# Characterizing 51 Eri b from 1-5 $\mu$m: a partly-cloudy exoplanet

**Authors:** Abhijith Rajan, Julien Rameau, Robert J. De Rosa, Mark S. Marley,, James R. Graham, Bruce Macintosh, Christian Marois, Caroline Morley, Jennifer, Patience, Laurent Pueyo, Didier Saumon, Kimberly Ward-Duong, S. Mark Ammons,, Pauline Arriaga, Vanessa P. Bailey, Travis Barman, Joanna Bulger, Adam S., Burrows, Jeffrey Chilcote, Tara Cotten, Ian Czekala, Rene Doyon, Gaspard, Duch\^ene, Thomas M. Esposito, Michael P. Fitzgerald, Katherine B. Follette,, Jonathan J. Fortney, Stephen J. Goodsell, Alexandra Z. Greenbaum, Pascale, Hibon, Li-Wei Hung, Patrick Ingraham, Mara Johnson-Groh, Paul Kalas, Quinn, Konopacky, David Lafreni\`ere, James E. Larkin, J\'er\^ome Maire, Franck, Marchis, Stanimir Metchev, Maxwell A. Millar-Blanchaer, Katie M. Morzinski,, Eric L. Nielsen, Rebecca Oppenheimer, David Palmer, Rahul I. Patel, Marshall, Perrin, Lisa Poyneer, Fredrik T. Rantakyr\"o, Jean-Baptiste Ruffio, Dmitry, Savransky, Adam C. Schneider, Anand Sivaramakrishnan, Inseok Song, R\'emi, Soummer, Sandrine Thomas, Gautam Vasisht, J. Kent Wallace, Jason J. Wang,, Sloane Wiktorowicz, Schuyler Wolff

arXiv: 1705.03887 · 2017-06-28

## TL;DR

This study provides detailed spectro-photometric characterization of 51 Eri b across 1-5 μm, revealing its atmospheric properties, cloud features, and formation scenario, suggesting a partly-cloudy atmosphere and a cold-start formation via core accretion.

## Contribution

First comprehensive multi-wavelength spectro-photometry of 51 Eri b, combining new data with models to determine atmospheric composition, cloud structure, and formation history.

## Key findings

- Effective temperature between 605-737 K.
- Atmosphere requires patchy clouds for accurate modeling.
- Consistent with cold-start formation via core accretion.

## Abstract

We present spectro-photometry spanning 1-5 $\mu$m of 51 Eridani b, a 2-10 M$_\text{Jup}$ planet discovered by the Gemini Planet Imager Exoplanet Survey. In this study, we present new $K1$ (1.90-2.19 $\mu$m) and $K2$ (2.10-2.40 $\mu$m) spectra taken with the Gemini Planet Imager as well as an updated $L_P$ (3.76 $\mu$m) and new $M_S$ (4.67 $\mu$m) photometry from the NIRC2 Narrow camera. The new data were combined with $J$ (1.13-1.35 $\mu$m) and $H$ (1.50-1.80 $\mu$m) spectra from the discovery epoch with the goal of better characterizing the planet properties. 51 Eri b photometry is redder than field brown dwarfs as well as known young T-dwarfs with similar spectral type (between T4-T8) and we propose that 51 Eri b might be in the process of undergoing the transition from L-type to T-type. We used two complementary atmosphere model grids including either deep iron/silicate clouds or sulfide/salt clouds in the photosphere, spanning a range of cloud properties, including fully cloudy, cloud free and patchy/intermediate opacity clouds. Model fits suggest that 51 Eri b has an effective temperature ranging between 605-737 K, a solar metallicity, a surface gravity of $\log$(g) = 3.5-4.0 dex, and the atmosphere requires a patchy cloud atmosphere to model the SED. From the model atmospheres, we infer a luminosity for the planet of -5.83 to -5.93 ($\log L/L_{\odot}$), leaving 51 Eri b in the unique position as being one of the only directly imaged planet consistent with having formed via cold-start scenario. Comparisons of the planet SED against warm-start models indicates that the planet luminosity is best reproduced by a planet formed via core accretion with a core mass between 15 and 127 M$_{\oplus}$.

## Full text

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## Figures

28 figures with captions in the complete paper: https://tomesphere.com/paper/1705.03887/full.md

## References

146 references — full list in the complete paper: https://tomesphere.com/paper/1705.03887/full.md

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Source: https://tomesphere.com/paper/1705.03887