Validation of TROPOMI tropospheric NO<sub>2</sub> columns using dual-scan multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements in Uccle, Brussels

<p>Ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements of aerosols and tropospheric nitrogen dioxide (<span class="inline-formula">NO<sub>2</sub></span>) were carried out in Uccle (50.8<span class="inline-formul...

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Bibliographic Details
Main Authors: E. Dimitropoulou, F. Hendrick, G. Pinardi, M. M. Friedrich, A. Merlaud, F. Tack, H. De Longueville, C. Fayt, C. Hermans, Q. Laffineur, F. Fierens, M. Van Roozendael
Format: Article
Language:English
Published: Copernicus Publications 2020-10-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/13/5165/2020/amt-13-5165-2020.pdf
Description
Summary:<p>Ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements of aerosols and tropospheric nitrogen dioxide (<span class="inline-formula">NO<sub>2</sub></span>) were carried out in Uccle (50.8<span class="inline-formula"><sup>∘</sup></span>&thinsp;N, 4.35<span class="inline-formula"><sup>∘</sup></span>&thinsp;E), Brussels, during 1 year from March 2018 until March 2019. The instrument was operated in both the UV and visible wavelength ranges in a dual-scan configuration consisting of two sub-modes: (1) an elevation scan in a fixed viewing azimuthal direction (the so-called main azimuthal direction) pointing to the northeast and (2) an azimuthal scan in a fixed low elevation angle (2<span class="inline-formula"><sup>∘</sup></span>). By applying a vertical profile inversion algorithm in the main azimuthal direction and a parameterization technique in the other azimuthal directions, near-surface <span class="inline-formula">NO<sub>2</sub></span> volume mixing ratios (VMRs) and vertical column densities (VCDs) were retrieved in 10 different azimuthal directions. The dual-scan MAX-DOAS dataset allows for partly resolving the horizontal distribution of <span class="inline-formula">NO<sub>2</sub></span> around the measurement site and studying its seasonal variations. Furthermore, we show that measuring the tropospheric <span class="inline-formula">NO<sub>2</sub></span> VCDs in different azimuthal directions improves the spatial colocation with measurements from the Sentinel-5 Precursor (S5P), leading to a reduction of the spread in validation results. By using <span class="inline-formula">NO<sub>2</sub></span> vertical profile information derived from the MAX-DOAS measurements, we also resolve a systematic underestimation in S5P <span class="inline-formula">NO<sub>2</sub></span> data due to the use of inadequate a priori <span class="inline-formula">NO<sub>2</sub></span> profile shape data in the satellite retrieval.</p>
ISSN:1867-1381
1867-8548