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Intra-pixel variability in satellite tropospheric NO2 column densities derived from simultaneous spaceborne and airborne observations the MAD-CAT Campaign: inter-comparison and sensitivity studies on spectral analysis settings

机译:卫星对流层NO 2 柱密度的像素内变异性来自同时星载和空中观测maD-CaT运动:光谱分析设置的相互比较和灵敏度研究

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摘要

Aircraft measurements of NO2 using an imaging differential optical absorption spectrometer (iDOAS) instrument over the South African Highveld region in August 2007 are presented and compared to satellite measurements from OMI and SCIAMACHY. In-situ aerosol and trace-gas vertical profile measurements, along with aerosol optical thickness and single-scattering albedo measurements from the Aerosol Robotic Network (AERONET), are used to devise scenarios for a radiative-transfer modelling sensitivity study. Uncertainty in the air-mass factor due to variations in the aerosol and NO2 profile shape is constrained, and used to calculate vertical column densities (VCD), which are compared to co-located satellite measurements. The lower spatial resolution of the satellites cannot resolve the detailed plume structures revealed in the aircraft measurements. The airborne DOAS in general measured steeper horizontal gradients and higher peak NO2 vertical column density. Aircraft measurements close to major sources, spatially-averaged to the satellite resolution, indicate NO2 column densities more than twice those measured by the satellite. The agreement between the high-resolution aircraft instrument and the satellite instrument improves with distance from the source. Despite their low spatial resolution, satellite images reveal point sources and plumes that retain their structure for several hundred kilometers downwind.
机译:介绍了2007年8月在南非Highveld地区使用成像差分光学吸收光谱仪(iDOAS)进行的飞机NO2测量结果,并将其与OMI和SCIAMACHY的卫星测量结果进行了比较。利用气溶胶机器人网络(AERONET)进行的原位气溶胶和痕量气体垂直剖面测量,以及气溶胶光学厚度和单散射反照率测量,可用于设计辐射传输建模敏感性研究的方案。由于气溶胶和NO2轮廓形状的变化而导致的空气质量因数的不确定性受到限制,并用于计算垂直列密度(VCD),并将其与同地卫星测量结果进行比较。卫星的较低空间分辨率无法解决飞机测量中揭示的详细羽状结构。机载DOAS通常可测得更陡的水平梯度和更高的NO2垂直色谱柱密度峰值。在接近主要来源的飞机测量值(在空间上平均为卫星分辨率)显示,NO2柱密度是卫星测量值的两倍以上。高分辨率飞机仪表和卫星仪表之间的协议随着距信号源距离的增加而提高。尽管其空间分辨率较低,但卫星图像仍显示出点源和羽流,这些点源和羽流在向下的几百公里处仍保持其结构。

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