2014
DOI: 10.5194/amtd-7-2187-2014
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The Heidelberg Airborne Imaging DOAS Instrument (HAIDI) – a novel Imaging DOAS device for 2-D and 3-D imaging of trace gases and aerosols

Abstract: 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 DOAS method. The Heidelberg Airborne Ima… Show more

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Cited by 5 publications
(6 citation statements)
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“…Though their column densities were below the detection limits of our instrument in the weak plumes encountered during our survey on 16 July 2021, the halogen oxides BrO, OClO, and IO have all been measured in more vigorous volcanic plumes with DOAS instruments Theys et al, 2009General et al, 2014a;Schönhardt et al, 2017;Kern and Lyons, 2018). These species are not primarily emitted from volcanoes, but instead are formed from primary volcanogenic emissions in a complex series of chemical reactions that occur as the plume ages and constituents are mixed with background air Kelly et al, 2013;.…”
Section: Imaging Volcanic Gases Other Than Somentioning
confidence: 77%
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“…Though their column densities were below the detection limits of our instrument in the weak plumes encountered during our survey on 16 July 2021, the halogen oxides BrO, OClO, and IO have all been measured in more vigorous volcanic plumes with DOAS instruments Theys et al, 2009General et al, 2014a;Schönhardt et al, 2017;Kern and Lyons, 2018). These species are not primarily emitted from volcanoes, but instead are formed from primary volcanogenic emissions in a complex series of chemical reactions that occur as the plume ages and constituents are mixed with background air Kelly et al, 2013;.…”
Section: Imaging Volcanic Gases Other Than Somentioning
confidence: 77%
“…Markus et al test a variety of plume identification algorithms on the operational TROPOMI SO 2 product and identify the DBSCAN multi-class classification algorithms (Ester et al, 1996) as the most promising category for plume classification and segmentation in operational environments. In situations where even greater resolution or sensitivity are needed, airborne Imaging DOAS techniques offer a solution General et al, 2014a). Kern and Kelly describe the implementation of an airborne Imaging DOAS system specifically for remote sensing of volcanic emissions and demonstrate its capabilities in an airborne gas survey of volcanoes in Alaska.…”
mentioning
confidence: 99%
“…Strictly speaking, our Imaging DOAS measurements do not fulfill these assumptions because light is collected from a range of angles forming a swath above the aircraft. Therefore, each SCD must be multiplied by the cosine of the measurement zenith angle to obtain a geometrical approximation of the vertical column density (General et al, 2014b). However, as our swath angle θ is 27.2 deg (Figure 5), the maximum measurement zenith angle during level flight is only 13.6 deg, which yields a geometrical correction of less than 3%.…”
Section: Sensitivity To Trace Gas Plumesmentioning
confidence: 99%
“…Markus et al test a variety of plume identification algorithms on the operational TROPOMI SO 2 product and identify the DBSCAN multi-class classification algorithms (Ester et al, 1996) as the most promising category for plume classification and segmentation in operational environments. In situations where even greater resolution or sensitivity are needed, airborne Imaging DOAS techniques offer a solution (Louban et al, 2009;General et al, 2014a). Kern and Kelly describe the implementation of an airborne Imaging DOAS system specifically for remote sensing of volcanic emissions and demonstrate its capabilities in an airborne gas survey of volcanoes in Alaska.…”
mentioning
confidence: 99%