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Nitrogen compounds and ozone in the stratosphere: comparison of MIPAS satellite data with the chemistry climate model ECHAM5/MESSy1

Authors :
Benedikt Steil
Patrick Jöckel
Bernd Funke
Christoph Brühl
Gabriele Stiller
Atmospheric Chemistry Department [MPIC]
Max Planck Institute for Chemistry (MPIC)
Max-Planck-Gesellschaft-Max-Planck-Gesellschaft
Institute for Meteorology and Climate Research (IMK)
Karlsruhe Institute of Technology (KIT)
Instituto de Astrofísica de Andalucía (IAA)
Consejo Superior de Investigaciones Científicas [Madrid] (CSIC)
EGU, Publication
Source :
Atmospheric chemistry and physics, 7 (21), 5585–5598, Atmospheric Chemistry and Physics, Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (21), pp.5585-5598, Atmospheric Chemistry and Physics Discussions, Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2007, 7 (4), pp.9899-9924, Atmospheric Chemistry and Physics, Vol 7, Iss 21, Pp 5585-5598 (2007), ResearcherID
Publication Year :
2007
Publisher :
Copernicus GmbH, 2007.

Abstract

The chemistry climate model ECHAM5/MESSy1 (E5/M1) in a setup extending from the surface to 80 km with a vertical resolution of about 600 m near the tropopause with nudged tropospheric meteorology allows a direct comparison with satellite data of chemical species at the same time and location. Here we present results out of a transient 10~years simulation for the period of the Antarctic vortex split in September 2002, where data of MIPAS on the ENVISAT-satellite are available. For the first time this satellite instrument opens the opportunity, to evaluate all stratospheric nitrogen containing species simultaneously with a good global coverage, including the source gas N2O and ozone which allows an estimate for NOx-production in the stratosphere. We show correlations between simulated and observed species in the altitude region between 10 and 50 hpa for different latitude belts, together with the Probability Density Functions (PDFs) of model results and observations. This is supplemented by global maps on pressure levels showing the comparison between the satellite and the simulated data sampled at the same time and location. We demonstrate that the model in most cases captures the partitioning in the nitrogen family, the diurnal cycles and the spatial distribution within experimental uncertainty. This includes even variations due to tropospheric clouds. There appears to be, however, a problem to reproduce the observed nighttime partitioning between N2O5 and NO2 in the middle stratosphere using the recommended set of reaction coefficients and photolysis data.

Details

ISSN :
16807324, 16807316, 16807367, and 16807375
Volume :
7
Database :
OpenAIRE
Journal :
Atmospheric Chemistry and Physics
Accession number :
edsair.doi.dedup.....1c1890e45a265b7ba7e7ba3ec4dc55ff
Full Text :
https://doi.org/10.5194/acp-7-5585-2007