Evaluation of UV–visible MAX-DOAS aerosol profiling products by comparison with ceilometer, sun photometer, and in situ observations in Vienna, Austria

• Published in: Atmospheric measurement techniques Vol. 14; no. 8; pp. 5299 - 5318
• Main Authors: Schreier, Stefan F, Bösch, Tim, Richter, Andreas, Lange, Kezia, Revesz, Michael, Weihs, Philipp, Vrekoussis, Mihalis, Lotteraner, Christoph
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 03.08.2021; Copernicus Publications
• Subjects: Absorption spectroscopy; Aerosol extinction; Aerosol optical depth; Aerosols; Algorithms; Analytical methods; Atmospheric aerosols; Azimuth; City centres; Coefficients; Correlation coefficient; Correlation coefficients; Gases; Instruments; Mathematical analysis; Measurement techniques; Natural resources; Nitrogen dioxide; Optical analysis; Optical instruments; Optical properties; Optical thickness; Performance evaluation; Photometers; Profiles; Profiling; Radiation; Remote sensing; Seasons; Sondes; Spatial variability; Spatial variations; Spectroscopy; Spring; Spring (season); Sun; Temporal variations; Trace gases; Ultraviolet radiation; Urban environments; Variability; Vertical profiles; Weighting functions; Winter; Austria
• ISSN: 1867-8548; 1867-1381; 1867-8548
• DOI: 10.5194/amt-14-5299-2021

Since May 2017 and August 2018, two ground-based MAX-DOAS (multi-axis differential optical absorption spectroscopy) instruments have been continuously recording daytime spectral UV–visible measurements in the northwest (University of Natural Resources and Life Sciences (BOKU) site) and south (Arsenal site), respectively, of the Vienna city center (Austria). In this study, vertical aerosol extinction (AE) profiles, aerosol optical depth (AOD), and near-surface AE are retrieved from MAX-DOAS measurements recorded on cloud-free days applying the Bremen Optimal estimation REtrieval for Aerosols and trace gaseS (BOREAS) algorithm. Measurements of atmospheric profiles of pressure and temperature obtained from routinely performed sonde ascents are used to calculate box-air-mass factors and weighting functions for different seasons. The performance of BOREAS was evaluated against co-located ceilometer, sun photometer, and in situ instrument observations covering all four seasons. The results show that the vertical AE profiles retrieved from the BOKU UV–visible MAX-DOAS observations are in very good agreement with data from the co-located ceilometer, reaching correlation coefficients (R) of 0.936–0.996 (UV) and 0.918–0.999 (visible) during the fall, winter, and spring seasons. Moreover, AE extracted using the lowest part of MAX-DOAS vertical profiles (up to 100 m above ground) is highly consistent with near-surface ceilometer AE (R>0.865 and linear regression slopes of 0.815–1.21) during the fall, winter, and spring seasons. A strong correlation is also found for the BOREAS-based AODs when compared to the AERONET ones. Notably, the highest correlation coefficients (R=0.953 and R=0.939 for UV and visible, respectively) were identified for the fall season. While high correlation coefficients are generally found for the fall, winter, and spring seasons, the results are less reliable for measurements taken during summer. For the first time, the spatial variability of AOD and near-surface AE over the urban environment of Vienna is assessed by analyzing the retrieved and evaluated BOREAS aerosol profiling products in terms of different azimuth angles of the two MAX-DOAS instruments and for different seasons. We found that the relative differences of averaged AOD between different azimuth angles are 7–13 %, depending on the season. Larger relative differences of up to 32 % are found for near-surface AE in the different azimuthal directions. This study revealed the strong capability of BOREAS to retrieve AE profiles, AOD, and near-surface AE over urban environments and demonstrated its use for identifying the spatial variability of aerosols in addition to the temporal variation.