Morphology of the tropopause layer and lower stratosphere above a tropical cyclone: A case study on cyclone Davina (1999)

F. Cairo (1) , C. Buontempo (1) , A. R. Mackenzie (2) , C. Schiller (3) , C. M. Volk (4) , A. Adriani (1) , V. Mitev (5) , R. Matthey (5) , G. Di Donfrancesco (6) , A. Oulanovsky (7) , F. Ravegnani (1) , V. Yushkov (7) , M. Snels (1) , C. Cagnazzo (8) , L. Stefanutti (8)

1 ISAC - Istituto di Scienze dell'Atmosfera e del Clima
2 Department of Environmental Science [Lancaster]
3 Institute for Stratospheric Research
4 Institute for Atmosphere and Environment
5 OCN - Observatoire Cantonal de Neuchâtel
6 Ente per le Nuove Tecnologie
7 CAO - Central Aerological Observatory
8 Istituto Nazionale di Geofisica e Vulcanologia

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.

Domaines: Océan, Atmosphère

F. Cairo, C. Buontempo, A. R. Mackenzie, C. Schiller, C. M. Volk, et al.. Morphology of the tropopause layer and lower stratosphere above a tropical cyclone: A case study on cyclone Davina (1999). Atmospheric Chemistry and Physics Discussions, 2007, 7 (6), pp.18319-18360. ⟨hal-00303220⟩