Observation on Structural Change of Low Level Atmosphere due to Effect of Sea Breeze

해풍 효과에 의한 저층대기구조 변화의 측정

  • 전병일 (부산대학교 대기과학과) ;
  • 김유근 (부산대학교 대기과학과, 부산대학교 지구과학교육과)
  • Published : 1996.08.01

Abstract

The surface meteorological and upper layer meteorological observation carried out to investigate influences of sea breeze effect on lower layer atmosphere at Gori nuclear power plant for 29∼30 July, 1996. According to surface meteorological data, the inflow of sea breeze was occurred 11:30 on 29 July, 10:30-on 30 July, respectively, at observation site. And the meteorological tower data showed that wind direction of sea breeze was identified as south-westerly, and wind speed of 58 m was 2 times stronger than that of 10 m. It is notworthy that surface inversion layer which built from the night time to daybreak of next day was not broken off by seab reeze's inflow for daytime, and strong inversion layer observed at 47∼243 m with moderately stable class (F) by URC. It was found that strong stable layer of potential temperature appeared at that layer, maximum relative humidity observed at the bottom of inversion layer and maximum mixing ratio observed in the low of inversion layer.

Keywords

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