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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >A global analysis on the view-angle dependence of plane-parallel oceanic liquid water cloud optical thickness using data synergy from MISR and MODIS
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A global analysis on the view-angle dependence of plane-parallel oceanic liquid water cloud optical thickness using data synergy from MISR and MODIS

机译:利用MISR和MODIS的数据协同效应对平面平行海洋液态水云光学厚度的视角依赖性进行全局分析

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摘要

We examine the viewing zenith angle dependent bias (VZA bias) in warm cloud optical thickness (τ) retrieved from a plane-parallel approach applied to fused Moderate Resolution Imaging Spectroradiometer (MODIS) and Multi-angle Imaging SpectroRadiometer (MISR) data for the months of January and July between 2001 and 2008. The near-simultaneous multiple view-angle observations from MISR offers many advantages over previous τ-VZA bias studies: 1) The analysis no longer requires seasonal and latitudinal cloud invariant assumptions, 2) consistent cloudy scene identification with VZA, 3) stratification of VZA-bias with scene characteristics, and 4) a greater range of sun-view geometries. Contrasting results between previous studies are resolved through careful consideration of the relative azimuth angle (RAZ) between sun and view. Relative to nadir-retrieved τ, τ increases in both forward- and backscatter directions with higher value in backscatter directions for solar zenith angle (SZA) < ~40°. For SZA ~40°, τ increases with increasing VZA in backscatter directions and strongly decreases in forward-scatter directions. For the most oblique views, ~40-100% absolute monthly mean differences relative to nadir-retrieved τ is common. This behavior is strongly tied to the sampled RAZ and explained based on three factors tied to the spatial heterogeneity of clouds. These factors also explain the behavior of the τ-VZA bias when stratified by nadir-retrieved τ and spatial heterogeneity, even in the thin-cloud limit where sun-glint effects are evident. We also observe an underestimation of τ relative to nadir in the rainbow-scattering directions and attribute it to an overestimation of the cloud-drop effective radius retrieved from MODIS due to cloud heterogeneity. There remains a need to quantify the bias in nadir-retrieved τ as a function of SZA and spatial heterogeneity as a step toward providing bias correction over a wide range of sun-view geometries.
机译:我们检查了几个月以来从适用于融合中分辨率成像光谱仪(MODIS)和多角度成像光谱仪(MISR)数据的平面平行方法获取的暖云光学厚度(τ)中与天顶角度相关的偏差(VZA偏差)从2001年到2008年的1月和7月。从先前的τ-VZA偏差研究来看,MISR几乎同时进行的多视角观测提供了许多优势:1)分析不再需要季节性和纬度云不变性假设,2)一致的多云场景使用VZA进行识别; 3)具有场景特征的VZA偏差分层;以及4)更大范围的太阳视图几何形状。通过仔细考虑太阳和视图之间的相对方位角(RAZ),可以解决以前研究之间的对比结果。相对于最低点τ,对于太阳天顶角(SZA)<〜40°,τ在向前和向后散射方向上均增加,在向后散射方向上具有更高的值。对于大约40°的SZA,τ随反向散射方向上VZA的增加而增加,而沿向前散射方向则大大降低。对于最倾斜的视图,相对于最低点τ的绝对月平均差异约为40-100%。此行为与采样的RAZ紧密相关,并基于与云的空间异质性相关的三个因素进行了解释。这些因素也解释了当被最低谷τ和空间异质性分层时τ-VZA偏斜的行为,即使在薄云层边界中也有明显的日照效应。我们还观察到了在彩虹散射方向上相对于最低点的τ的低估,并将其归因于由于云异质性而从MODIS检索到的有效云滴有效半径。仍然有必要对作为SZA和空间异质性的函数的最低天平τ中的偏差进行量化,以作为在广泛的太阳视几何范围内提供偏差校正的步骤。

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