首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Algorithm to Retrieve Aerosol Optical Properties From High-Spectral-Resolution Lidar and Polarization Mie-Scattering Lidar Measurements
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Algorithm to Retrieve Aerosol Optical Properties From High-Spectral-Resolution Lidar and Polarization Mie-Scattering Lidar Measurements

机译:从高光谱分辨率激光雷达和偏振米氏散射激光雷达测量中检索气溶胶光学特性的算法

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We developed an algorithm to estimate the vertical profiles of extinction coefficients at 532 nm for three aerosol types that are water-soluble, soot, and dust particles, using the extinction and backscattering coefficients at 532 nm for total aerosols derived from high-spectral-resolution lidar (HSRL) measurements and the receiving signal at 1064 nm and total depolarization ratio at 532 nm measured with Mie scattering lidar (MSL). The mode radii, standard deviations, and refractive indexes for each aerosol component are prescribed by the optical properties of aerosols and clouds database; the optical properties for each aerosol component are computed from Mie theory on the assumption that their particles are spherical and homogeneous, except for dust. To consider the effect of nonsphericity, the dust lidar ratio at 532 nm is assumed to be 50 sr, the value that is reported for Asian dust from the other observational studies. We performed sensitivity study on retrieval errors. The errors in extinction coefficient for each aerosol component were smaller than 30% and 60% when the measurement errors were $pm$5% and $pm$ 10%. We demonstrated the ability of the algorithm by applying to the $ hbox{HSRL} + hbox{MSL}$ data measured at Tsukuba, Japan. Plumes consisting of water-soluble aerosols, soot, dust, or their mixture were retrieved; these results were consistent with simulation with a global aerosol transport model. Introducing the dust lidar ratio significantly improved a correlation between the retrieved dust concentration and the aerosol depolarization ratio at 532 nm derived from $ hbox{HSRL} + hbox{MSL}$ than the use of spherical dust optical model in the retrieval.
机译:我们开发了一种算法,用于估计水溶性,烟灰和粉尘颗粒这三种气溶胶类型在532 nm处的消光系数的垂直分布,使用源自高光谱分辨率的总气溶胶在532 nm处的消光系数和反向散射系数激光雷达(HSRL)测量,并使用Mie散射激光雷达(MSL)测量1064 nm处的接收信号和532 nm处的总去极化率。每种气溶胶组分的模式半径,标准偏差和折射率由气溶胶和云数据库的光学特性规定。每种气溶胶组分的光学特性是根据Mie理论计算得出的,假设它们的颗粒是球形且均质的,除了灰尘。为了考虑非球形性的影响,假设532 nm处的尘埃激光雷达比率为50 sr,该值是其他观测研究报告的亚洲尘埃的报告值。我们对检索错误进行了敏感性研究。当测量误差为$ pm $ 5%和$ pm $ 10%时,每种气溶胶成分的消光系数误差均小于30%和60%。我们通过应用在日本筑波市测量的$ hbox {HSRL} + hbox {MSL} $数据证明了该算法的能力。回收了由水溶性气溶胶,烟灰,灰尘或它们的混合物组成的羽状物;这些结果与使用全球气溶胶传输模型进行的模拟一致。引入粉尘激光雷达比,与在检索中使用球形粉尘光学模型相比,显着改善了从hbox {HSRL} + hbox {MSL} $导出的粉尘浓度与532 nm气溶胶去极化比之间的相关性。

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