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Volume 17, issue 23
Atmos. Chem. Phys., 17, 14631-14643, 2017
https://doi.org/10.5194/acp-17-14631-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Quadrennial Ozone Symposium 2016 – Status and trends...

Atmos. Chem. Phys., 17, 14631-14643, 2017
https://doi.org/10.5194/acp-17-14631-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Dec 2017

Research article | 07 Dec 2017

Diurnal variations of BrONO2 observed by MIPAS-B at midlatitudes and in the Arctic

Gerald Wetzel1, Hermann Oelhaf1, Michael Höpfner1, Felix Friedl-Vallon1, Andreas Ebersoldt2, Thomas Gulde1, Sebastian Kazarski1, Oliver Kirner3, Anne Kleinert1, Guido Maucher1, Hans Nordmeyer1, Johannes Orphal1, Roland Ruhnke1, and Björn-Martin Sinnhuber1 Gerald Wetzel et al.
  • 1Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Karlsruhe, Germany
  • 2Karlsruhe Institute of Technology, Institute for Data Processing and Electronics, Karlsruhe, Germany
  • 3Karlsruhe Institute of Technology, Steinbuch Centre for Computing, Karlsruhe, Germany

Abstract. The first stratospheric measurements of the diurnal variation in the inorganic bromine (Bry) reservoir species BrONO2 around sunrise and sunset are reported. Arctic flights of the balloon-borne Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B) were carried out from Kiruna (68°N, Sweden) in January 2010 and March 2011 inside the stratospheric polar vortices where diurnal variations of BrONO2 around sunrise have been observed. High nighttime BrONO2 volume mixing ratios of up to 21pptv (parts per trillion by volume) were detected in late winter 2011 in the absence of polar stratospheric clouds (PSCs). In contrast, the amount of measured BrONO2 was significantly lower in January 2010 due to low available NO2 amounts (for the build-up of BrONO2), the heterogeneous destruction of BrONO2 on PSC particles, and the gas-phase interaction of BrO (the source to form BrONO2) with ClO. A further balloon flight took place at midlatitudes from Timmins (49°N, Canada) in September 2014. Mean BrONO2 mixing ratios of 22pptv were observed after sunset in the altitude region between 21 and 29km. Measurements are compared and discussed with the results of a multi-year simulation performed with the chemistry climate model ECHAM5/MESSy Atmospheric Chemistry (EMAC). The calculated temporal variation in BrONO2 largely reproduces the balloon-borne observations. Using the nighttime simulated ratio between BrONO2 and Bry, the amount of Bry observed by MIPAS-B was estimated to be about 21–25pptv in the lower stratosphere.

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We report the first stratospheric measurements of the diurnal variation in the inorganic bromine (Bry) reservoir species BrONO2 around sunrise and sunset. The main goal of these observations was to check the current understanding of stratospheric bromine chemistry and to estimate the amount of lower-stratospheric Bry. The calculated temporal variation in BrONO2 largely reproduces the balloon-borne observations. The amount of Bry was estimated to be about 21–25 pptv in the lower stratosphere.
We report the first stratospheric measurements of the diurnal variation in the inorganic bromine...
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