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The 2010 European Venus Explorer (EVE) mission proposal
Authors:Colin Frank Wilson  Eric Chassefière  Emmanuel Hinglais  Kevin H Baines  Tibor S Balint  Jean-Jacques Berthelier  Jacques Blamont  Georges Durry  Csaba S Ferencz  Robert E Grimm  Takeshi Imamura  Jean-Luc Josset  Fran?ois Leblanc  Sebastien Lebonnois  Johannes J Leitner  Sanjay S Limaye  Bernard Marty  Ernesto Palomba  Sergei V Pogrebenko  Scot C R Rafkin  Dean L Talboys  Rainer Wieler  Liudmila V Zasova  Cyrill Szopa
Institution:1. Department of Physics, Oxford University, Oxford, UK
2. IDES, Université de Paris-Sud 11, Orsay, France
3. CNES (PASO), Toulouse, France
4. NASA/JPL, Pasadena, CA, USA
5. SSEC, University of Wisconsin, Madison, WI, USA
6. LATMOS, IPSL, CNRS, Guyancourt, France
7. CNES, Paris, France
8. Université de Reims, Reims, France
9. Space Research Group, E?tv?s University, Budapest, Hungary
10. Southwest Research Institute, Boulder, CO, USA
11. ISAS/JAXA, Sagamihara, Japan
12. Space Exploration Institute, Neuchatel, Switzerland
13. Laboratoire de Météorologie Dynamique, IPSL, UPMC, CNRS, Paris, France
14. Institute of Astronomy, University of Vienna, Vienna, Austria
15. CRPG, Ecole Nationale Supérieure de Géologie, Nancy, France
16. INAF-IFSI, Rome, Italy
17. Joint Institute for VLBI in Europe, Dwingeloo, The Netherlands
18. Space Research Centre, University of Leicester, Leicester, UK
19. Institute of Geochemistry and Petrology, ETH, Zürich, Switzerland
20. Space Research Institute, Moscow, Russia
Abstract:The European Venus Explorer (EVE) mission described in this paper was proposed in December 2010 to ESA as an ‘M-class’ mission under the Cosmic Vision programme. It consists of a single balloon platform floating in the middle of the main convective cloud layer of Venus at an altitude of 55?km, where temperatures and pressures are benign (~25°C and ~0.5 bar). The balloon float lifetime would be at least 10 Earth days, long enough to guarantee at least one full circumnavigation of the planet. This offers an ideal platform for the two main science goals of the mission: study of the current climate through detailed characterization of cloud-level atmosphere, and investigation of the formation and evolution of Venus, through careful measurement of noble gas isotopic abundances. These investigations would provide key data for comparative planetology of terrestrial planets in our solar system and beyond.
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