TY - JOUR
T1 - Warm spitzer photometry of the transiting exoplanets CoRoT-1 and CoRoT-2 at secondary eclipse
AU - Deming, Drake
AU - Knutson, Heather
AU - Agol, Eric
AU - Desert, Jean Michel
AU - Burrows, Adam
AU - Fortney, Jonathan J.
AU - Charbonneau, David
AU - Cowan, Nicolas B.
AU - Laughlin, Gregory
AU - Langton, Jonathan
AU - Showman, Adam P.
AU - Lewis, Nikole K.
PY - 2011/1/10
Y1 - 2011/1/10
N2 - We measure secondary eclipses of the hot giant exoplanets CoRoT-1 at 3.6 and 4.5ìm, and CoRoT-2 at 3.6μm, both using Warm Spitzer. We find that the Warm Spitzer mission is working very well for exoplanet science. For consistency of our analysis we also re-analyze archival cryogenic Spitzer data for secondary eclipses of CoRoT-2 at 4.5 and 8μm.We compare the total data for both planets, including optical eclipse measurements by the CoRoT mission, and ground-based eclipse measurements at 2μm, to existingmodels. Both planets exhibit stronger eclipses at 4.5 than at 3.6μm, which is often indicative of an atmospheric temperature inversion. The spectrum of CoRoT-1 is best reproduced by a 2460 K blackbody, due either to a high altitude layer that strongly absorbs stellar irradiance, or an isothermal region in the planetary atmosphere. The spectrum of CoRoT-2 is unusual because the 8μm contrast is anomalously low. Non-inverted atmospheres could potentially produce the CoRoT-2 spectrum if the planet exhibits line emission from CO at 4.5μm, caused by tidal-induced mass loss. However, the viability of that hypothesis is questionable because the emitting region cannot be more than about 30% larger than the planet's transit radius, based on the ingress and egress times at eclipse. An alternative possibility to account for the spectrum of CoRoT-2 is an additional opacity source that acts strongly at wavelengths less than 5μm, heating the upper atmosphere while allowing the deeper atmosphere seen at 8μm to remain cooler. We obtain a similar result as Gillon et al. for the phase of the secondary eclipse of CoRoT-2, implying an eccentric orbit with e cos(ù) =.0.0030 ± 0.0004.
AB - We measure secondary eclipses of the hot giant exoplanets CoRoT-1 at 3.6 and 4.5ìm, and CoRoT-2 at 3.6μm, both using Warm Spitzer. We find that the Warm Spitzer mission is working very well for exoplanet science. For consistency of our analysis we also re-analyze archival cryogenic Spitzer data for secondary eclipses of CoRoT-2 at 4.5 and 8μm.We compare the total data for both planets, including optical eclipse measurements by the CoRoT mission, and ground-based eclipse measurements at 2μm, to existingmodels. Both planets exhibit stronger eclipses at 4.5 than at 3.6μm, which is often indicative of an atmospheric temperature inversion. The spectrum of CoRoT-1 is best reproduced by a 2460 K blackbody, due either to a high altitude layer that strongly absorbs stellar irradiance, or an isothermal region in the planetary atmosphere. The spectrum of CoRoT-2 is unusual because the 8μm contrast is anomalously low. Non-inverted atmospheres could potentially produce the CoRoT-2 spectrum if the planet exhibits line emission from CO at 4.5μm, caused by tidal-induced mass loss. However, the viability of that hypothesis is questionable because the emitting region cannot be more than about 30% larger than the planet's transit radius, based on the ingress and egress times at eclipse. An alternative possibility to account for the spectrum of CoRoT-2 is an additional opacity source that acts strongly at wavelengths less than 5μm, heating the upper atmosphere while allowing the deeper atmosphere seen at 8μm to remain cooler. We obtain a similar result as Gillon et al. for the phase of the secondary eclipse of CoRoT-2, implying an eccentric orbit with e cos(ù) =.0.0030 ± 0.0004.
KW - Eclipses
KW - Planetary systems
KW - Techniques: photometric
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U2 - 10.1088/0004-637X/726/2/95
DO - 10.1088/0004-637X/726/2/95
M3 - Article
AN - SCOPUS:84891238633
SN - 0004-637X
VL - 726
JO - Astrophysical Journal
JF - Astrophysical Journal
IS - 2
ER -