Issue |
A&A
Volume 533, September 2011
|
|
---|---|---|
Article Number | A136 | |
Number of page(s) | 8 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201016237 | |
Published online | 16 September 2011 |
Venus transit 2004: Illustrating the capability of exoplanet transmission spectroscopy
1
CNRS, UMR 5804, Laboratoire d’Astrophysique de Bordeaux, 2 rue de
l’Observatoire,
BP 89,
33271
Floirac Cedex,
France
e-mail: pascal.hedelt@obs.u-bordeaux1.fr
2
Université de Bordeaux, Observatoire Aquitain des Sciences de
l’Univers, 2 rue de l’Observatoire, BP 89, 33271
Floirac Cedex,
France
3
Observatoire Astronomique de l’Université de Genève,
51 chemin des
Maillettes, 1290
Sauverny,
Switzerland
4
Las Cumbres Observatory Global Telescope,
6720 Cortona Dr. Ste.
102, Goleta,
CA
93117,
USA
5
Instituto de Astrofisica de Canarias, 38200 La Laguna, Tenerife, Spain
6
Institut für Planetenforschung, Deutsches Zentrum für Luft- und Raumfahrt, Rutherfordstr.
2, 12489
Berlin,
Germany
7
Zentrum für Astronomie und Astrophysik, Technische Universität
Berlin, Hardenbergstr.
36, 10623
Berlin,
Germany
8
Kiepenheuer-Institut für Sonnenphysik,
Schöneckstr. 6,
79104
Freiburg,
Germany
9
Institut für Methodik der Fernerkundung,
Deutsches Zentrum für Luft- und
Raumfahrt, 82234
Oberpfaffenhofen-Wessling,
Germany
Received:
30
November
2010
Accepted:
1
August
2011
The transit of Venus in 2004 offered the rare possibility to remotely sense a well-known planetary atmosphere using ground-based absorption spectroscopy. Transmission spectra of Venus’ atmosphere were obtained in the near infrared using the Vacuum Tower Telescope (VTT) in Tenerife. Since the instrument was designed to measure the very bright photosphere of the Sun, extracting Venus’ atmosphere was challenging. We were able to identify CO2 absorption lines in the upper Venus atmosphere. Moreover, the relative abundance of the three most abundant CO2 isotopologues could be determined. The observations resolved Venus’ limb, showing Doppler-shifted absorption lines that are probably caused by high-altitude winds. We demonstrate the utility of ground-based measurements in analyzing the atmospheric constituents of a terrestrial planet atmosphere using methods that might be applied in future to terrestrial extrasolar planets.
Key words: planets and satellites: atmospheres / planets and satellites: composition / planets and satellites: detection / radiative transfer / techniques: spectroscopic
© ESO, 2011
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