The thermal emission of the young and massive planet CoRoT-2b at 4.5 and 8 microns

TL;DR

This study measures the thermal emission of CoRoT-2b at 4.5 and 8 microns, analyzing its atmospheric properties, orbital eccentricity, and tidal evolution, revealing insights into its heat distribution, atmosphere, and future orbital fate.

Contribution

It provides new infrared measurements of CoRoT-2b's thermal emission and refines its physical and orbital parameters, including constraints on atmospheric structure and tidal Q values.

Findings

Measured occultation depths at 4.5 and 8 microns.

Indicates poor heat redistribution and possible absence of temperature inversion.

Models suggest the planet's large radius can be explained by tidal heating within 20 Myr.

Abstract

We report measurements of the thermal emission of the young and massive planet CoRoT-2b at 4.5 and 8 microns with the Spitzer Infrared Array Camera (IRAC). Our measured occultation depths are 0.510 +- 0.042 % and 0.41 +- 0.11 % at 4.5 and 8 microns, respectively. In addition to the CoRoT optical measurements, these planet/star flux ratios indicate a poor heat distribution to the night side of the planet and are in better agreement with an atmosphere free of temperature inversion layer. Still, the presence of such an inversion is not definitely ruled out by the observations and a larger wavelength coverage is required to remove the current ambiguity. Our global analysis of CoRoT, Spitzer and ground-based data confirms the large mass and size of the planet with slightly revised values (Mp = 3.47 +- 0.22 Mjup, Rp = 1.466 +- 0.044 Rjup). We find a small but significant offset in the timing of the occultation when compared to a purely circular orbital solution, leading to e cos(omega) = -0.00291 +- 0.00063 where e is the orbital eccentricity and omega is the argument of periastron. Constraining the age of the system to be at most of a few hundreds of Myr and assuming that the non-zero orbital eccentricity is not due to a third undetected body, we model the coupled orbital-tidal evolution of the system with various tidal Q values, core sizes and initial orbital parameters. For log(Q_s') = 5 - 6, our modelling is able to explain the large radius of CoRoT-2b if log(Q_p') <= 5.5 through a transient tidal circularization and corresponding planet tidal heating event. Under this model, the planet will reach its Roche limit within 20 Myr at most.