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Long-term Changes in Wintertime Precipitation and Snowfall over Gangwon Province

강원 지역의 장기 겨울철 강수 및 강설 변화의 경향 분석

  • Baek, Hee-Jeong (Numerical Modeling Center, Korea Meteorological Administration) ;
  • Ahn, Kwangdeuk (Numerical Modeling Center, Korea Meteorological Administration) ;
  • Joo, Sangwon (Numerical Modeling Center, Korea Meteorological Administration) ;
  • Kim, Yoonjae (Numerical Modeling Center, Korea Meteorological Administration)
  • 백희정 (기상청 수치모델링센터) ;
  • 안광득 (기상청 수치모델링센터) ;
  • 주상원 (기상청 수치모델링센터) ;
  • 김윤재 (기상청 수치모델링센터)
  • Received : 2016.07.07
  • Accepted : 2017.06.01
  • Published : 2017.06.30

Abstract

The effects of recent climate change on hydrological systems could affect the Winter Olympic Games (WOG) because the event is dependent on suitable snow and ice conditions to support elite-level competitions. We investigate the long-term variability and change in winter total precipitation (P), snowfall water equivalent (SFE), and ratios of SFE to P during the period 1973/74~2015/16 in Gangwon province. The climatological percentages of SFE relative to winter total precipitation were 71%, 28%, and 44% in Daegwallyeong, Chuncheon, and Gangneung, respectively. The winter total P, SFE, and SFE/P has decreased (but not significantly), although significant increases of winter maximum and minimum temperature were detected at a 95% confidence level. Notably, a significant negative trend of SFE/P at Daegwallyeong in February, the month of the WOG, was attributable to a larger decrease in SFE related to the increases in maximum and minimum temperature. Winter wet-day minimum temperatures were warmer than climatological minimum temperatures averaged over the study period. The 20-year return values of daily maximum P and SFE decreased in Yongdong area. Since the SFE/P decrease with increasing temperature, the probability of rainfall rather than snowfall can increase if global warming continues.

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