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Retrieval of tropospheric NO2 columns over Berlin from high-resolution airborne observations with the spectrolite breadboard instrument

机译:用光谱仪面包板仪器从高分辨率机载观测中提取柏林对流层NO2柱

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摘要

This paper presents the retrieval method that was developed to derive tropospheric NOcolumns from UV/VIS spectral measurements obtained with the Spectrolite Breadboard Instrument during the AROMAPEX campaign in Berlin (April 2016). A typical DOAS retrieval approach is followed. For the calculation of air mass factors this study specifically focuses on the impact of the surface reflectance, which varies considerably from pixel to pixel over this urban region. Ground-based aerosol optical thickness measurements are used as prior information. It is shown that retrieved surface reflectance shows good agreement with those derived from Landsat 8 measurements performed on the same day. Furthermore we demonstrate that tropospheric NO columns retrieved for pairs of adjacent pixels are self-consistent in the sense that they do not show a substantial systematic dependence on surface reflectance, in contrast to differential slant column densities. Also some cases are identified to illustrate this on a pixel-by-pixel level. An error budget is provided to quantify the impact of various assumptions on the accuracy of the retrieval of surface reflectance and tropospheric NO columns. Both in the morning and afternoon flight a NO plume is observed stretching out over Berlin from West to East. Peak values between 15 × 10 and 20 × 10 molec/cm are detected, whereas – at much lower spatial resolution – OMI detects peak values between 9 × 10 (first overpass) and 4 × 10 molec/cm (second overpass).
机译:本文介绍了一种检索方法,该方法是通过在柏林AROMAPEX活动期间(2016年4月)使用Spectrolite Breadboard仪器从UV / VIS光谱测量获得对流层NO柱而得出的。遵循典型的DOAS检索方法。为了计算空气质量因子,本研究特别关注表面反射率的影响,该反射率在该城市区域因像素而异。地面气溶胶光学厚度测量值用作先验信息。结果表明,与当天进行的Landsat 8测量得出的表面反射率具有很好的一致性。此外,我们证明,从对角线倾斜的密度不同,它们对表面反射率没有实质性的系统依赖性的意义上说,对对相邻像素对取回的对流层NO列是自洽的。还确定了一些情况,以逐像素的方式对此进行说明。提供误差预算以量化各种假设对表面反射率和对流层NO柱反演精度的影响。在上午和下午的飞行中,都没有观察到从西到东在柏林上空延伸的羽状物。检测到的峰值在15××10和20×10摩尔/厘米之间,而–在较低的空间分辨率下,OMI检测到的峰值在9××10(第一次过桥)和4××10 10摩尔/厘米(第二过桥)之间。

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