Atmos. Chem. Phys. Discuss., 7, 18319-18360, 2007
www.atmos-chem-phys-discuss.net/7/18319/2007/
doi:10.5194/acpd-7-18319-2007
© Author(s) 2007. This work is licensed under the
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Morphology of the tropopause layer and lower stratosphere above a tropical cyclone: A case study on cyclone Davina (1999)
F. Cairo1,*, C. Buontempo1, A. R. MacKenzie2, C. Schiller3, C. M. Volk4, A. Adriani1,**, V. Mitev5, R. Matthey5, G. Di Donfrancesco6, A. Oulanovsky7, F. Ravegnani1, V. Yushkov7, M. Snels1, C. Cagnazzo8, and L. Stefanutti8,***
1Istituto di Scienze dell'Atmosfera e del Clima, CNR, Roma, Italy
2Environmental Science Department, Lancaster University, Lancaster, UK
3Institute for Stratospheric Research, Forschungszentrum Jülich GmbH, Jülich, Germany
4Institute for Atmosphere and Environment, J. W. Goethe University, Frankfurt, Germany
5Observatoire Cantonal Neuchatel, Neuchatel, Switzerland
6Ente per le Nuove Tecnologie, l'Energia e l'Ambiente, Frascati, Rome, Italy
7Central Aerological Observatory, Dolgoprudny, Russia
8Istituto Nazionale di Geofisica e Vulcanologia, Boulogne, Italy
*now at: United Kingdom Meteorological Office, Exeter, UK
**now at: Istituto di Fisica dello Spazio Interplanetario, INAF, Rome, Italy
***now at: Geophysica Gruppo Europeo di Interesse Economico, Florence, Italy

Abstract. During the APE-THESEO mission in the Indian Ocean the Myasishchev Design Bureau stratospheric research aircraft M55 Geophysica performed a flight over and within the inner core region of tropical cyclone Davina. Measurements of total water, water vapour, temperature, aerosol backscattering, ozone and tracers were made and are discussed here in comparison with the averages of those quantities acquired during the campaign time frame.

Temperature anomalies in the tropical tropopause layer (TTL), warmer than average in the lower part and colder than average in the upper TTL were observed. Ozone was strongly reduced compared to its average value, and thick cirrus decks were present up to the cold point, sometimes topped by a layer of very dry air. Evidence for meridional transport of trace gases in the stratosphere above the cyclone and the perturbed water distribution in the TTL is illustrated and discussed.


Citation: Cairo, F., Buontempo, C., MacKenzie, A. R., Schiller, C., Volk, C. M., Adriani, A., Mitev, V., Matthey, R., Di Donfrancesco, G., Oulanovsky, A., Ravegnani, F., Yushkov, V., Snels, M., Cagnazzo, C., and Stefanutti, L.: Morphology of the tropopause layer and lower stratosphere above a tropical cyclone: A case study on cyclone Davina (1999), Atmos. Chem. Phys. Discuss., 7, 18319-18360, doi:10.5194/acpd-7-18319-2007, 2007.
 
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