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Optical properties of Asian dust aerosol by SeaWiFS and contemporaneous ground observation data

机译:海盗亚洲粉尘气雾剂的光学特性及同期观察数据

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Asian dust aerosol layer of 4-6 km altitude accompanied by low clouds was observed with a LIDAR in Tokyo urban area on April 10 2001. In addition, column-integrated size distribution of aerosol was measured with a SkyRadiometer. To synthesize the top of atmosphere (TOA) reflectance, radiative transfer simulation was conducted assuming aerosol/cloud vertical structure and aerosol size distribution that were estimated after the ground observations. The refractive index of Asian dust was derived from a laboratory measurement of sampled Chinese soil particles. The synthesized TOA reflectance was compared to the SeaWiFS-derived one sampled at the low cloud pixels whose airmass is the same as the one passed at the observation site. TOA reflectance of the one of Asian dust models compare generally well with few percent difference in reflectance. We estimated an affect of Asian dust aerosol to ocean color remote sensing. Simulated TOA radiance absorbed by Asian dust was 20.0 W/m2/μm/sr in 443 nm. It is suggest that the existence of Asian dust occurs to dervie negative water-leaving radiance.
机译:与4月10日2001年在东京市区一个LIDAR此外,观察到伴随着低云层4-6公里高度的亚灰尘气雾剂层,气雾剂的柱集成尺寸分布用SkyRadiometer测量。为了合成气氛(TOA)的反射率的顶部,辐射传输模拟是在假定气溶胶/云垂直结构和地面观测后估计,气雾剂的粒度分布。亚洲粉尘的折射率是从中国采集土壤颗粒的实验室测量得出。将合成的TOA反射率相比的SeaWiFS衍生一个在低云像素,其气团是一样的一个在观察部位通过采样。亚洲粉尘车型之一的TOA反射率一般比较好,在反射率百分之几的差别。我们估计亚洲沙尘气溶胶对海洋水色遥感的影响。通过亚灰尘吸收模拟TOA辐射为20.0瓦/平方米/微米/ SR在443纳米。据认为,亚洲粉尘存在发生dervie负离水辐射。

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