Abstract

Abstract. The use of satellite NO2 data for air quality studies is increasingly revealing the need for observations with higher spatial and temporal resolution. The study of the NO2 diurnal cycle, global sub-urban-scale observations, and identification of emission point sources are some examples of important applications not possible at the resolution provided by current instruments. One way to achieve increased spatial resolution is to reduce the spectral information needed for the retrieval, allowing both dimensions of conventional 2-D detectors to be used to record spatial information. In this work we investigate the use of 10 discrete wavelengths with the well-established differential optical absorption spectroscopy (DOAS) technique for NO2 slant column density (SCD) retrievals. To test the concept we use a selection of individual OMI and TROPOMI Level 1B swaths from various regions around the world, which contain a mixture of clean and heavily polluted areas. To discretise the data we simulate a set of Gaussian optical filters centred at various key wavelengths of the NO2 absorption cross section. We perform SCD retrievals of the discrete data using a simple implementation of the DOAS algorithm and compare the results with the corresponding Level 2 SCD products, namely QA4ECV for OMI and the operational TROPOMI product. For OMI the overall results from our discrete-wavelength retrieval are in very good agreement with the Level 2 data (mean difference <5 %). For TROPOMI the agreement is good (mean difference <11 %), with lower uncertainty owing to its higher signal-to-noise ratio. These discrepancies can be mostly explained by the differences in retrieval implementation. There are some larger differences around the centre of the swath and over water. While further research is needed to address specific retrieval issues, our results indicate that our method has potential. It would allow for simpler, more economic satellite instrument designs for NO2 monitoring at high spatial and temporal resolution. Constellations of small satellites with such instruments on board would be a valuable complement to current and upcoming high-budget hyperspectral instruments.

Highlights

  • Nitrogen dioxide (NO2) is a gaseous air pollutant from the NOx family (NOx = NO + NO2) that exists in trace amounts in the atmosphere

  • The NO2 slant column density (SCD) results from our DWDOAS retrieval of selected single orbits from January 2005 are compared with the corresponding Ozone Monitoring Instrument (OMI) QA4ECV NO2 product

  • The largest differences are found around the centre of each swath, which coincides with the areas with the lowest SCDs in the QA4ECV dataset

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Summary

Introduction

Nitrogen dioxide (NO2) is a gaseous air pollutant from the NOx family (NOx = NO + NO2) that exists in trace amounts in the atmosphere. Its sources are of natural origin (e.g. lightning, volcanoes, and microbial activity) or a result of anthropogenic activities (e.g. agricultural biomass burning, fossil fuel combustion). Most of the background NO2 is in the stratosphere and is produced mainly by natural processes. In polluted areas tropospheric NO2 is predominant and its main sources are anthropogenic emissions, which occur close to the surface in the boundary layer. Other sources of tropospheric NO2 include fires, microbiological soil emissions, and lightning (Wallace and Hobbs, 2006). The most polluted regions are usually highly industrialised and densely populated urban areas, where the air pollution is complex due to the varied mix of constituents (Monks et al, 2009).

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