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    이어도 해양종합과학기지에서의 3차원 바람성분에 따른 에어로솔 수 농도 변동 특성

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    https://www.riss.kr/link?id=A60109265

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    다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

    To investigate variation of aerosol number concentration at each different size with three-dimensional (3D) wind components in ocean area, aerosol particles and 3D wind components were measured in the Ieodo Ocean Research Station, which is located to 419 km southwest from Marado, the southernmost island of Korea, from 25 June to & July 2010. The Laser Particle Counter (LPC) and ultrasonic anemometer were used to measure the size of aerosol particles and 3D wind components (zonal (u), meridional (v)), and vertical (w) wind) respectively. Surface weather chart, NCEP/NCAR reanalysis data and sounding data were used to analyze the synoptic condition. The distribution of aerosol number concentration had a large variation from bigger particles more than 1.0μm in diameter by wind direction during precipitation. In the number concentration of aerosol particles with respect to the weather conditions, particles larger than 1.0μm in size were decreased and sustained to the similar concentration at smaller particles during precipitation. The increase in aerosol number concentration was due to the sea-salt particles which was suspended by southwesterly and upward winds. In addition, the aerosol number concentration with vertical wind flow colud be related with the occurrence and increasing mechanism of aerosol in marine boundary layer.
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    To investigate variation of aerosol number concentration at each different size with three-dimensional (3D) wind components in ocean area, aerosol particles and 3D wind components were measured in the Ieodo Ocean Research Station, which is located to ...

    To investigate variation of aerosol number concentration at each different size with three-dimensional (3D) wind components in ocean area, aerosol particles and 3D wind components were measured in the Ieodo Ocean Research Station, which is located to 419 km southwest from Marado, the southernmost island of Korea, from 25 June to & July 2010. The Laser Particle Counter (LPC) and ultrasonic anemometer were used to measure the size of aerosol particles and 3D wind components (zonal (u), meridional (v)), and vertical (w) wind) respectively. Surface weather chart, NCEP/NCAR reanalysis data and sounding data were used to analyze the synoptic condition. The distribution of aerosol number concentration had a large variation from bigger particles more than 1.0μm in diameter by wind direction during precipitation. In the number concentration of aerosol particles with respect to the weather conditions, particles larger than 1.0μm in size were decreased and sustained to the similar concentration at smaller particles during precipitation. The increase in aerosol number concentration was due to the sea-salt particles which was suspended by southwesterly and upward winds. In addition, the aerosol number concentration with vertical wind flow colud be related with the occurrence and increasing mechanism of aerosol in marine boundary layer.

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    참고문헌 (Reference)

    1 김지영, "한반도에서 측정된 에어러솔의 크기 분포와 지역별 특성" 한국기상학회 38 (38): 95-104, 2002

    2 박성화, "이어도 해양종합과학기지에서의 에어로솔 수 농도 변동" 한국환경과학회 18 (18): 721-733, 2009

    3 강미영, "내륙지역 강설시 레이더 바람장을 이용한 에어러솔 농도 변동" 부경대학교 대학원 2003

    4 김종환, "남해, 황해 상에서의 미세 에어러솔 크기별 수농도 분포 관측" 5 : 203-205, 2005

    5 이동인, "남서해안지역 강설시 바람장 변화에 따른 에어로솔 수 농도 변동" 한국환경과학회 17 (17): 699-709, 2008

    6 Arao, K., "Volume and mass of yellow sand dust in the air over Japan as estimated from atmospheric turbidity" 64 : 79-94, 1986

    7 Shimizu, S, "The relationship between distribution of humidity and types of rainfall on three rainbands near Shanghai during Meiyu period in 2001" 13-18, 2001

    8 Neiman, P. J, "Retrieving horizontal temperature gradients and advection from single-station wind-profiler observations" 4 : 22-233, 1989

    9 Kikuchi, K., "Relationship between aerosol number concentrations and convergence fields in winter monsoon seasons" 108 (108): 4115-, 2003

    10 Carlson, T. N., "Radiative characteristics of Saharan dust at solar wavelengths" 82 : 3141-3152, 1997

    1 김지영, "한반도에서 측정된 에어러솔의 크기 분포와 지역별 특성" 한국기상학회 38 (38): 95-104, 2002

    2 박성화, "이어도 해양종합과학기지에서의 에어로솔 수 농도 변동" 한국환경과학회 18 (18): 721-733, 2009

    3 강미영, "내륙지역 강설시 레이더 바람장을 이용한 에어러솔 농도 변동" 부경대학교 대학원 2003

    4 김종환, "남해, 황해 상에서의 미세 에어러솔 크기별 수농도 분포 관측" 5 : 203-205, 2005

    5 이동인, "남서해안지역 강설시 바람장 변화에 따른 에어로솔 수 농도 변동" 한국환경과학회 17 (17): 699-709, 2008

    6 Arao, K., "Volume and mass of yellow sand dust in the air over Japan as estimated from atmospheric turbidity" 64 : 79-94, 1986

    7 Shimizu, S, "The relationship between distribution of humidity and types of rainfall on three rainbands near Shanghai during Meiyu period in 2001" 13-18, 2001

    8 Neiman, P. J, "Retrieving horizontal temperature gradients and advection from single-station wind-profiler observations" 4 : 22-233, 1989

    9 Kikuchi, K., "Relationship between aerosol number concentrations and convergence fields in winter monsoon seasons" 108 (108): 4115-, 2003

    10 Carlson, T. N., "Radiative characteristics of Saharan dust at solar wavelengths" 82 : 3141-3152, 1997

    11 Penner, J. E, "Quantifying and minimizing uncertainty of climate forcing by anthropogenic aerosols" 75 (75): 375-400, 1994

    12 Alpert, P., "Quantification of dust-forced heating of the lower troposphere" 395 : 367-370, 1998

    13 Smirnov, A., "Optical properties of Saharan dust during ACE-2" 103 (103): 28079-28092, 1998

    14 Lee, D. I., "On the atmospheric aerosol particles in the relation to wind systems" 27 : 333-352, 1991

    15 Pruppacher, H. R, "Microphysics of clouds and precipitation" D. Reidel Publishing Company 202-218, 1978

    16 Peng, L., "Marine aerosol size distributions in the springtime over China adjacent seas" 41 : 6784-6796, 2007

    17 Duce, R. A, "Long-range atmospheric transport of soil dust from Asia to the tropical North Pacific: Temporal variability" 209 : 1522-1524, 1980

    18 Khemani, L. T., "Influence of atmospheric pollutants on cloud microphysics and rainfall" 41 : 367-380, 1987

    19 Dutton, E. G, "Features and effect of aerosol optical depth observed at Mauna Loa, Hawaii: 1982-1992" 99 (99): 8295-8306, 1994

    20 Nemesure, S., "Direct shortwave forcing of climate by the anthropogenic sulfate aerosol: Sensitivity to particle size, composition, and relative humidity" 100 : 26105-26116, 1995

    21 IPCC, "Climate Change 1995: In the science of climate change" Cambridge Univ. Press 572-, 1995

    22 Seinfeld, J. H., "Atmospheric chemistry and physics-from air pollution to climate change" John Wiley & Sons, Inc 132-, 1998

    23 Wark, K., "Air pollution: its origin control" Harper and Row Pub. 153-, 1976

    24 Willeke, K, "Aerosol measurement principles: Techniques and Applications" Van Nostrand Reinhold 876-, 1993

    25 Ogren, J. A., "A systematic approach to in situ observations of aerosol properties, In Aerosol Forcing of Climate" Wiley 215-226, 1995

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    학술지 이력

    학술지 이력
    연월일 이력구분 이력상세 등재구분
    2026 평가 재인증평가 신청대상 (재인증)
    2020-01-01 등재 등재학술지 유지 (재인증) KCI등재
    2017-01-01 등재 등재학술지 유지 (계속평가) KCI등재
    2013-01-01 등재 등재 1차 FAIL (등재유지) KCI등재
    2010-01-01 등재 등재학술지 선정 (등재후보2차) KCI등재
    2009-01-01 등재 등재후보 1차 PASS (등재후보1차) KCI등재후보
    2008-01-01 등재 등재후보 1차 FAIL (등재후보1차) KCI등재후보
    2006-01-01 등재 등재후보학술지 선정 (신규평가) KCI등재후보
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    학술지 인용정보

    학술지 인용정보
    기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
    2016 0.64 0.64 0.57
    KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
    0.55 0.55 0.864 0.1
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