DOI QR코드

DOI QR Code

The Performance Assessment of Special Observation Program (ProbeX-2009) and the Analysis on the Characteristics of Precipitation at the Ulleungdo

울릉도 특별관측 수행평가 및 강수특성 분석

  • Kim, Ki-Hoon (Forecast Research Laboratory, National Institute of Meteorological Research, KMA) ;
  • Kim, Yeon-Hee (Forecast Research Laboratory, National Institute of Meteorological Research, KMA) ;
  • Kim, Do-Woo (Forecast Research Laboratory, National Institute of Meteorological Research, KMA) ;
  • Chang, Dong-Eon (Forecast Research Laboratory, National Institute of Meteorological Research, KMA)
  • 김기훈 (기상청 국립기상연구소 예보연구과) ;
  • 김연희 (기상청 국립기상연구소 예보연구과) ;
  • 김도우 (기상청 국립기상연구소 예보연구과) ;
  • 장동언 (기상청 국립기상연구소 예보연구과)
  • Received : 2010.11.30
  • Accepted : 2011.06.13
  • Published : 2011.06.30

Abstract

The performance assessment in radiosonde observation on the special observation program (ProbeX-2009) is performed and the characteristics of precipitation using Auto Weather System (AWS) and radiosonde data in 2009 at the Ulleungdo are investigated. The launching time, observation time, and maximum altitude of radiosonde are satisfied with the regulation from Korea Meteorological Administration (KMA) and World Meteorological Organization (WMO) but the duration of observational time of radiosonde is much shorter than that of the ProbeX-2007 because the altitude of launching site is higher than others in 2007. From the analysis of trajectories of radiosonde, most radiosondes at the Ulleungdo tend to move into the east because the westerly prevail at the middle latitude. However, when the Okhotsk high is expanded to the Korean peninsula and the north-westerly winds strengthen over the East Sea as the subtropical high is retreated, radiosonde tends to move into the south-west and south-east, respectively. Maximum distance appears at the end of observation level before May but the level of maximum distance is changed into 100 hPa after June because the prevailing wind direction is reversed from westerly to easterly at the stratosphere during summer time. The condition of precipitation was more correlated with the dynamic instability except Changma season. Precipitation in 2009 at the Ulleungdo occurred under the marine climate so that total precipitation amounts and precipitation intensity were increased and intensified during nighttime. The local environment favorable for the precipitation during nighttime was while the wind speed at the surface and the inflow from the shoreline were strengthened. Precipitation events also affected by synoptic condition but the localized effect induced by topography was more strengthened at the northern part of Ulleungdo.

Keywords

References

  1. 기상청, 2003: 고층기상관측지침. 기상청, 7-9.
  2. 김기훈, 김연희, 장동언, 2009: KEOP-2007 라디오존데 관측자료를 이용한 장마 특성 분석: Part I. 라디오존데 관측자료 평가 분석. 대기, 19, 213-226.
  3. 김희종, 윤일희, 권병혁, 2004: 울릉도에서의 구름 유입시 관측한 해양대기경계층의 열수지에 관한 사례연구. 한국지구과학회지, 25, 629-636.
  4. 안중배, 남재철, 서장원, 이해진, 2002: 해무 예측 모듈 개발과 울릉도 해무 사례 적용 연구. 한국기상학회지, 38, 155-164.
  5. 이승호, 최병철, 2001: 울릉도의 적설량 변화, 한국기상학회지, 37, 317-328.
  6. Ha, J., K.-D. Park, K. Kim, and Y.-H. Kim, 2010: Comparison of atmospheric water vapor profiles otained by GPS, MWR, and radiosonde. Asia-Pacific J. Atmos. Sci., 46, 233-241. https://doi.org/10.1007/s13143-010-1012-1
  7. WMO, 2006: WMO guide to meteorological instruments and methods of observation. WMO publication No.8, World Meteorological Organization.
  8. Wu P., M. D. Yamanaka, and J. Matsumoto, 2008: The formation of nocturnal rainfall offshore from convection over western Kalimantan Island. J. Meteor. Soc. Japan, 86, 187-203.
  9. Wu P., M. Hara, J.-I. Hamada, and M. D. Yamanaka, 2009: Why a large amount of rain falls over the sea in the vicinity of western Sumatra Island during nighttime. J. Appl. Meteor, 48, 1345-136. https://doi.org/10.1175/2009JAMC2052.1