基于MAX-DOAS测量的华北城市气溶胶和云分类及其与多遥感数据的比较

J. Jin, Yong Zhang, Yang Wang, Qing Zhou, Shanshan Lv, Jianzhong Ma
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引用次数: 0

摘要

多轴差分光学吸收光谱(Multi-Axis Differential Optical Absorption Spectroscopy,简称MAX-DOAS)是一项蓬勃发展的地面被动遥感技术,它利用从不同轴角测量的散射阳光来获取低层大气中气溶胶和微量气体的垂直特征。云对大气辐射传输过程有明显的影响,从而影响垂直分布的反演,因此对云的性质进行研究和分类是必要的。在本研究中,基于MAX-DOAS观测得到的几个关键量,如亮度、颜色指数和氧二聚体的吸收$\text{O}_{\mathbf{4}}$等,开发了云识别和分类算法脚本。将该算法应用于2017年夏季华北特大城市北京南城$(39.81 ^{\circ}\mathrm {N}, 116.47 ^{\circ}\mathrm {E})$的两个月MAX-DOAS观测。建立了具有较高时间分辨率的云分类数据集。利用MPIC的PriAM方法,得到了气溶胶廓线、近地表气溶胶消光和气溶胶光密度。结果被系统地与几种遥感技术进行了比较,如MODIS、太阳光度计和毫米波云雷达,这些技术以前很少被做过。在不同的气溶胶和云场景下,实现了大致的一致性和良好的一致性,保证了云识别分类算法脚本的可靠性和MAX-DOAS提供气溶胶和云信息的可靠能力。这进一步表明,为了减少气溶胶和云的影响,提高MAX-DOAS垂直柱密度和剖面的反演精度,未来还需要进行更深入的研究。
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Aerosol and Cloud Classifications Derived from MAX-DOAS Measurements in Urban North China and their Comparisons to Multiple Remote Sensing Datasets
Multi-Axis Differential Optical Absorption Spectroscopy, MAX-DOAS for short, is a thriving ground-based passive remote sensing technique, which retrieves the vertical characteristics of aerosol and trace gases in the lower atmosphere using scattered sunlight measured from different axis angles. Clouds have obvious influence on atmospheric radiative transfer process and thus affect the inversion of vertical distribution, making it essential to study and classify the cloud properties. In this study, a cloud identification and classification algorithm script was developed based on several key quantities derived from MAX-DOAS observations, like radiance, color index and the absorption of oxygen dimer $\text{O}_{\mathbf {4}}$ et al. The algorithm was applied to two-month’s MAX-DOAS observations in southern urban Beijing $( 39.81 ^{\circ}\mathrm {N}, 116.47 ^{\circ}\mathrm {E})$, the megacity in North China, in summer 2017. A cloud classification dataset was created with relatively high time resolution. Aerosol profiles, near surface aerosol extinction and AOD (aerosol optical density) were derived as well by applying PriAM methods of MPIC. The results were compared systematically to several remote sensing techniques, like MODIS, sun photometer and Millimeter wave cloud radar, which have rarely been done before. General consistency and good agreement were achieved under respective aerosol and cloud scenarios, assuring the reliability of the cloud identification and classification algorithm script and the dependable capability of MAX-DOAS to provide aerosol and cloud information. This further indicates that more thorough studies should be carried out to diminish the influence of aerosol and cloud and improve the retrieval accuracy of vertical column densities and profiles from MAX-DOAS in the future.
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