Atmos. Chem. Phys. Discuss., 11, 33511-33541, 2011
www.atmos-chem-phys-discuss.net/11/33511/2011/
doi:10.5194/acpd-11-33511-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Global stratospheric hydrogen peroxide distribution from MIPAS-Envisat full resolution spectra compared to KASIMA model results
S. Versick1,2, G. P. Stiller1, T. von Clarmann1, T. Reddmann1, N. Glatthor1, U. Grabowski1, M. Höpfner1, S. Kellmann1, M. Kiefer1, A. Linden1, R. Ruhnke1, and H. Fischer1
1Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Germany
2Steinbuch Centre for Computing, Karlsruhe Institute of Technology, Germany

Abstract. MIPAS-ENVISAT full resolution spectra were analyzed to obtain a global distribution of hydrogen peroxide (H2O2) in the stratosphere. H2O2 acts as reservoir gas for the HOx family (=H+OH+HO2) and thus, observations of H2O2 provide a better understanding of the HOx chemistry in the atmosphere. A retrieval approach based on constrained least squares fitting was developed and applied to small dedicated spectral analysis windows with maximum H2O2 information and minimum contribution of interfering gases. Due to a low signal to noise ratio in the measured spectra single profiles cannot be used for scientific interpretation and about 100 profiles have to be averaged temporally or spatially. Our retrievals of H2O2 from MIPAS measurements provide meaningful results between approximately 20 and 60 km. A possible impact by the high uncertainty of the reaction rate constant for HO2 + HO2→H2O2 + O2 in our 3d-CTM KASIMA is discussed. We find best agreement between model and observations for applying rate constants according to Christensen et al. (2002). The observations were compared to the model results of KASIMA focusing on low to mid latitudes. Good agreement in spatial distribution and in temporal evolution was found. Highest vmr of H2O2 in the stratosphere were observed and modeled in low latitudes shortly after equinox at about 30 km. The modelled diurnal cycle with lowest vmr shortly after sunrise and highest vmr in the afternoon is confirmed by the MIPAS observations.

Citation: Versick, S., Stiller, G. P., von Clarmann, T., Reddmann, T., Glatthor, N., Grabowski, U., Höpfner, M., Kellmann, S., Kiefer, M., Linden, A., Ruhnke, R., and Fischer, H.: Global stratospheric hydrogen peroxide distribution from MIPAS-Envisat full resolution spectra compared to KASIMA model results, Atmos. Chem. Phys. Discuss., 11, 33511-33541, doi:10.5194/acpd-11-33511-2011, 2011.
 
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