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Observations of three-dimensional radiative effects that influence MODIS cloud optical thickness retrievals

机译:影响MODIS云光学厚度检索的三维辐射效应的观察

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When cloud properties are retrieved from satellite observations, current calculations apply one-dimensional (1D) theory to the three-dimensional (3D) world: they consider only vertical processes and ignore horizontal interactions. This paper proposes a novel approach that estimates 3D effects in cloud optical thickness retrievals. The proposed method combines visible and thermal infrared images to see whether 3D radiative effects make clouds appear asymmetric-that is, whether cloud surfaces tilted toward the sun are systematically brighter than surfaces tilted away from it. The observed asymmetries are then used to estimate 3D effects for 1-km-size pixels as well as 50-km-size areas. Initial results obtained for Moderate-Resolution Imaging Spectroradiometer (MODIS) images reveal that 3D effects cause abundant uncertainties in the 1-km-resolution 1D retrievals. Averaging over 50 km by 50 km areas greatly reduces the errors but does not remove them completely. Conservative estimates show that the mean optical thickness values are biased by more than 10% in 10% of the areas, and the errors in the areas' standard deviation values are more than 10% in about 20% of areas. [References: 24]
机译:当从卫星观测中获取云特性时,当前的计算将一维(1D)理论应用于三维(3D)世界:它们仅考虑垂直过程,而忽略水平相互作用。本文提出了一种新颖的方法,可以估算云光学厚度检索中的3D效果。所提出的方法结合了可见光图像和热红外图像,以查看3D辐射效应是否使云显得不对称-也就是说,朝太阳倾斜的云表面是否比从太阳倾斜的表面系统地更亮。然后,将观察到的不对称性用于估计1公里大小的像素以及50公里大小的区域的3D效果。对于中分辨率成像光谱仪(MODIS)图像获得的初步结果表明,3D效应在1 km分辨率的1D检索中引起大量不确定性。将50 km x 50 km区域平均可以大大减少错误,但不能完全消除。保守估计表明,平均光学厚度值在10%的区域中偏差超过10%,并且在大约20%的区域中,标准偏差值的误差超过10%。 [参考:24]

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