• Title/Summary/Keyword: 종관적 특성

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월성원전 부지의 가을철 방사성 물질의 대기확산인자 분포 특성

  • 이갑복;이명찬;송영일
    • Proceedings of the Korean Nuclear Society Conference
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    • 1998.05b
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    • pp.665-670
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    • 1998
  • 삼차원 해륙풍 모델과 라그랑지안 입자확산모델을 이용하여 해안지역에 위치한 원전으로부터 정상운전시 장기적으로 연속 방출되는 방사성 물질의 대기확산 평가방법론을 개발하였다. 개발된 방법론을 적용하여 월성원전 부지를 대상으로 풍향, 풍속 및 운량에 따라 범주화된 각 종관기상 상태에 대해 가을철 방사성 물질 대기확산 특성을 분석하였다. 분석 결과, 방사성 물질의 계절 또는 연중 핑균적인 대기확산인자의 분포는 종관바람 둥과 같은 주풍의 발생빈도에 영향을 받을 뿐만 아니라, 해륙풍 등과 같은 국지 대기순환의 특성에 따라서도 그 분포특성이 결정됨을 알 수 있었다.

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Synoptic Analysis of Heavy Rainstorms over Urban Areas in the Southern United States (미국 남부지방 도시호우의 종관적 분석)

  • Youngeun Choi
    • Journal of the Korean Geographical Society
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    • v.33 no.3
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    • pp.395-409
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    • 1998
  • The purpose of this paper is to determine the atmospheric conditions in whih urban areas affect the precipitation processes and to evaluate whether certain weather types show more apparent urban effect on precipitation modification over five cities in the southem United States. Each heavy rainstorm is classified into one of three synoptic weather types (frontal storm, airmass storm or tropical disturbance storm). Heavy rainstorm day is defined as day producing rainfall totals that equal o exceed 2 inches (50.08 mm). Houston, Dallass and San Antonio show possible urban effects on rainfall totals and frequencies of heavy rainstorms by airmass storm type while New Orleans and Memphis do not reveal any distinct precipitation enhancements through the synoptic analysis. The results of TSA (Trend Surface Analysis) show that frontal and tropical disturbance storm types have stronger climatic gradients than airmass types and the patterns of rainfall totals have stronger trends than those of rainfall frequencies for the five cities. The results suggest that airmass type events may well reveal possible precipitation enhancements due to urban effects since they are less influenced by a strong climate gradient and they provide favorable conditions for development of urban heat islands. Residual analysis confirms that rainfall totals and frequencies of heavy rainstorms by airmass storm type have positive residuals over the city or the major effect area.

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Difference of Synoptic Characteristics according to the Persistence of Rainfall in Korea during the Changma Season (장마철 우리나라 강수의 지속성에 따른 종관 특성의 차이)

  • Park, Byong-Ik
    • Journal of the Korean Geographical Society
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    • v.45 no.6
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    • pp.748-765
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    • 2010
  • This study aims to investigate the difference of synoptic characteristics over East Asia according to the persistence of rainfall in Korea during the Changma season (June and July). In the cases of consecutive rainfall which lasts four or more days, there are developed ridges in 850hPa level east of the Korean peninsula which introduce stagnation of the synoptic cyclone over Korea. An cold area in 850hPa level moves southward from the Northern China in one day before the beginning the rainfall day in Korea and it aids the development of the stationary front in East Asia. When rainfall lasts a day or two, cyclones pass over Korea in rainy day and the stationary front in East Asia is not intensified. In both cases the synoptic cyclones near the Korean peninsula shows a deep-baroclinic structure, while in the former cases over the southwestern part of Japan a subtropical frontal zone which has a shallow structure appears near Japan. In latter cases the frontal structures are same near Korea and Japan. So, this means that the Changma is not necessarily similar to the Baiu of Japan in all cases.

A Synoptic Climatological Study on the Distribution of Winter Precipitation in South Korea (韓國의 冬季 降水 分布에 關한 綜觀氣候學的 硏究)

  • Park, Byong-Ik;Yoon, Suk-Eun
    • Journal of the Korean Geographical Society
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    • v.32 no.1
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    • pp.31-46
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    • 1997
  • The purposes of this paper are to classify the spatial distribution types of precipitation by making daily isohyetal maps based on the winter daily precipitation and to analyse both the distributional characteristics of precipitation during the winter in South Korea and the synoptic characteristics related to them. Also, the correspondence between the spatial distribution types of precipitation and the synoptic characteristics occuring among them is examined with regards to pressure patterns and then precipitation distribution types. In addition, the characteristics of the pressure fields and temperature fields in 850hPa, 700hPa, and 500hPa level were analysed to find out the difference between the Ullung-do type and the Ullung-do${\cdot}$Honam type, which have similar characteristics on the surface weather map. As a result, the Ullung-do area showed a high frequency of occurrence regardless of precipitation classes, the East Coast area revealed a higher frequency of occurrence in over the 5mm section, while the Honam area had high frequency of occurrence in the 1~5mm section. There are twelve distribution types of precipitation during the winter. These distribution types show clear changes according to the season. The difference in precipitation distribution between the Ullung-do type and the Ullung-do${\cdot}$Honam type has a close relationship with the aspect of the upper cold air advection rather than the direction and the speed of the wind.

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