Letter
Nature 450, 641-645 (29 November 2007) | doi:10.1038/nature06140; Received 9 April 2007; Accepted 27 July 2007
A dynamic upper atmosphere of Venus as revealed by VIRTIS on Venus Express
P. Drossart1, G. Piccioni2, J. C. Gérard4, M. A. Lopez-Valverde5, A. Sanchez-Lavega6, L. Zasova7, R. Hueso6, F. W. Taylor8, B. Bézard1, A. Adriani3, F. Angrilli9, G. Arnold10, K. H. Baines11, G. Bellucci3, J. Benkhoff10, J. P. Bibring12, A. Blanco13, M. I. Blecka14, R. W. Carlson11, A. Coradini3, A. Di Lellis15, T. Encrenaz1, S. Erard1, S. Fonti13, V. Formisano3, T. Fouchet1, R. Garcia16, R. Haus10, J. Helbert10, N. I. Ignatiev7, P. Irwin8, Y. Langevin12, S. Lebonnois17, D. Luz1,19, L. Marinangeli18, V. Orofino13, A. V. Rodin7, M. C. Roos-Serote19, B. Saggin20, D. M. Stam21, D. Titov22, G. Visconti23, M. Zambelli2, C. Tsang8 & the VIRTIS-Venus Express Technical Team
- LESIA, Observatoire de Paris, CNRS, UPMC, Université Paris-Diderot, 5 place Jules Janssen, 92195 Meudon, France
- INAF-IASF,
- INAF-IFSI, 100 Via del Fosso del Cavaliere, 00133 Rome, Italy
- LPAP-Université de Liège, 5 Avenue de Cointe, B-4000 Liège, Belgium
- Instituto de Astrofisica de Andalucia (CSIC), 50 Camino Bajo de Huetor, 18008 Granada, Spain
- Universidad del Pais Vasco, Escuela Superior de Ingenieros, Física Aplicada I, C/Alda. Urquijo s/n 48013, Bilbao, Spain
- Space Research Institute (IKI), Profsouznaya 84/32, Moscow, Russia
- Atmospheric, Oceanic and Planetary Physics, Clarendon Laboratory, Parks Road, Oxford OX1 3PU, UK
- CISAS Università di Padova, 1 via Venezia, I-35131 Padova, Italy
-
German Aerospace Center (DLR), 2 Rutherfordstra
e, 12489 Berlin-Adlershof, Germany
- Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, California 91109, USA
- Institut d'Astrophysique Spatiale, batiment 121, Université de Paris-Sud, 91405 Orsay, France
- Dipartimento di Fisica, Università degli Studi di Lecce, Via Arnesano, 73100 Lecce, Italy
- Centrum Badan Kosmicznych Pan (CBK), 00716 Warszawa, Bartycka 18A, Poland
- AMDLSPACE, 33 Via Giovanni Angelini, 00149 Rome, Italy
- Dynamique Terrestre et Planétaire, CNRS UMR5562, Observatoire Midi Pyrénées, 31400 Toulouse, France
- Laboratoire de Météeorologie Dynamique, UPMC, 4 place Jussieu, 75252 Paris cedex 05, France
- Universita d'Annunzio, 42 Viale Pindaro, 65127 Pescara, Italy
- Lisbon Astronomical Observatory, Tapada da Ajuda, 1349-018 Lisbon, Portugal
- Politecnico di Milano, 26 Piazza Leonardo Da Vinci, 20133 Milano, Italy
- University of Amsterdam, 403 Kruislaan, 1098 SJ Amsterdam, The Netherlands
- Max-Planck Institute for Aeronomy, 2 Max-Planck-Strasse, 37191 Katlenburg-Lindau, Germany
- University of l'Aquila, Dipartimento di Fisica, 10 Via Vetoio, 67010 Coppito l'Aquila, Italy
- INAF-IFSI, 00133 Rome, Italy.
- Galileo Avionica, Florence, 50013, Italy.
- DLR, 12489 Berlin, Germany.
- Università di Padova, 35131, Italy.
- INAF-IASF, 00133 Rome, Italy.
- IAS Orsay, 91405, France.
- LESIA, Observatoire de Paris, France.
- ASI Rome, 00198, Italy.
- Techno System Developments, Naples, 80078, Italy.
- Kayser Threde, Munich, 81379, Germany.
Correspondence to: P. Drossart1 Correspondence and requests for materials should be addressed to P.D. (Email: pierre.drossart@obspm.fr).
The upper atmosphere of a planet is a transition region in which energy is transferred between the deeper atmosphere and outer space. Molecular emissions from the upper atmosphere (90–120 km altitude) of Venus can be used to investigate the energetics and to trace the circulation of this hitherto little-studied region. Previous spacecraft1 and ground-based2, 3, 4 observations of infrared emission from CO2, O2 and NO have established that photochemical and dynamic activity controls the structure of the upper atmosphere of Venus. These data, however, have left unresolved the precise altitude of the emission1 owing to a lack of data and of an adequate observing geometry5, 6. Here we report measurements of day-side CO2 non-local thermodynamic equilibrium emission at 4.3
m, extending from 90 to 120 km altitude, and of night-side O2 emission extending from 95 to 100 km. The CO2 emission peak occurs at
115 km and varies with solar zenith angle over a range of
10 km. This confirms previous modelling7, and permits the beginning of a systematic study of the variability of the emission. The O2 peak emission happens at 96 km
1 km, which is consistent with three-body recombination of oxygen atoms transported from the day side by a global thermospheric sub-solar to anti-solar circulation, as previously predicted8.
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