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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/39RS9SS
Repositorydpi.inpe.br/plutao/2011/06.11.13.35.48
Last Update2011:11.03.19.02.35 (UTC) administrator
Metadata Repositorydpi.inpe.br/plutao/2011/06.11.13.35.49
Metadata Last Update2021:07.28.23.06.02 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.5194/acpd-11-16147-2011
ISSN1680-7375
Labellattes: 9873289111461387 9 MarécalKMCLAADFLRR:2011:ImDeCo
Citation KeyMarécalKMCLAADFLRR:2011:ImDeCo
TitleImpact of deep convection on the tropical tropopause layer composition in Equatorial Brazil
Year2011
Access Date2024, May 11
Secondary TypePRE PI
Number of Files1
Size6209 KiB
2. Context
Author 1 Marécal, V.
 2 Krysztofiak, G.
 3 Mébarki, Y.
 4 Catoire, V.
 5 Lott, F.
 6 Attié, J. -L.
 7 Arteta, J.
 8 Deeter, M. N.
 9 Freitas, Saulo Ribeiro de
10 Longo, K. M.
11 Renard, J. -B.
12 Robert, C.
Resume Identifier 1
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 9 8JMKD3MGP5W/3C9JJ7M
Group 1
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 9 DMD-CPT-INPE-MCT-BR
10 DGE-CEA-INPE-MCT-BR
Affiliation 1 Centre National de Recherche M´ et ´eorologique-Groupe d’ ´etude de l’Atmosph`ere
 2 Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS and Universit ´e of Orl ´eans, UMR 6115, Orl ´eans, France
 3 Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS and Universit ´e of Orl ´eans, UMR 6115, Orl ´eans, France
 4 Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS and Universit ´e of Orl ´eans, UMR 6115, Orl ´eans, France
 5 Laboratoire de M´ et ´eorologie Dynamique, Ecole Normale Sup´ erieure and CNRS, UMR 8539, Paris, France
 6 4Laboratoire d’A´ erologie, Universit ´e de Toulouse and CNRS, UMR 5560, Toulouse, France
 7 Centre National de Recherche M´ et ´eorologique-Groupe d’ ´etude de l’Atmosphere
 8 National Center for Atmospheric Research, Atmospheric Chemistry Division, Boulder, USA
 9 Instituto Nacional de Pesquisas Espaciais (INPE)
10 Instituto Nacional de Pesquisas Espaciais (INPE)
11 Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS and Universit ´e of Orl ´eans, UMR 6115, Orl ´eans, France
12 Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS and Universit ´e of Orl ´eans, UMR 6115, Orl ´eans, France
Author e-Mail Address 1
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 9 saulo.freitas@cptec.inpe.br
e-Mail Addresssaulo.freitas@cptec.inpe.br
JournalAtmospheric Chemistry and Physics Discussion
Volume11
Pages16147-16183
Secondary MarkB4_ENGENHARIAS_II B3_GEOCIÊNCIAS B2_INTERDISCIPLINAR
History (UTC)2011-06-11 17:43:47 :: lattes -> marciana :: 2011
2011-06-20 18:19:40 :: marciana -> administrator :: 2011
2011-07-18 13:22:28 :: administrator -> valdirene :: 2011
2011-11-03 19:02:35 :: valdirene -> administrator :: 2011
2012-07-25 15:51:13 :: administrator -> banon :: 2011
2012-09-21 14:41:38 :: banon -> administrator :: 2011
2012-10-19 20:25:41 :: administrator -> valdirene :: 2011
2013-01-17 12:12:23 :: valdirene -> administrator :: 2011
2021-07-28 23:06:02 :: administrator -> valdirene :: 2011
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractThis paper documents measurements of carbon monoxide (CO), ozone (O3) and temperature in the tropical tropopause layer over Equatorial Brazil for the first time. These measurements were sampled by the balloon-borne instrument SPIRALE (Spectro- 5 scopie Infa-Rouge par Absorption de Lasers Embarque´s) in June 2005 and in June 2008, both at the transition period from wet to dry season. The height of the Tropical Tropopause Layer (TTL) top and bottom determined from the chemical species profiles are similar for the two flights. Nevertheless the measured profiles of ozone and CO are different in their volume mixing ratio and shape. The larger CO values measured 10 in the TTL in 2005 can be linked to a more intense biomass burning activity in 2005 than in 2008. We also show that both measured profiles are influenced by convection but in different ways leading to different shapes. The CO profile in 2005 is characterised by a generally smooth decrease in the TTL from tropospheric to stratospheric conditions, except for two layers of enhanced CO around 14.2 (>100 parts per billion 15 by volume=ppbv) and 16.3 km altitude (>85 ppbv). Backward trajectories indicate that these layers come from the vertical transport by remote deep convection occurring 2 and 3 days prior to the flight, respectively. This shows that the transition period from wet to dry season is favourable for the transport of significant amounts of CO in the TTL, sometimes above the level of zero radiative heating, because of increasing biomass 20 burning together with decaying but still important convective activity. In 2008 we focus our analysis on a 1 km deep layer, between 17 and 18 km, where both the temperature and the ozone profiles are uniform in the vertical, corresponding to a layer of well-mixed air. We show that this unusual behaviour is indirectly related to the interaction between convection and the Quasi-Biennial Oscillation (QBO), through vertically propagating 25 gravity waves. Quasi-stationary gravity waves are likely to be produced by convective systems and certainly break in the intense wind shear that imposes the QBO at these altitudes. This conclusion is supported by the fact that the 1618km layer is devoid of ice particles (hence the mixing is not convective) and from backward trajectories that point towards a convective region as the origin of the air masses in this layer.
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data URLhttp://urlib.net/ibi/J8LNKAN8RW/39RS9SS
zipped data URLhttp://urlib.net/zip/J8LNKAN8RW/39RS9SS
Languageen
Target FileMarecal_Impact of deep.pdf
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/43SKC35
DisseminationWEBSCI; PORTALCAPES.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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