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Assessment of the Level-3 MODIS daily aerosol optical depth in the context of surface solar radiation and numerical weather modeling

机译:在地面太阳辐射和数值天气模拟的背景下评估MODIS 3级日常气溶胶光学深度

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摘要

The daily Level-3 MODIS aerosol optical depth (AOD) product is a global daily spatial aggregation of the Level-2 MODIS AOD (10-km spatial resolution) into a regular grid with a resolution of 1° × 1°. It offers interesting characteristics for surface solar radiation and numerical weather modeling applications. However, most of the validation efforts so far have focused on Level-2 products and only rarely on Level 3. In this contribution, we compare the Level-3 Collection 5.1 MODIS AOD dataset from the Terra satellite available since 2000 against observed daily AOD values at 550 nm from more than 500 AERONET ground stations around the globe. Overall, the mean error of the dataset is 0.03 (17%, relative to the mean ground-observed AOD), with a root mean square error of 0.14 (73%, relative to the same), but these errors are also found highly dependent on geographical region. We propose new functions for the expected error of the Level-3 AOD, as well as for both its mean error and its standard deviation. Additionally, we investigate the role of pixel count vis-à-vis the reliability of the AOD estimates, and also explore to what extent the spatial aggregation from Level 2 to Level 3 influences the total uncertainty in the Level-3 AOD. Finally, we use a radiative transfer model to investigate how the Level-3 AOD uncertainty propagates into the calculated direct normal and global horizontal irradiances.
机译:每天的3级MODIS气溶胶光学深度(AOD)产品是2级MODIS AOD(10公里空间分辨率)的全球日空间聚集,形成规则分辨率为1°×1°的规则网格。它为表面太阳辐射和数值天气建模应用提供了有趣的特性。但是,到目前为止,大多数验证工作都集中在2级产品上,很少关注3级产品。在此贡献中,我们将2000年以来可用的Terra卫星的3级采集5.1 MODIS AOD数据集与观测到的每日AOD值进行了比较550纳米来自全球500多个AERONET地面站。总体而言,数据集的平均误差为0.03(相对于平均地面观测AOD为17%),均方根误差为0.14(相对于地面平均AOD为73%),但这些误差也被高度依赖在地理区域上。我们针对Level-3 AOD的预期误差及其平均误差和标准偏差提出了新的功能。此外,我们调查了像素数相对于AOD估计值的可靠性的作用,还探讨了从第2级到第3级的空间聚集在多大程度上影响了第3级AOD的总不确定性。最后,我们使用辐射传输模型来研究3级AOD不确定度如何传播到所计算的直接法向和全局水平辐照度中。

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