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Volume 11, issue 15
Atmos. Chem. Phys., 11, 8103-8131, 2011
https://doi.org/10.5194/acp-11-8103-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 11, 8103-8131, 2011
https://doi.org/10.5194/acp-11-8103-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Aug 2011

Research article | 09 Aug 2011

Representation of tropical deep convection in atmospheric models – Part 2: Tracer transport

C. R. Hoyle1,2, V. Marécal5, M. R. Russo7, G. Allen14, J. Arteta5, C. Chemel4, M. P. Chipperfield3, F. D'Amato11, O. Dessens10, W. Feng3, J. F. Hamilton12, N. R. P. Harris9, J. S. Hosking10,**, A. C. Lewis12, O. Morgenstern7,*, T. Peter1, J. A. Pyle7, T. Reddmann8, N. A. D. Richards3, P. J. Telford9, W. Tian3, S. Viciani11, A. Volz-Thomas13, O. Wild6, X. Yang10, and G. Zeng7,* C. R. Hoyle et al.
  • 1Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
  • 2Department of Geosciences, University of Oslo, Norway
  • 3Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
  • 4NCAS-Weather, Centre for Atmospheric & Instrumentation Research, University of Herfordshire, UK
  • 5Centre National de Recherches Météorologiques/Groupe d'étude de l'Atmosphére Météorologique, Météo-France and CNRS, Toulouse, France
  • 6Lancaster Environment Centre, Lancaster University, UK
  • 7NCAS climate, Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, UK
  • 8Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
  • 9European Ozone Research Coordinating Unit, University of Cambridge Department of Chemistry, Lensfield Road, Cambridge CB2 1EW, UK
  • 10Centre for Atmospheric Science, University of Cambridge, Cambridge, UK
  • 11CNR-INO (Istituto Nazionale di Ottica) Largo E. Fermi, 6 50125 Firenze, Italy
  • 12University of York, Heslington, York, YO105DD, UK
  • 13Institute for Energy and Climate Research, Forschungszentrum Jülich, Germany
  • 14Centre for Atmospheric Science, University of Manchester, Manchester, UK
  • *now at: National Institute of Water and Atmospheric Research, Lauder, New Zealand
  • **now at: British Antarctic Survey, Cambridge, UK

Abstract. The tropical transport processes of 14 different models or model versions were compared, within the framework of the SCOUT-O3 (Stratospheric-Climate Links with Emphasis on the Upper Troposphere and Lower Stratosphere) project. The tested models range from the regional to the global scale, and include numerical weather prediction (NWP), chemical transport, and chemistry-climate models. Idealised tracers were used in order to prevent the model's chemistry schemes from influencing the results substantially, so that the effects of modelled transport could be isolated. We find large differences in the vertical transport of very short-lived tracers (with a lifetime of 6 h) within the tropical troposphere. Peak convective outflow altitudes range from around 300 hPa to almost 100 hPa among the different models, and the upper tropospheric tracer mixing ratios differ by up to an order of magnitude. The timing of convective events is found to be different between the models, even among those which source their forcing data from the same NWP model (ECMWF). The differences are less pronounced for longer lived tracers, however they could have implications for modelling the halogen burden of the lowermost stratosphere through transport of species such as bromoform, or short-lived hydrocarbons into the lowermost stratosphere. The modelled tracer profiles are strongly influenced by the convective transport parameterisations, and different boundary layer mixing parameterisations also have a large impact on the modelled tracer profiles. Preferential locations for rapid transport from the surface into the upper troposphere are similar in all models, and are mostly concentrated over the western Pacific, the Maritime Continent and the Indian Ocean. In contrast, models do not indicate that upward transport is highest over western Africa.

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