Abstract

Abstract. The Airborne imaging differential optical absorption spectroscopy (DOAS) instrument for Measurements of Atmospheric Pollution (AirMAP) has been developed for the purpose of trace gas measurements and pollution mapping. The instrument has been characterized and successfully operated from aircraft. Nitrogen dioxide (NO2) columns were retrieved from the AirMAP observations. A major benefit of the push-broom imaging instrument is the spatially continuous, gap-free measurement sequence independent of flight altitude, a valuable characteristic for mapping purposes. This is made possible by the use of a charge coupled device (CCD) frame-transfer detector. A broad field of view across track of around 48° is achieved with wide-angle entrance optics. This leads to a swath width of about the same size as the flight altitude. The use of fibre coupled light intake optics with sorted light fibres allows flexible instrument positioning within the aircraft and retains the very good imaging capabilities. The measurements yield ground spatial resolutions below 100 m depending on flight altitude. The number of viewing directions is chosen from a maximum of 35 individual viewing directions (lines of sight, LOS) represented by 35 individual fibres. The selection is adapted to each situation by averaging according to signal-to-noise or spatial resolution requirements. Observations at 30 m spatial resolution are obtained when flying at 1000 m altitude and making use of all 35 viewing directions. This makes the instrument a suitable tool for mapping trace gas point sources and small-scale variability. The position and aircraft attitude are taken into account for accurate spatial mapping using the Attitude and Heading Reference System of the aircraft. A first demonstration mission using AirMAP was undertaken in June 2011. AirMAP was operated on the AWI Polar-5 aircraft in the framework of the AIRMETH-2011 campaign. During a flight above a medium-sized coal-fired power plant in north-west Germany, AirMAP clearly detected the emission plume downwind from the exhaust stack, with NO2 vertical columns around 2 × 1016 molecules cm−2 in the plume centre. NOx emissions estimated from the AirMAP observations are consistent with reports in the European Pollutant Release and Transfer Register. Strong spatial gradients and variability in NO2 amounts across and along flight direction are observed, and small-scale enhancements of NO2 above a motorway are detected.

Highlights

  • Nitrogen dioxide, NO2, is an important trace gas in the Earth’s atmosphere

  • The present study introduces the push-broom Airborne imaging differential optical absorption spectroscopy (DOAS) instrument for Measurements of Atmospheric Pollution (AirMAP), which is well suited for trace gas mapping of comparably small-scale emissions at fine spatial resolution

  • The instantaneous field of view (FOV) (IFOV) along track is around 1.2◦, while the effective FOV along track is given by the convolution of the IFOV with the travelled distance

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Summary

Introduction

NO2, is an important trace gas in the Earth’s atmosphere. NO2 and nitrogen monoxide, NO, are coupled together by the reaction of NO with ozone, O3, which produces NO2 and the photolysis of the latter which produces NO. DOAS measurements from high-altitude balloons yield NO2 columns and vertical profiles in the stratosphere (Pfeilsticker and Platt, 1994), and observations from aircraft yield tropospheric NO2 amounts over emission point sources and polluted regions (Melamed et al, 2003; Wang et al, 2005), as well as from shipping emissions (Berg et al, 2012) Such airborne measurements are valuable for satellite validation (Heue et al, 2005). The present study introduces the push-broom Airborne imaging DOAS instrument for Measurements of Atmospheric Pollution (AirMAP), which is well suited for trace gas mapping of comparably small-scale emissions at fine spatial resolution. The NO2 column amount was observed during multiple overpasses over the power plant exhaust plume

Instrumental set-up
Objective
Field of view
Aircraft angles and correction of geolocation
Instrument quality
Spatial resolution and imaging quality
Spectral resolution and spectral response function
Observations of NO2
Retrieval settings
NO2 slant columns and retrieval quality
Air mass factors for tropospheric NO2
NO2 vertical columns
Power plant emissions
Wind data
Calculation and discussion of the emission rate
Comparison to emission reports
Limitations of the emission calculations
Non-uniform plume dispersion
Error estimates
Uncertainties of the vertical NO2 columns
Uncertainties of the path element length
Uncertainties of the wind speed and direction
Findings
NO2 above motorways
10 Conclusions and outlook
Full Text
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