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Operational remote sensing of aerosols over land to account for directional effects

机译:对陆地上的气溶胶进行操作性遥感以说明方向性影响

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The assumption that the ground is a Lambertian reflector is commonly adopted in operational atmospheric corrections of spaceborne sensors. Through a simple modeling of directional effects in radiative transfer following the second simulation of the satellite signal in the solar spectrum (6S) approach, we propose an operational method to account for the departure from Lambertian behavior of a reflector covered by a scattering medium. This method relies on the computation of coupling terms between the reflecting and the scattering media and is able to deal with a two-layer atmosphere. We focus on the difficult problem of aerosol remote sensing over land. One popular sensing method relies on observations over dense dark vegetation, for which the surface reflectance is low and quite well defined in the blue and in the red. Therefore a study was made for three cases: (1) dark vegetation covered by atmospheric aerosols, (2) atmospheric aerosols covered by molecules, and finally (3) dark vegetation covered by atmospheric aerosols covered by molecules. Comparisons of top-of-the-atmosphere reflectances computed with our modeling and reference computations made with the successive-order-of-scattering code show the robustness of the modeling in the blue and in the red for aerosol optical thicknesses as great as 0.6 and solar zenith angles as large as 60°. The model begins to fail only in the blue for large solar zenith angles. The benefits expected for aerosol remote sensing over land are evaluated with an aerosol retrieval scheme developed for the Medium-Resolution Imaging Spectrometer. The main result is a better constraint on the aerosol model with inclusion of directional effects and a weaker effect on the optical thickness of the retrieved aerosol. The directional scheme is then applied to the aerosol remote-sensing problem in actual Indian Remote Sensing Satellite P3/Modular Optoelectronic Scanner images over land and shows significant improvement compared with a Lambertian algorithm. Moreover, it confirms our main theoretical conclusion.
机译:在星载传感器的实际大气校正中,通常采用地面是朗伯反射器的假设。通过在太阳光谱(6S)方法中对卫星信号进行第二次模拟之后,对辐射传递中的方向效应进行简单建模,我们提出了一种操作方法来解决被散射介质覆盖的反射器偏离朗伯行为的问题。该方法依赖于反射介质和散射介质之间耦合项的计算,并且能够处理两层气氛。我们专注于陆地上的气溶胶遥感难题。一种流行的感测方法依赖于在茂密的黑暗植被上进行的观测,对于这些植被,其表面反射率较低,并且蓝色和红色的清晰度非常好。因此,针对以下三种情况进行了研究:(1)大气气溶胶覆盖的黑暗植被,(2)分子覆盖的大气气溶胶,最后(3)分子覆盖的大气气溶胶覆盖的黑暗植被。通过我们的建模计算得到的最高大气反射率与通过连续散射码进行的参考计算的比较表明,对于气溶胶光学厚度最大为0.6和0.5的蓝色和红色,建模的鲁棒性。太阳天顶角高达60°。对于大太阳天顶角,该模型仅在蓝色处开始失效。使用为中分辨率成像光谱仪开发的气溶胶回收方案评估了陆上气溶胶遥感的预期收益。主要结果是对气溶胶模型的约束更好,包括方向性影响,对回收气溶胶光学厚度的影响较弱。然后将定向方案应用于实际的印度遥感卫星P3 /模块化光电扫描仪在陆地上的图像中的气溶胶遥感问题,并且与Lambertian算法相比,显示出明显的改进。此外,它证实了我们的主要理论结论。

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