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MODTRAN-based Retrieval of Aerosol Optical Thickness over Chiba Area from Himawari-8/AHI visible images

机译:基于MODTRAN的从Himawari-8 / AHI可见图像中检索千叶地区气溶胶光学厚度的方法

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Atmospheric aerosol has a pivotal role in both air-pollution and radiation budget studies. In this paper, we retrieve the spatial distribution of aerosol optical thickness (AOT) over Chiba Area from daytime images of Himawari-8 geostationary satellite. The concurrent data from ground-based measurements are used in the analysis, namely the temporal variation of AOT from a sunphotometer and sky-radiometer located at the Center for Environmental Remote Sensing (CEReS), Chiba University. Also, the information on vertical profiles of aerosols and clouds is obtained from the data of NIES (National Institute for Environmental Studies) lidar operated also on the campus of Chiba University. We employ the MODTRAN (MODerate resolution atmospheric TRANsmission) radiative transfer code for simulating the radiance components that reach the AHI sensor onboard the satellite. The retrieval of AOT is based on look-up tables (LUTs) that are calculated for plausible values of both AOT and the surface reflectance for each of the AHI bands. The choice of aerosol model is optimized with the help of sunphotometer and sky-radiometer data coupled with the surface-based weather and aerosol sampling data. Additional information that is available from the present approach is the influence of thin clouds such as cirrus, since the discrimination of aerosol and cirrus effects is usually a difficult task in most of the atmospheric correction studies. We discuss the seasonal changes of AOT and surface reflectance from the present analysis based on LUTs. It is demonstrated that for each season, the satellite data observed on a clear day with minimum aerosol loading can be used to establish a good reference for the analysis of various satellite data such as MODIS or Landsat to evaluate the AOT distribution over the Chiba area.
机译:大气气溶胶在空气污染和辐射预算研究中都具有举足轻重的作用。在本文中,我们从Himawari-8对地静止卫星的白天图像中检索了千叶地区气溶胶光学厚度(AOT)的空间分布。分析中使用了来自地面测量的并行数据,即位于千叶大学环境遥感中心(CEReS)的太阳光度计和天空辐射计产生的AOT的时间变化。另外,关于气溶胶和云的垂直剖面的信息是从也在千叶大学校园内运行的NIES(国家环境研究所)激光雷达的数据中获得的。我们使用MODTRAN(中等分辨率大气TRANsmission)辐射传输代码来模拟到达卫星上AHI传感器的辐射分量。 AOT的检索基于查找表(LUT),这些查找表是针对每个AHI频段的AOT和表面反射率的合理值而计算的。借助日光光度计和天空辐射计数据以及基于地面的天气和气溶胶采样数据,可以优化气溶胶模型的选择。从目前的方法中可以获得的其他信息是诸如卷云之类的薄云的影响,因为在大多数大气校正研究中,气溶胶和卷云效应的辨别通常是一项艰巨的任务。我们从当前基于LUT的分析中讨论了AOT和表面反射率的季节性变化。事实证明,对于每个季节,在晴朗的一天观察到的具有最小气溶胶负荷的卫星数据都可以用来为分析各种卫星数据(例如MODIS或Landsat)以评估千叶地区的AOT分布提供良好的参考。

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