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Aerosol optical depth and surface reflectance retrieval over land using geostationary satellite data

机译:利用对地静止卫星数据反演陆地上的气溶胶光学深度和表面反射率

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In this paper, an analytical strategy is presented to retrieve jointly aerosol optical depth (AOD) and surface reflectance (R) from geostationary satellites. The new algorithm is based on a parameterization of the atmospheric radiative transfer model. Taking AOD and R as unknown parameters and based on some reasonable assumptions of AOD's spatial consistence and R's temporal invariance, both parameters of each pixel can be derived. Applying this algorithm to data from the Spinning Enhanced Visible and Infrared Imager (SEVIRI) observations on board Meteosat Second Generation (MSG), we obtain regional maps of AOD and R from two adjacent observations. Preliminary validation results by comparing our retrieved AOD with Aerosol Robotic Network (AERONET) data show good accuracy, and retrieved R is also reasonable. This method is potential to be applied in instantaneously monitoring aerosol spatio-temporal variation using geostationary satellite sensors with only one single visible channel and high-frequency observations.
机译:本文提出了一种从对地静止卫星中共同检索气溶胶光学深度(AOD)和表面反射率(R)的分析策略。新算法基于大气辐射传递模型的参数化。将AOD和R作为未知参数,并基于AOD的空间一致性和R的时间不变性的合理假设,可以得出每个像素的两个参数。将这种算法应用于Meteosat第二代(MSG)上的自旋增强型可见光和红外成像仪(SEVIRI)观测值的数据,我们从两个相邻观测值获得AOD和R的区域图。通过将我们检索到的AOD与Aerosol机器人网络(AERONET)数据进行比较,初步验证结果显示出良好的准确性,并且检索到的R也很合理。该方法有可能应用在仅具有一个可见通道和高频观测的对地静止卫星传感器的瞬时监测气溶胶时空变化中。

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