• 제목/요약/키워드: 라만 라이다

검색결과 38건 처리시간 0.022초

라만-탄성 라이다를 이용한 황사 및 오염 에어러솔의 라이다 비 측정 연구 (Measurements of the Lidar Ratio for Asian Dust and Pollution Aerosols with a Combined Raman and Back-scatter Lidar)

  • 윤순창;이영지;김상우;김만해
    • 대기
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    • 제20권4호
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    • pp.483-494
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    • 2010
  • The vertical profiles of the extinction coefficient, the backscatter coefficient, and the lidar ratio (i.e., extinction-to-backscattering ratio) for Asian dust and pollution aerosols are determined from Raman (inelastic) and elastic backscatter signals. The values of lidar ratios during two polluted days is found between 52 and 82 sr (July 22, 2009) and 40~60 sr (July 31, 2009) at 52 nm, with relatively low value of particle depolarization ratio (<5%) and high value of sun photometer-derived Angstrom exponent (> 1.2). However, lidar ratios between 25 and 40 sr are found during two Asian dust periods (October 20, 2009 and March 15, 2010), with 10~20% of particle depolarization ratio and the relatively low value of sun photometer-derived Angstrom exponent (< 0.39). The lidar ratio, particle depolarization ratio and color ratio are useful optical parameter to distinguish non-spherical coarse dust and spherical fine pollution aerosols. The comparison of aerosol extinction profiles determined from inelastic-backscatter signals by the Raman method and from elastic-backscatter signals by using the Fernald method with constant value of lidar ratio (50 sr) have shown that reliable aerosol extinction coefficients cannot be determined from elastic-backscatter signals alone, because the lidar ratio varies with aerosol types. A combined Raman and elastic backscatter lidar system can provide reliable information about the aerosol extinction profile and the aerosol lidar ratio.

라만 라이다의 석영 채널을 이용한 고도별 황사 농도 산출 (A Retrieval of Vertically-Resolved Asian Dust Concentration from Quartz Channel Measurements of Raman Lidar)

  • 노영민;이권호;이한림
    • 한국대기환경학회지
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    • 제27권3호
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    • pp.326-336
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    • 2011
  • The Light Detection and Ranging (Lidar) observation provides a specific knowledge of the temporal and vertical distribution and the optical properties of the aerosols. Unlike typical Mie scattering Lidars, which can measure backscattering and depolarization, the Raman Lidar can measure the quartz signal at the ultra violet (360 nm) and the visible (546 nm) wavelengths. In this work, we developed a method for estimating mineral quartz concentration immersed in Asian dust using Raman scattering of quartz (silicon dioxide, silica). During the Asian dust period of March 15, 16, and 21 in 2010, Raman lidar measurements detected the presence of quartz, and successfully showed the vertical profile of the dust concentrations. The satellite observations such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) confirmed spatial distribution of Asian dust. This approach will be useful for characterizing the quartz dominated in the atmospheric aerosols and the investigations of mineral dust. It will be especially applicable for distinguishing the dust and non-dust aerosols in studies on the mixing state of Asian aerosols. Additionally, the presented method combined with satellite observations is enable qualitative and quantitative monitoring for Asian dust.

다파장 라만 라이다 시스템을 이용한 황사/비황사입자 구분 및 비황사입자의 미세물리적 특성 연구 (Classification of Dust/Non-dust Particle from the Asian Dust Plumes and Retrieval of Microphysical Properties using Raman Lidar System)

  • 신성균;신동호;이권호;노영민
    • 한국대기환경학회지
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    • 제28권6호
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    • pp.688-696
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    • 2012
  • The particle depolarization ratios were retrieved from the observation with a multi-wavelength Raman lidar at Gwangju, Korea ($35.11^{\circ}N$, $126.54^{\circ}E$). The measurements were carried out on 24 February and 9 March 2004. Using the particle depolarization ratios, the non-dust aerosol particles were distinguished from the Asian dust plume, and the proportion of the non-dust particle to total dust plume was retrieved. The calculated proportion of the non-dust particle was used for the retrieval of backscatter coefficients at 355, 532, and 1064 nm and extinction coefficients at 355 and 532 nm of non-dust particles in the dust plume. Microphysical parameters of non-dust particles including single-scattering albedo at 532 nm were retrieved using retrieved optical values. The retrieved single-scattering albedo of non-dust particles was 0.92~0.95 below 1 km height and 0.82~0.91 above 1 km height on 24 February 2004 and $0.81{\pm}0.03$ on 9 March 2004.

다파장 라만 라이다 시스템을 이용한 발원지 및 이동 경로에 따른 황사의 광학적 특성 변화 연구 (Study on the Variation of Optical Properties of Asian Dust Plumes according to their Transport Routes and Source Regions using Multi-wavelength Raman LIDAR System)

  • 신성균;노영민;이권호;신동호;김관철;김영준
    • 대한원격탐사학회지
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    • 제30권2호
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    • pp.241-249
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    • 2014
  • 본 연구에서는 광주과학기술원의 다파장 라만 라이다 시스템을 이용하여 2009년부터 2011년, 3년동안 광주에서 대기 에어로졸의 관측을 실시하였다. 관측된 라이다 신호의 분석으로부터 산출된 편광소멸도를 이용하여 황사의 층을 구분해 내었다. 구분 된 황사의 층의 고도에 따른 정보들은 Hybrid Single Particle Lagrangian Integrated Trajectory(HYSPLIT) 모델을 이용한 황사 층의 역궤적 분석에 이용되었고, 그 정보들을 통하여, 황사 층의 발원지 및 유입경로를 규명할 수 있었다. 한반도로 유입되는 황사는 고비사막을 기원으로 하는 경우가 가장 많은 것으로 나타났으며, 또한, 황사의 이동경로에 따른 광학적 특성 변화를 규명하기 위해, 중국 공업지역을 통과하여 유입된 황사 층과 발원지로부터 한반도로 직접적으로 유입된 황사의 구분하여 경로에 따른 입자 편광소멸도의 통계 분석을 실시하였다. 중국 공업지역을 통과하여 한반도로 유입된 황사의 편광소멸도는 0.07-0.1의 값을 보인 반면, 발원지로부터 공업지역을 경유하지 않고 직접 유입된 황사의 편광소멸도는 0.11-0.15로 상대적으로 높은 값을 보였다. 이는 발원지에서 발생한 순수 황사입자가 이동 중에 공업지역에서 발생한 오염입자와 혼합하여 황사층의 편광소멸도를 감소시킨 것으로 사료된다.

다파장 라만 라이다를 이용한 발생지에 따른 안면도 지역 에어러솔의 광학적 및 미세물리적 특성 (Investigation of Source Dependent Optical and Microphysical Characteristics of Aerosol Using Multi-wavelength Raman Lidar in Anmyun, Korea)

  • 노영민;이한림
    • 한국대기환경학회지
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    • 제26권5호
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    • pp.554-566
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    • 2010
  • We present optical and microphysical particle properties of aerosol retrieved by multi-wavelength Raman lidar at Anmyun island ($36.32^{\circ}N$, $126.19^{\circ}E$), Korea. The results present aerosol properties in various height layers of the atmospheric pollution layers observed over the Korean peninsula on eight consecutive days (27, 28, 29, 30 and 31 May, 4, 5 and 7 June) in 2005 at Anmyun island. We found anthropogenic pollution on 27, 28, and 29 May and local haze on other measurement days. The origin of the particle plumes was determined by simulations of FLEXPART. The source regions of the particles resulted in rather clear differences between the optical and microphysical properties of the pollution layers. The single-scattering albedo of anthropogenic aerosols from China ($0.91{\pm}0.01$ at 532 nm) were lower than the single-scattering albedo of local haze aerosols ($0.95{\pm}0.01$ at 532 nm). Local haze aerosols show larger effective radii of $0.24{\pm}0.02\;{\mu}m$ at relative humidity of 55~75%. The effective radii of anthropogenic aerosols are $0.20{\pm}0.2\;{\mu}m$ and $0.27\;{\mu}m$ at relative humidity of 25~50%.

역행렬 알고리즘을 이용한 다파장 라만 라이다 데이터의 고도별 에어로졸 Microphysical Parameter 도출 (Retrieval of Aerosol Microphysical Parameter by Inversion Algorithm using Multi-wavelength Raman Lidar Data)

  • 노영민;김영준
    • 한국대기환경학회지
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    • 제23권1호
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    • pp.97-109
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    • 2007
  • Vertical distribution and optical properties of atmospheric aerosols above the Korean peninsula are quite important to estimate effects of aerosol on atmospheric environment and regional radiative forcing. For the first time in Korea, vertical microphysical properties of atmospheric aerosol obtained by inversion algorithm were analyzed based on optical data of multi-wavelength Raman lidar system developed by the Advanced Environmental Monitoring Research Center (ADEMRC), Gwangju Institute Science and Technology (GIST). Data collected on 14 June 2004 at Gwangju ($35.10^{\circ}N,\;126.53^{\circ}E$) and 27 May 2005 at Anmyeon island ($36.32^{\circ}N,\;126.19^{\circ}E$) were used as raw optical data for inversion algorithm. Siberian forest fire smoke and local originated haze were observed above and within the height of PBL, respectively on 14 June 2004 according to NOAA/Hysplit backstrajectory analysis. The inversion of lidar optical data resulted in particle effective radii around $0.31{\sim}0.33{\mu}m$, single scattering albedo between $0.964{\sim}0.977$ at 532 nm in PBL and effective radii of $0.27{\mu}m$ and single scattering albedo between $0.923{\sim}0.924$ above PBL. In the case on 27 May 2005, biomass burning from east China was a main source of aerosol plume. The inversion results of the data on 27 May 2005 were found to be particle effective radii between $0.23{\sim}0.24{\mu}m$, single scattering albedo around $0.924{\sim}0.929$ at 532 nm. Additionally, the inversion values were well matched with those of Sun/sky radiometer in measurement period.

GIST/ADEMRC 다파장 라만 라이다 시스템을 이용한 안면도 지역에서의 라이다 비 연구 (Determination of the Lidar Ratio Using the GIST / ADEMRC Multi-wavelength Raman Lidar System at Anmyeon Island)

  • 노영민;김영민;김영준;최병철
    • 한국대기환경학회지
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    • 제22권1호
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    • pp.1-14
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    • 2006
  • Tropospheric aerosols are highly variant in time and space due to non-uniform source distribution and strong influence of meteorological conditions. Backscatter lidar measurement is useful to understand vertical distribution of aerosol. However, the backscatter lidar equation is undetermined due to its dependence on the two unknowns, extinction and backscattering coefficient. This dependence necessitates the exact value of the ratio between two parameters, that is, the lidar ratio. Also, Iidar ratio itself is useful optical parameter to understand properties of aerosols. Tropospheric aerosols were observed to understand variance of lidar ratio at Anmyeon island ($36.32^{/circ}N$, $126.19^{/circ}E$), Korea using a multi-wavelength raman lidar system developed by the Advanced Environmental Monitoring Research Center (ADEMRC), Gwangju Institute Science and Technology (GIST), Korea during measurement periods; March 15$\sim$April $16^{th}$, 2004 and May 24$\sim$ $8^{th}$ 2005. Extinction coefficient, backscattering coefficient, and lidar ratio were measured at 355 and 532 nm by the Raman method. Different types of aerosol layers were distinguished by the differences in the optical properties such as Angstrom exponent, and lidar ratio. The average value of lidar ratio during two observation periods was found to be $50.85\pm4.88$ sr at 355 nm and $52.43\pm15.15$ sr at 532 nm at 2004 and $57.94\pm10.29$ sr at 355 nm and $82.24\pm15.90$ sr at 532 nm at 2005. We conduct hysplit back-trajectory to know the pathway of airmass during the observation periods. We also calculate lidar ratio of different type of aerosol, urban, maritime, dust, continental aerosols using OPAC (Optical Properties of Aerosols and Clouds), Remote sensing of atmospheric aerosol using a multi-wavelengh lidar system with Raman channels is quite and powerful tool to characterize the optical propertises of troposheric aerosols.

가식성 코팅처리가 토종다래(Actinidia arguta) 동결건조 스낵의 흡습과 품질에 미치는 영향 (Effect of Edible Coating on Hygroscopicity and Quality Characteristics of Freeze-Dried Korean Traditional Actinidia (Actinidia arguta) Cultivars Snack)

  • 김아나;소슬아;박찬양;이교연;샤피어라만;최성길
    • 한국식품영양과학회지
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    • 제45권9호
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    • pp.1344-1350
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    • 2016
  • 본 연구는 수분 흡습으로 인해 건조 후 저장이 어려운 다래 동결건조 스낵의 저장성 및 상품성을 증가시키기 위해 다양한 가식성 코팅제를 처리한 스낵의 품질 특성과 흡습 저해효과를 분석하였다. 따라서 가식성 코팅처리제로는 albumin, dextrin, whole soy flour를 이용하였고, 5%의 농도로 코팅제를 증류수에 용해한 코팅액에 슬라이스를 침지하여 제조하였다. 스낵의 주요 품질 특성인 수분 함량, 수분활성도, 수율, 수분용해지수 및 수분흡착지수, 수화 복원성을 분석한 결과 모든 시료에서 가식성 코팅처리에 따른 유의적인 차이가 나타나지 않아 코팅처리는 다래 동결건조 스낵의 기본적인 품질 특성에 영향을 미치지 않는 것으로 나타났다. 가식성 코팅처리는 다래 동결건조 스낵의 흡습을 저해하는 것으로 나타났으며 dextrin으로 처리한 시료의 흡습 저해 효과가 가장 우수한 것으로 나타났다. 흡습 저해가 스낵의 이화학적 특성에 미치는 영향을 알아보기 위해 흡습 시간에 따른 경도와 총페놀 함량 및 항산화 활성을 측정하였다. 흡습 시간이 길어질수록 모든 시료의 경도가 감소하였고 코팅처리는 흡습으로 인한 경도의 감소를 저해하는 것을 확인하였으며, dextrin 처리가 가장 높은 경도를 가지는 것으로 나타났다. 또한, 스낵의 총페놀 함량 및 항산화 활성은 흡습시간이 경과함에 따라 감소하는 것으로 나타났으며, 가식성 코팅처리군의 총페놀 함량과 항산화 활성은 비처리군보다 비교적 높게 유지하였고, dextrin으로 코팅한 스낵이 가장 높은 총페놀 함량과 항산화 활성을 가지는 것으로 나타났다. 이상의 결과를 바탕으로 토종다래 동결건조 스낵의 흡습을 방지하고 품질을 보존하는 방법으로 가식성 코팅제인 dextrin으로 코팅하는 것이 가장 효과적일 것으로 생각되며, 가식성 코팅은 여러 가공식품의 상품성 및 저장성을 향상시킬 것으로 생각한다.