Atmospheric Chemistry and Physics www.atmos-chem-phys.net 1680-7316 1680-7324 7 9 2007 10.5194/acp-7-2357-2007 http://www.atmos-chem-phys.net/7/2357/2007/ http://www.atmos-chem-phys.net/7/2357/2007/acp-7-2357-2007.html http://www.atmos-chem-phys.net/7/2357/2007/acp-7-2357-2007.pdf 2357 2369 2007-05-09 Mid-latitude ozone changes: studies with a 3-D CTM forced by ERA-40 analyses W. Feng M. P. Chipperfield M. Dorf K. Pfeilsticker P. Ricaud Institute for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK Institute für Umweltphysik, University of Heidelberg, Heidelberg, Germany Laboratoire d'Aerologie, Observatoire Midi-Pyrenees, Toulouse, France We have used an off-line three-dimensional (3-D) chemical transport model (CTM) to study long-term changes in stratospheric O₃. The model was run from 1977–2004 and forced by ECMWF ERA-40 and operational analyses. Model runs were performed to examine the impact of increasing halogens and additional stratospheric bromine from short-lived source gases. The analyses capture much of the observed interannual variability in column ozone, but there are also unrealistic features. In particular the ERA-40 analyses cause a large positive anomaly in northern hemisphere (NH) column O₃ in the late 1980s. Also, the change from ERA-40 to operational winds at the start of 2002 introduces abrupt changes in some model fields (e.g. temperature, ozone) which affect analysis of trends. The model reproduces the observed column increase in NH mid-latitudes from the mid 1990s. Analysis of a run with fixed halogens shows that this increase is not due to a significant decrease in halogen-induced loss, i.e. is not an indication of recovery. The model predicts only a small decrease in halogen-induced loss after 1999. In the upper stratosphere, despite the modelled turnover of chlorine around 1999, O₃ does not increase because of the effects of increasing ECMWF temperatures, decreasing modelled CH₄ at this altitude, and abrupt changes in the SH temperatures at the end of the ERA-40 period. The impact of an additional 5 pptv stratospheric bromine from short-lived species decreases mid-latitude column O₃ by about 10 DU. However, the impact on the modelled relative O₃ anomaly is generally small except during periods of large volcanic loading. Chipperfield, M. P.: Multiannual simulations with a three-dimensional chemical transport model, \JGR, 104, 1781–1805, 1999. Chipperfield, M. P.: A three-dimensional model study of long-term mid-high latitude lower stratosphere ozone changes, Atmos. Chem. Phys., 3, 1253–1265, 2003. Chipperfield, M. P.: New Version of the TOMCAT/SLIMCAT Off-Line Chemical Transport Model: Intercomparison of Stratospheric Tracer Experiments, Q. J. R. Meteorol. 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