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@ARTICLE{Cairo:1470,
author = {Cairo, F. and Buontempo, C. and MacKenzie, A. R. and
Schiller, C. and Volk, M. and Adriani, A. and Mitev, V. and
Matthey, R. and Di Donfrancesco, G. and Qulanovsky, A. and
Ravegnani, F. and Rudakov, S. and Yushkov, V. and Snels, M.
and Cagnazzo, C. and Stefanutti, L.},
title = {{M}orphology of the tropopause layer and lower stratosphere
above a tropical cyclone: {A} case study on cyclone {D}avina
(1999)},
journal = {Atmospheric chemistry and physics},
volume = {8},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-1470},
pages = {3411 - 3426},
year = {2008},
note = {The APE-THESEO project was funded by the European
Commission under the contract ENVSCY97-0533. by the Italian
Space Agency (ASI), by the European Science Foundation and
by the German Ministry of Science and Education (BMBF). all
of whom gratefully acknowledged. Help in-kind was provided
by the UK Meteorological Office and the Directorate of Civil
Aviation of the Seychelles.A. R. MacKenzie gratefully
acknowledges NERC support under contracts GST/02/2210 and
NER/T/S/00977.This work also informs Activity 2 of the
SCOUT-O3 Integrated Project of the European Commission
(contract 505390-GOCE-CT-2004) as part of that project's
data mining and exploitation of existing data.ECMWF ERA-40
data used in this study have been obtained from the ECMWF
data server.},
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 was
observed and perturbed water distribution in the TTL was
documented. The paper discuss possible processes of
dehydration induced by the cirrus forming above the cyclone,
and change in the chemical tracer and water distribution in
the lower stratosphere 400-430 K due to meridional transport
from the mid-latitudes and link with Davina. Moreover it
compares the data prior and after the cyclone passage to
discuss its actual impact on the atmospheric chemistry and
thermodynamics.},
keywords = {J (WoSType)},
cin = {ICG-1},
ddc = {550},
cid = {I:(DE-Juel1)VDB790},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK406},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000257516800003},
doi = {10.5194/acp-8-3411-2008},
url = {https://juser.fz-juelich.de/record/1470},
}