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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 10 | Copyright
Atmos. Meas. Tech., 7, 3459-3485, 2014
https://doi.org/10.5194/amt-7-3459-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Oct 2014

Research article | 09 Oct 2014

The Heidelberg Airborne Imaging DOAS Instrument (HAIDI) – a novel imaging DOAS device for 2-D and 3-D imaging of trace gases and aerosols

S. General1, D. Pöhler1, H. Sihler1, N. Bobrowski1, U. Frieß1, J. Zielcke1, M. Horbanski1, P. B. Shepson2, B. H. Stirm3, W. R. Simpson4, K. Weber5, C. Fischer5, and U. Platt1 S. General et al.
  • 1Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
  • 2Purdue University, Dept. of Chemistry, West Lafayette, IN, USA
  • 3Purdue University, Dept. of Aviation Technology, West Lafayette, IN, USA
  • 4Department of Chemistry and Biochemistry, University of Alaska, Fairbanks, AK, USA
  • 5University of Applied Sciences, Environmental Measurement Techniques, Düsseldorf, Germany

Abstract. Many relevant processes in tropospheric chemistry take place on rather small scales (e.g., tens to hundreds of meters) but often influence areas of several square kilometer. Thus, measurements of the involved trace gases with high spatial resolution are of great scientific interest. In order to identify individual sources and sinks and ultimately to improve chemical transport models, we developed a new airborne instrument, which is based on the well established Differential Optical Absorption Spectroscopy (DOAS) method. The Heidelberg Airborne Imaging DOAS Instrument (HAIDI) is a passive imaging DOAS spectrometer, which is capable of recording horizontal and vertical trace gas distributions with a resolution of better than 100 m. Observable species include NO2, HCHO, C2H2O2, H2O, O3, O4, SO2, IO, OClO and BrO.

Here we give a technical description of the instrument including its custom-built spectrographs and CCD detectors. Also first results from measurements with the new instrument are presented. These comprise spatial resolved SO2 and BrO in volcanic plumes, mapped at Mt. Etna (Sicily, Italy), NO2 emissions in the metropolitan area of Indianapolis (Indiana, USA) as well as BrO and NO2 distributions measured during arctic springtime in context of the BRomine, Ozone, and Mercury EXperiment (BROMEX) campaign, which was performed 2012 in Barrow (Alaska, USA).

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