat extremes in South Korea do not have a strong dependency on latitude, which differs from the common assumption of people

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Summary

Introduction

Heat extremes bring extremely hot air into midlatitude and subtropical regions. Because of the vulnerability of living things to extreme weather conditions corresponding to climate change, heat extremes have inflicted an immense amount of suffering on human societies, resulting in several deaths worldwide [1]. It is important to examine and assess the characteristics of heat extremes, especially in relation to global warming. In 2003, the heat extremes that swept across Europe resulted in approximately 35,000 deaths [2,3]. Especially Russia, experienced an extremely hot summer accompanied by strong heat extremes in 2010 [4]. Heat extremes have tended to increase in their intensity and frequency [9,10]

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