Evaporation of Hot Jupiters Observations & Models Alfred Vidal-Madjar Jean-Michel Désert Guillaume Hébrard Alain Lecavelier (IAP, Paris) Roger Ferlet Institut d’Astrophysique Alain Lecavelier des Etangsde Paris Institut d’Astrophysique de Paris Evaporation of Hot-Jupiters Evaporation of Hot-Jupiters HD 209458b transit (Charbonneau et al. 2000) Evaporation of Hot-Jupiters Osiris Period = 3.524738 jours Mass = 0.69 ± 0.05 MJupiter Occultation = 1.58 % Radius = 1.35 ± 0.04 RJupiter Density = 0.35 ± 0.05 g/cm3 Evaporation of Hot-Jupiters Evaporation of Hot-Jupiters HD 209458b: Detection of the atmosphere in NaI (Charbonneau et al. 2002) 0.0232 ± 0.0057 % Evaporation of Hot-Jupiters -100 0 100 (km s-1) | | | HI Lyman α Flux (erg cm-2 s-1 Å-1) Before transit During transit Wavelength (Å) Evaporation of Hot-Jupiters End of transit Begin of transit Flux Ratio 15 ±4% (~ 4 σ) Time (hours) Evaporation of Hot-Jupiters Flux ratio 2 constraints: 15 ±4% -100 | 0 | 100 (km s-1) | Before transit Vidal-Madjar et al. Nature, 2003, 422 143 During transit Time (hours) Wavelength (A) • HD209458b (1.35 RJupiter = 96,500 km) → 1.6 % absorption Roche lobe (2.7 Rplanet = 3.6 RJupiter) → 10 % absorption Hydrogen: 15 % absorption → 3.2 Rplanet= 4.3 RJupiter = 300 000 km → Beyond the Roche lobe Î Hydrogen is escaping • Absorption width: Vred ≤ –100 km/s Vesc = 54 km/s → Beyond escape velocity Î Hydrogen is escaping ÎThe planet is evaporating Escape rate estimate How much for 15% absorption? Particle simulation • Radiation pressure: β = 0.7 • Star and planet gravity are taken into account • Free parameters: – HI volume density at the exobase: (at r ~ 0.5xRRoche : 2 x 105 cm-3) – Life time of HI: few hours (~ 6 h) → Escape rate > 1010 g/s Evaporation of Hot-Jupiters Escape rate estimate How much for 15% absorption? Evaporation of Hot-Jupiters Flux Ratio Escape rate > 1010 g/s Nature, => Taux d’évaporation > 1010 g s-1 Nature, 2003, 422, 143 Time (hours) Evaporation of Hot-Jupiters STIS G140L, low resolution observations Oct-Nov 2003 • Fig Lyman 1 α Evaporation of Hot-Jupiters Terrestrial airglow SiIII H I Lyman α OI C II Confirmation of the HI absorption HI Lyman α Out of transit • Fig 2a In transit Si III ~5% Wavelength (Å) Evaporation of Hot-Jupiters Detection of Carbon and Oxygen Out of Transit In Transit C II OI Vidal-Madjar et al. 2004 (astro-ph/0401457) ~ 13 % ~8% ± 4.5 % ± 3.5 % Wavelength (Å) Evaporation of Hot-Jupiters Consequences (Vidal-Madjar et al. 2004 ApJ 604, L69) • Oxygen and carbon are also present in the upper atmosphere of HD 209458b • They are carried away by the hydrogen flow at least with a velocity of about V > 10 km/s (~ sound speed) Î HYDRODYNAMIC ESCAPE (« BLOW-OFF ») Evaporation of Hot-Jupiters Other consequences • Presence of OI*, OI** Î n ≈ 106 cm -3 at RRoche • n = τ/(σ.L) (L~3 105 km) Î n ≈ 106 cm -3 at RRoche • Escape rate: ~ n.S.V where S is the surface of the Roche lobe (RRoche= 3.6 RJup) V is the H, O and C atoms velocity at the Roche lobe level (V > 10 km/s) Escape rate > 1.3 x 1010 g/s !!! Evaporation of Hot-Jupiters Models of the atmospheric escape Two important hypothesis: • Temperature of the upper atmosphere: Tup ≠ Teff Note that Tup(Jupiter) ~1000 K is not explained… • Tidal forces from the close-by parent star NB: Burrows & Lunine, Nature 378, 333 (1995) ÎEscape(H2+,H+,HI) = 1010 g s-1 Evaporation of Hot-Jupiters Le Roche Lobe de Roche Lobe • Lobe de Roche 1D Evaporation of Hot-Jupiters Escape through the exobase Evaporation of Hot-Jupiters Escape rate (Lecavelier et al., 2004, A&A, 418, L1) -1 -1)) Log escape rate (g s Log10 escape rate (g s 10 W Evaporation > 1010 g s-1 Evaporation of Hot-Jupiters ces r o f l a ith tid et n a l p d Isolate Temperature of the upper atmosphere Hypothesis: Heating = UV (Lyα) + EUV Cooling = Thermal Conduction + Collisional excitation of HI levels + Collisional ionisation + Escape Evaporation ofDistance Hot-Jupiters Orbital (AU) Log10 escape rate (g s-1) Escape Rate c es r o f l a id t h t i W et n a l p d Isolate Evaporation of Hot-Jupiters Planets‘ Life Time (log10 t/years) Planet Mass (M Jupiter) « Evaporation-modified » planets. Evaporation of Hot-Jupiters(AU) Orbital Distance
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