• 제목/요약/키워드: Aerosol properties

검색결과 235건 처리시간 0.027초

Aerosol radiative forcing estimated from ground-based sky radiation measurements over East Asia

  • Kim, Do-Hyeong;Sohn, B.J.;Nakajima, T.;Okada, I.;Takamura, T.
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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    • pp.12-16
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    • 2002
  • The clear sky radiative forcings of aerosols were evaluated over East Asia. We first investigated optical characteristics of aerosol using sky radiation measurements. An algorithm of Nakajima et al. (1996) is used for retrieving aerosol parameters such as optical thickness, ${\AA}$ngstr$\"{O}$m exponent, single scattering albedo, and size distribution from sky-radiation measurements, which then can be used for examining spatial and temporal variations of aerosol. Obtaining aerosol radiative forcing at TOA and surface, a radiative transfer model is used with inputs of obtained aerosol parameters and GMS-5 satellite-based cloud optical properties. Results show that there is a good agreement of simulated downwelling radiative flux at the surface with observation within 10 W m$^{-2}$ rms errors under the clear sky condition. However, a relatively large difference up to 40 W m$^{-2}$ rms error is found under the cloudy sky condition. The computed aerosol radiative forcing at the surface shows downward flux changes ranging from -100 to -170 W m$^{-2}$ per unit aerosol optical thickness at 0.7 $\mu$m. The different values of aerosol radiative forcing among the stations is mainly due to the differences in single scattering albedo ($\omega$$_{0.7}$) and asymmetric parameter (g$_1$) related to the geographical and seasonal variations.

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수동형-능동형 위성센서 관측자료를 이용한 대기 에어러솔의 3차원 분포 및 복사강제 효과 산정 (Aerosol Direct Radiative Forcing by Three Dimensional Observations from Passive- and Active- Satellite Sensors)

  • 이권호
    • 한국대기환경학회지
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    • 제28권2호
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    • pp.159-171
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    • 2012
  • Aerosol direct radiative forcing (ADRF) retrieval method was developed by combining data from passive and active satellite sensors. Aerosol optical thickness (AOT) retrieved form the Moderate Resolution Imaging Spectroradiometer (MODIS) as a passive visible sensor and aerosol vertical profile from to the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) as an active laser sensor were investigated an application possibility. Especially, space-born Light Detection and Ranging (Lidar) observation provides a specific knowledge of the optical properties of atmospheric aerosols with spatial, temporal, vertical, and spectral resolutions. On the basis of extensive radiative transfer modeling, it is demonstrated that the use of the aerosol vertical profiles is sensitive to the estimation of ADRF. Throughout the investigation of relationship between aerosol height and ADRF, mean change rates of ADRF per increasing of 1 km aerosol height are smaller at surface than top-of-atmosphere (TOA). As a case study, satellite data for the Asian dust day of March 31, 2007 were used to estimate ADRF. Resulting ADRF values were compared with those retrieved independently from MODIS only data. The absolute difference values are 1.27% at surface level and 4.73% at top of atmosphere (TOA).

Annealing Temperature Dependence of Magnetic and Optic Properties of Bi:YIG Films Deposited with Aerosol Deposition Method

  • Shin, Kwang-Ho;Mizoguchi, Masahiko;Inoue, Mitsuteru
    • Journal of Magnetics
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    • 제12권3호
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    • pp.129-132
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    • 2007
  • Bismuth-substituted yttrium iron garnet (Bi:YIG, $Bi_{0.5}Y_{2.5}Fe_5O_{12}$) films were deposited with aerosol deposition method and their magnetic and optical properties were investigated as a function of annealing temperature. Since the ceramic films deposited with aerosol deposition method have not a perfect crystal structure due to non-uniform internal stress occurred by mechanical collision during their deposition, the post annealing could be a key process to release its internal stress and to improve its micro structure for optimizing the magnetic and magneto-optic properties of films. The crystallinity of Bi: YIG film was improved with increase of annealing temperature, and the saturation magnetization increased up to 87 emu/cc at $800^{\circ}C$. The Faraday rotation increased up to $1.4deg/{\mu}m$ by annealing at $700^{\circ}C$ around the wavelength of $0.5{\mu}m$. The optical transmittance of the Bi:YIG film was also improved in visible region.

The Influence of Aerosol Source Region on Size-resolved Hygroscopicity During the Asian Pacific Regional Aerosol Characterization Experiment (ACE-Asia) Campaign

  • Lee, Yong-Seob
    • Journal of Korean Society for Atmospheric Environment
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    • 제22권E1호
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    • pp.9-18
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    • 2006
  • Aerosol hygroscopic properties were measured by a tandem differential mobility analyzer (TDMA) system during the Aerosol Characterization Experiment (ACE)-Asia campaign from 31 March to 1 May 2001. Two high flow differential mobility analyzers (DMAs) were used to maximize the count rate on board the Center for Interdisciplinary Remotely Piloted Aircraft (CIRPAS) Twin Otter aircraft. Hygroscopic growth factor distributions of particles having initial dry nanoparticle diameters of 0.040, 0.059, 0.086, 0.126, 0.186, 0.273, 0.400, and $0.586{\mu}m$ were measured during 19 research flights. Data collected during 12 of those flights were used to investigate aerosol mixing state and the influence of aerosol source region on size-resolved hygroscopicity. The uniformity in size-resolved hygroscopicity was quantified to facilitate comparison between measurements made in different air masses. Hygroscopic growth factors are strongly dependent on source region and sizes. Mean hygroscopic growth factors were observed to be greatest when the air mass origin was from the south. The mean growth factors for continental sources decreased with initial size from 1.47 to 1.27 for $0.040{\mu}m\;and\;0.586{\mu}m$, but increased with initial size from 1.44 to 1.8 for $0.040{\mu}m\;and\;0.400{\mu}m$ dry diameters for marine sources.

Monitoring of Climate Change of Northeast Asia and Background Atmosphere in Korea

  • Oh, Sung-Nam;Chung, Hyo-Sang;Choi, Jae-Cheon;Bang, So-Young;Hyun, Myung-Suk
    • 한국환경과학회:학술대회논문집
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    • 한국환경과학회 2003년도 International Symposium on Clean Environment
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    • pp.232-235
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    • 2003
  • In general, the parameters of climate change include aerosol chemical compounds, aerosol optical depth, greenhouse gases(carbon dioxide, CFCs, methane, nitrous oxide, tropospheric ozone), ozone distribution, precipitation acidity and chemical compounds, persistent organic pollutants and heavy metals, radioactivity, solar radiation including ultra-violet and standard meteorological parameters. Over the last ten years, the monitoring activities of Korea regarding to the climate change have been progressed within the WMO GAW and ACE-Asia IOP programs centered at the observation sites of Anmyeon and Jeju Gosan islands respectively. The Greenhouse gases were pointed out that standard air quality monitoring techniques are required to enhance data comparability and that data presentation formats need to be harmonized and easily understood. Especially, the impact of atmospheric aerosols on climate depends on their optical properties, which, in turn, are a function of aerosol size distribution and the spectral reflective indices. Aerosol optical depth and single scattering albedo in the visible are used as the two basic parameters in the atmospheric temperature variation studies. The former parameter is an indicator of the attenuation power of aerosols, while the latter represents the relative strength of scattering and absorption by aerosols. For aerosols with weak absorption, surface temperature decreases as the optical depth increases because of the domination of backscattering. For aerosols with strong absorption, however, warming could occur as the optical depth increases. The objective of the study is to characterize the means, variability, and trends of Greenhouse gases and aerosol properties on a regional basis using data from its baseline observatories in Korea peninsula. A further goal is to understand the factors that control radiative forcing of the greenhouse and aerosol.

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에어로졸성막법으로 성막한 Bi:YIG 막의 광학적/자기적특성에 미치는 에어로졸 입사각도의 영향 (Aerosol Incident Angle Dependence of Optical and Magnetic Properties of Bi:YIG Films Deposited with Aerosol Deposition Method)

  • 신광호
    • 한국자기학회지
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    • 제18권1호
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    • pp.9-13
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    • 2008
  • 에어로졸 성막법으로 제작된 Bi:YIG($Bi_{0.5}Y_{2.5}Fe_5O_{12}$) 막에 있어서, 에어로졸 입사각도가 광학적 특성과 자기적 특정에 미치는 영향에 대하여 조사하였다. 에어로졸입사각도를 0도에서 30도로 증가시킴으로써 입사광의 파장이 450 nm일 때 광투과율은 약 80%의 향상이 얻어졌다. 그 이유는 에어로졸 입사각도를 높임으로써 입자간 응집체 등에 의해서 생성되는 막표면 혹은 막내부의 결함을 줄일 수 있기 때문으로 고찰되었다. 또한, 에어로졸 입사각도를 높임으로써 Bi:YIG막의 보자력을 크게 줄일 수 있다는 것을 실험적으로 검증할 수 있었다. 그 이유로는 에어로졸 입사각도를 높임으로써 입자와 기판간의 충돌에너지의 변화와 자벽이동의 방해가 되는 결함의 감소가 정성적으로 예상되었다.

전기방사 나노섬유 에어필터의 정전기적 특성 및 에어로졸 여과특성 (Aerosol filtration and electrostatic properties of electrospun nanofiber air filters)

  • 박현설;임경수
    • 한국입자에어로졸학회지
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    • 제5권2호
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    • pp.71-81
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    • 2009
  • In this study, Nylon 6,6 electrospun (ES) nanofiber filter media were prepared at various spinning conditions. The ES filters tested had no intrinsic electrical charges. The ES filters were triboelectrically charged in the course of filter sample handling, and the charge was drastically decayed in a few hours. On the other hand, the corona charged melt blown filter media showed a permanent electrical charge. The electrical charge state of the ES filters was also examined by comparing collection efficiencies of ES filters for uncharged and charged aerosol particles.

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MODIS센서를 이용한 aerosol의 계절별 특성 연구 (Studies on the aerosol Seasonal aerosol properties using MODIS sensor)

  • 한근혁;봉춘근;김동술
    • 한국대기환경학회:학술대회논문집
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    • 한국대기환경학회 2001년도 추계학술대회 논문집
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    • pp.119-120
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    • 2001
  • 우리나라에서는 에어로졸에 대해서 많은 관측과 분석이 이루어졌지만 바다와 육지의 에어로졸 분포에 대한 연구에는 어려움이 많았다. 인공위성자료를 이용하면 한반도와 주위의 바다가 한 화면에 나타나기 때문에 에어로졸의 공간분포 연구에 사용할 수 있다. 본 연구에서는 MODIS 자료를 이용해 에어로졸의 optical thickness를 이용하여 미세입자와 거대입자의 구성비를 구하고, 에어로졸의 공간 분포 및 특성을 연구하였다. (중략)

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Himawari-8/AHI 관측자료를 이용한 주요 대기 에어로솔 탐지 및 분류 방법 (Detection and Classification of Major Aerosol Type Using the Himawari-8/AHI Observation Data)

  • 이권호;이규태
    • 한국대기환경학회지
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    • 제34권3호
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    • pp.493-507
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    • 2018
  • Due to high spatio-temporal variability of amount and optical/microphysical properties of atmospheric aerosols, satellite-based observations have been demanded for spatiotemporal monitoring the major aerosols. Observations of the heavy aerosol episodes and determination on the dominant aerosol types from a geostationary satellite can provide a chance to prepare in advance for harmful aerosol episodes as it can repeatedly monitor the temporal evolution. A new geostationary observation sensor, namely the Advanced Himawari Imager (AHI), onboard the Himawari-8 platform, has been observing high spatial and temporal images at sixteen wavelengths from 2016. Using observed spectral visible reflectance and infrared brightness temperature (BT), the algorithm to find major aerosol type such as volcanic ash (VA), desert dust (DD), polluted aerosol (PA), and clean aerosol (CA), was developed. RGB color composite image shows dusty, hazy, and cloudy area then it can be applied for comparing aerosol detection product (ADP). The CALIPSO level 2 vertical feature mask (VFM) data and MODIS level 2 aerosol product are used to be compared with the Himawari-8/AHI ADP. The VFM products can deliver nearly coincident dataset, but not many match-ups can be returned due to presence of clouds and very narrow swath. From the case study, the percent correct (PC) values acquired from this comparisons are 0.76 for DD, 0.99 for PA, 0.87 for CA, respectively. The MODIS L2 Aerosol products can deliver nearly coincident dataset with many collocated locations over ocean and land. Increased accuracy values were acquired in Asian region as POD=0.96 over land and 0.69 over ocean, which were comparable to full disc region as POD=0.93 over land and 0.48 over ocean. The Himawari-8/AHI ADP algorithm is going to be improved continuously as well as the validation efforts will be processed by comparing the larger number of collocation data with another satellite or ground based observation data.

MODIS AEROSOL RETRIEVAL IN FINE SPATIAL RESOLUTION FOR LOCAL AND URBAN SCALE AIR QUALITY MONITORING APPLICATIONS

  • Lee, Kwon-Ho;Kim, Young-Joon
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2005년도 Proceedings of ISRS 2005
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    • pp.378-380
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    • 2005
  • Remote sensing of atmospheric aerosol using MODIS satellite data has been proven to be very useful in global/regional scale aerosol monitoring. Due to their large spatial resolution of $10km^2$ MODIS aerosol optical thickness (AOT) data have limitations for local/urban scale aerosol monitoring applications. Modified Bremen Aerosol Retrieval (BAER) algorithm developed by von Hoyningen-Huene et al. (2003) and Lee et al. (2005) has been applied in this study to retrieve AOT in fe resolutions of $500m^2$ over Korea. Look up tables (LUTs) were constructed from the aerosol properties based on sun-photometer observation and radiation transfer model calculations. It was found that relative error between the satellite products and the ground observations was within about $15\%$. Resulting AOT products were correlated with surface PMIO concentration data. There was good correlation between MODIS AOT and surface PM concentration under certain atmospheric conditions, which supports the feasibility of using the high-resolution MODIS AOT for local and urban scale air quality monitoring

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