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Sentinel-5P TROPOMI NO2 retrieval: impact of version v2.2 improvements and comparisons with OMI and ground-based data.

Authors :
van Geffen, Jos
Eskes, Henk
Compernolle, Steven
Pinardi, Gaia
Verhoelst, Tijl
Lambert, Jean-Christopher
Sneep, Maarten
ter Linden, Mark
Ludewig, Antje
Boersma, K. Folkert
Veefkind, J. Pepijn
Source :
Atmospheric Measurement Techniques Discussions; 11/25/2021, p1-37, 37p
Publication Year :
2021

Abstract

Nitrogen dioxide (NO<subscript>2</subscript>) is one of the main data products measured by the Tropospheric Monitoring Instrument (TROPOMI) on the Sentinel-5 Precursor (S5P) satellite, which combines a high signal-to-noise ratio with daily global coverage and high spatial resolution. TROPOMI provides a valuable source of information to monitor emissions from local sources such as power plants, industry, cities, traffic and ships, and variability of these sources in time. Validation exercises of NO<subscript>2</subscript> version v1.2-v1.3 data, however, have revealed that TROPOMI's tropospheric vertical columns (VCDs) are too low by up to 50 % over highly polluted areas. These findings are mainly attributed to biases in the cloud pressure retrieval, the surface albedo climatology and the low resolution of the a-priori profiles derived from global simulations of the TM5-MP chemistry model. This study describes improvements in the TROPOMI NO<subscript>2</subscript> retrieval leading to version v2.2, operational since 1 July 2021. Compared to v1.x, the main changes are: (1) The NO<subscript>2</subscript>-v2.2 data is based on version 2 level-1B (ir)radiance spectra with improved calibration, which results in a small and fairly homogeneous increase of the NO<subscript>2</subscript> slant columns of 3 to 4 %, most of which ends up as a small increase of the stratospheric columns; (2) The cloud pressures are derived with a new version of the FRESCO cloud retrieval already introduced in NO<subscript>2</subscript>-v1.4, which lead to a lowering of the cloud pressure, resulting in larger tropospheric NO<subscript>2</subscript> columns over polluted scenes with a small but non- zero cloud coverage; (3) For cloud-free scenes a surface albedo correction is introduced based on the observed reflectance, which also leads to a general increase of the tropospheric NO<subscript>2</subscript> columns over polluted scenes of order 15 %; (4) An outlier removal was implemented in the spectral fit, which increases the number of good quality retrievals over the South-Atlantic Anomaly region and over bright clouds where saturation may occur; (5) Snow-Ice information is now obtained from ECMWF weather data, increasing the number of valid retrievals at high latitudes. On average the NO<subscript>2</subscript>-v2.2 data have tropospheric VCDs that are between 10 and 40 % larger than the v1.x data, depending on the level of pollution and season; the largest impact is found at mid- and high- latitudes in wintertime. This has brought these tropospheric NO<subscript>2</subscript> closer to OMI observations. Ground-based validation shows on average an improvement of the negative bias of the stratospheric (from -6 % to -3 %), tropospheric (from -32 % to -23 %) and total (from -12 % to -5 %) columns. For individual measurement stations, however, the picture is more complicated, in particular for the tropospheric and total columns. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
18678610
Database :
Complementary Index
Journal :
Atmospheric Measurement Techniques Discussions
Publication Type :
Academic Journal
Accession number :
153879694
Full Text :
https://doi.org/10.5194/amt-2021-329