598 citations
Counting papers with at most 25 authors, so collaboration author lists do not stand in for the people here.
- Centre National de la Recherche ScientifiqueFR51 papers
- Nantes UniversitéFR47 papers
- Jet Propulsion LaboratoryUS20 papers
- Université Paris CitéFR16 papers
- Observatoire de ParisFR15 papers
- Sorbonne UniversitéFR15 papers
- Université de NantesFR15 papers
- Laboratoire d’études spatiales et d’instrumentation en astrophysiqueFR14 papers
- Institut de physique du globe de ParisFR12 papers
- Astrophysique, Instrumentation et ModélisationFR10 papers
- Planetary Science InstituteUS10 papers
- Université Paris DiderotFR10 papers
5 papers · 1 filter
Water and the interior structure of terrestrial planets and icy bodies
Julien Monteux, Gregor J. Golabek, David C. Rubie +2
Water content and the internal evolution of terrestrial planets and icy bodies are closely linked. The distribution of water in planetary systems is controlled by the temperature s…
Transparency of 2 μm window of Titan's atmosphere
Pascal Rannou, Benoît Seignovert, Stéphane Le Mouélic +3
Titan's atmosphere is optically thick and hides the surface and the lower layers from the view at almost all wavelengths. However, because gaseous absorptions are spectrally select…
Role of the global water ocean on the evolution of Titan's primitive atmosphere
Nadejda Marounina, Olivier Grasset, Gabriel Tobie +1
During the accretion of Titan, impact heating may have been sufficient to allow the global melting of water ice and the release of volatile compounds, mainly constituted of CO2, CH…
Modelling climate diversity, tidal dynamics and the fate of volatiles on TRAPPIST-1 planets
Martin Turbet, Emeline Bolmont, Jeremy Leconte +6
TRAPPIST-1 planets are invaluable for the study of comparative planetary science outside our Solar System and possibly habitability. First, we derive from N-body simulations possib…
CO2 condensation is a serious limit to the deglaciation of Earth-like planets
Martin Turbet, Francois Forget, Jeremy Leconte +2
It is widely believed that the carbonate-silicate cycle is the main agent to trigger deglaciations by CO greenhouse warming on Earth and on Earth-like planets when they get in…