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2014년 대설관측실험(Experiment on Snow Storms At Yeongdong: ESSAY)기간 강설 및 눈결정 특성분석

Study on Characteristics of Snowfall and Snow Crystal Habits in the ESSAY (Experiment on Snow Storms At Yeongdong) Campaign in 2014

  • 서원석 (강릉원주대학교 대기환경과학과) ;
  • 은승희 (강릉원주대학교 대기환경과학과) ;
  • 김병곤 (강릉원주대학교 대기환경과학과) ;
  • 고아름 (강릉원주대학교 대기환경과학과) ;
  • 성대경 (강릉원주대학교 대기환경과학과) ;
  • 이규민 (강릉원주대학교 대기환경과학과) ;
  • 전혜림 (강릉원주대학교 대기환경과학과) ;
  • 한상옥 (국립기상과학원 관측예보연구과) ;
  • 박영산 (응용기상연구과)
  • Seo, Won-Seok (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Eun, Seung-Hee (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Kim, Byung-Gon (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Ko, A-Reum (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Seong, Dae-Kyeong (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Lee, Gyu-Min (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Jeon, Hye-Rim (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Han, Sang-Ok (Department of Observation and Forecast Research) ;
  • Park, Young-San (Department of Applied Meteorology Research, National Institute of Meteorological Research)
  • 투고 : 2015.02.17
  • 심사 : 2015.03.11
  • 발행 : 2015.06.30

초록

Characteristics of snowfall and snow crystal habits have been investigated in the campaign of Experiment on Snow Storms At Yeongdong (ESSAY) using radiosonde soundings, Global Navigation Satellite System (GNSS), and a digital camera with a magnifier for taking a photograph of snowfall crystals. The analysis period is 6 to 14 February 2014, when the accumulated snowfall amount is 192.8 cm with the longest snowfall duration of 9 days. The synoptic situations are similar to those of the previous studies such as the Low pressure system passing by the far South of the Korean peninsula along with the Siberian High extending to northern Japan, which eventually results in the northeasterly or easterly flows and the long-lasting snowfall episodes in the Yeongdong region. In general, the ice clouds tended to exist below around 2~3 km with the consistent easterly flows, and the winds shifted to northerly~northwesterly above the clouds layer. The snow crystal habits observed in the ESSAY campaign were mainly dendrite, consisting of 70% of the entire habits. The rimed habits were frequently captured when two-layered clouds were observed, probably through the process of freezing of super-cooled droplets on the ice particles. The homogeneous habit such as dendrite was shown in case of shallow clouds with its thickness of below 500 m whereas various habits were captured such as dendrites, rimed dendrites, aggregates of dendrites, plates, rimed plates, etc in the thick cloud with its thickness greater than 1.5 km. The dendrites appeared to be dominant in the condition of cloud top temperature specifically ranging $-12{\sim}-16^{\circ}C$. However, the association of snow crystal habits with temperature and super-saturation in the cloud could not be examined in the current study. Better understandings of characteristics of snow crystal habits would contribute to preventing breakdown accidents such as a greenhouse destruction and collapse of a temporary building due to heavy snowfall, and traffic accidents due to snow-slippery road condition, providing a higher-level weather information of snow quality for skiers participating in the winter sports, and estimating more accurate snowfall amount, location, and duration with the fallspeed of solid precipitation.

키워드

참고문헌

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피인용 문헌

  1. Intercomparison between Temperature and Humidity Sensors of Radiosonde by Different Manufacturers in the ESSAY (Experiment on Snow Storms At Yeongdong) Campaign vol.26, pp.2, 2016, https://doi.org/10.14191/Atmos.2016.26.2.347
  2. Observation and Numerical Simulation of Cold Clouds and Snow Particles in the Yeongdong Region vol.54, pp.3, 2018, https://doi.org/10.1007/s13143-018-0055-6