6533b7d3fe1ef96bd126159c

RESEARCH PRODUCT

The novel HALO mini-DOAS instrument: inferring trace gas concentrations from airborne UV/visible limb spectroscopy under all skies using the scaling method

T. HünekeO.-a. AderholdJ. BouninM. DorfM. DorfE. GentryE. GentryK. GrossmannK. GrossmannJ.-u. GrooßP. HoorP. JöckelM. KenntnerM. KenntnerM. KnappM. KnechtD. LörksS. LudmannS. LudmannS. MatthesR. RaeckeM. ReichertJ. WeimarJ. WeimarB. WernerA. ZahnH. ZiereisK. Pfeilsticker

subject

Atmospheric Science010504 meteorology & atmospheric sciences0207 environmental engineering02 engineering and technology010502 geochemistry & geophysics01 natural sciencesUV/visible limb spectroscopylaw.inventionOpticslawErdsystem-Modellierungddc:550Nadirlcsh:TA170-171020701 environmental engineeringAbsorption (electromagnetic radiation)SpectroscopyScaling0105 earth and related environmental sciencesRemote sensingSpectrometerVerkehrsmeteorologielcsh:TA715-787business.industrylcsh:Earthwork. FoundationsAtmosphärische SpurenstoffeOptical spectrometerlcsh:Environmental engineeringTrace gasHALO mini-DOASEarth sciences13. Climate actionEnvironmental scienceHalobusiness

description

Abstract. We report on a novel six-channel optical spectrometer (further on called mini-DOAS instrument) for airborne nadir and limb measurements of atmospheric trace gases, liquid and solid water, and spectral radiances in the UV/vis and NIR spectral ranges. The spectrometer was developed for measurements from aboard the German High-Altitude and Long-Range (HALO) research aircraft during dedicated research missions. Here we report on the relevant instrumental details and the novel scaling method used to infer the mixing ratios of UV/vis absorbing trace gases from their absorption measured in limb geometry. The uncertainties of the scaling method are assessed in more detail than before for sample measurements of NO2 and BrO. Some first results are reported along with complementary measurements and comparisons with model predictions for a selected HALO research flight from Cape Town to Antarctica, which was performed during the research mission ESMVal on 13 September 2012.

https://doi.org/10.5194/amt-10-4209-2017