ground-based exoplanet atmospheres characterization: progress since the 2009 breakthrough
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Ground-based Exoplanet Atmospheres Characterization: Progress Since the 2009 Breakthrough. Mercedes L ópez-Morales Carnegie Institution of Washington. Hubble Fellows Symposium 2010. - PowerPoint PPT PresentationTRANSCRIPT
Ground-based Exoplanet Atmospheres Characterization:
Progress Since the 2009 Breakthrough
Mercedes López-MoralesCarnegie Institution of Washington
Hubble Fellows Symposium 2010
Collaborators: Daniel Apai (STScI), David Sing (Exeter, UK), Sara Seager (MIT), Justin Rogers (JHU/CIW), Adam Burrows (Princeton), Jeff Coughlin (NMSU), Michael Sterzik (ESO)
Nov 1995: discovery of51 Pegasi b by Mayor &Queloz; confirmed by Marcy & Butler on December 1995.
Star’s Spectral Type: G2VMp sin i = 0.468 Mjup; P = 4.23077 day
March 2010: more than 400 discovered.
Finding Earth-mass planets
Atmospheric characterization
How can we measure an exoplanet’s atmosphere?
Direct Imaging
Transits
Primary Eclipse
Secondary Eclipse
Primary eclipse (~ 1% of total light)
Secondary eclipse(< 0.1 - 0.2% of total light)
Real data for HD 189733b (Knutson et al. 2007)
Primary Eclipses: Transmission Spectra
Secondary Eclipses: Emission spectra
Showman & Guillot 2002López-Morales & Seager 2007
;
(Tinetti et al. 2007)Exoplanet atm
osphere’s spectrum
Sodium (HD 209458b)(Charbonneau et al. 2002)
HST/STIS
Secondary @ 24 μm (HD 209458b)(Deming et al. 2005)
Spitzer/MIPS
First exoplanet atmosphere detections
Results from the ground
6.5-m Magellan
3.5-m APO
8.0-m VLT
4.2-m WHT
+ HET, Subaru, IRTF
Primary Eclipses: Transmission Spectra
Ground-based detection of Sodium in HD 189733b (Redfield et al. 2008)
> 3 detection
Ground-based confirmation of Sodium in HD 209458b (Snellen et al. 2008)
= 3.0 Å Depth = 0.056%
= 0.75 Å Depth = 0.135%
> 5 detection
Secondary Eclipse: Thermal + Reflected Emission
Ogle-TR-56b(Sing & López-Morales 2009) (de Mooij & Snellen 2009)TrES-3b
z’-band (0.9 m) Depth = 0.036% (3.6)
K-band (2.2 m) Depth = 0.241% (~6)
8-m VLT + 6.5-m Magellan
4.5-m WHT
Tz’ = 2718 ± 120 KAB ~ 0.0 (no-clouds)f ~ 0.56 (low winds)
Thermal Inversion
TK = 2040 ± 185 KAB ~ 0.0 (no-clouds)f ~ 2/3 (low winds)
Thermal Inversion
Secondary Eclipse: Thermal + Reflected EmissionCoRoT-1b(Gillon et al. 2009)
HJD (days)NB2090 (2.09 m) Depth = 0.278% (~5) Ks-band (2.2 m) Depth = 0.324% (7.7)
8-m VLT 3.5-m APO
(Rogers et al. 2009)
(Rogers et al. 2009)
Tz’ = 2460 (+80/-160) KAB ~ 0.00 (+0.08/-0.00)f ~ 0.52 (+0.07/-0.08)
Heat
Red
istrib
utio
n Fa
ctor
(f)
Bond Albedo AB
Bond Albedo AB
Flux
Fν
[ Jy
]
Prominent dT between day and night sides
** Atmospheric models generated by co-author A. Burrows
Secondary Eclipse: Thermal + Reflected Emission
(Rogers et al. 2009)
- Models for different f (Pn) and extra-absorber opacities κe
-The extra-absorber is at Pheight = 1 mbar
- Models reproduce emission in the optical, but near-IR emission is twice larger than predicted.
- Attempt to reproduce the near- IR emission using Pn = 0.1 and extra-absorber with κe = 0.05 cm2g-1 at Pheight = 10 mbar
- Models still cannot reproduce near-IR emission.
WASP-12b(López-Morales et al. 2010)
Secondary Eclipse: Thermal + Reflected Emission
z’-band (0.9 m) Depth = 0.082% (5.4)
-The measured z’-band depth fits well BB models and atmospheric models with and w/o thermal inversions. Need more λ’s.
Eclipse’s central phase = 0.5100 ± 0.0022
e |cosω| = 0.0156 ± 0.0035e = 0.057 ± 0.013 (assuming ω = 74°)
(Hebb et al. 2009)
3.5-m APO
Secondary Eclipse: Thermal + Reflected EmissionWASP-19b (Anderson et al. 2010) (Gibson et al. 2010)
H-band (1.62 m) Depth = 0.259% (~5.7) NB2090 (2.09 m) Depth = 0.366% (~5)
8-m VLT 8-m VLT
-The hottest possible models cannot reproduce the H-band depth.- The 2.09 m atmosphere is slightly better reproduced, but still ~ 1-sigma brighter than the models.
HD 189733b(Swain et al. 2010)
Depth > 1.0%(>10)
Secondary Eclipse: Spectro-photometry
- Day-side observations between 2.0 – 2.4 μm and 3.0 – 4.1 μm
- Spectro-photometry with R= 470
Eclipse depths agree when compared to available HST and Spitzer data.
Secondary Eclipse: SpectrophotometryHD 189733b(Swain et al. 2010)
LTE models OK
Non-LTE?
Conclusions• We have now observed the atmospheres of 7 Hot Jupiters from the ground:
transmission NaI D signals of 2 planets in 2008 emission photometry of 5 planets in 2009-2010 spectro-photometry of 1 exoplanet in 2010• For CoRoT-1b we can now assure that AB ~ 0 and the
planet does have a much hotter day-side than night-side (thermal inversion layer)
hints of the same behavior in other planets, but need more color measurements
• Previously untested models seem to have problems reproducing the emission of some hot Jupiters in the near-IR. Non-LTE??• Observational improvements in the next few years will be aimed at studying the atmospheres of the first transiting exo-Earths