- Rajan, Abhijith;
- Rameau, Julien;
- De Rosa, Robert J;
- Marley, Mark S;
- Graham, James R;
- Macintosh, Bruce;
- Marois, Christian;
- Morley, Caroline;
- Patience, Jennifer;
- Pueyo, Laurent;
- Saumon, Didier;
- Ward-Duong, Kimberly;
- Ammons, S Mark;
- Arriaga, Pauline;
- Bailey, Vanessa P;
- Barman, Travis;
- Bulger, Joanna;
- Burrows, Adam S;
- Chilcote, Jeffrey;
- Cotten, Tara;
- Czekala, Ian;
- Doyon, Rene;
- Duchêne, Gaspard;
- Esposito, Thomas M;
- Fitzgerald, Michael P;
- Follette, Katherine B;
- Fortney, Jonathan J;
- Goodsell, Stephen J;
- Greenbaum, Alexandra Z;
- Hibon, Pascale;
- Hung, Li-Wei;
- Ingraham, Patrick;
- Johnson-Groh, Mara;
- Kalas, Paul;
- Konopacky, Quinn;
- Lafrenière, David;
- Larkin, James E;
- Maire, Jérôme;
- Marchis, Franck;
- Metchev, Stanimir;
- Millar-Blanchaer, Maxwell A;
- Morzinski, Katie M;
- Nielsen, Eric L;
- Oppenheimer, Rebecca;
- Palmer, David;
- Patel, Rahul I;
- Perrin, Marshall;
- Poyneer, Lisa;
- Rantakyrö, Fredrik T;
- Ruffio, Jean-Baptiste;
- Savransky, Dmitry;
- Schneider, Adam C;
- Sivaramakrishnan, Anand;
- Song, Inseok;
- Soummer, Rémi;
- Thomas, Sandrine;
- Vasisht, Gautam;
- Wallace, J Kent;
- Wang, Jason J;
- Wiktorowicz, Sloane;
- Wolff, Schuyler
We present spectrophotometry spanning 1-5 μm of 51 Eridani b, a 2-10 planet discovered by the Gemini Planet Imager Exoplanet Survey. In this study, we present new K1 (1.90-2.19 μm) and K2 (2.10-2.40 μm) spectra taken with the Gemini Planet Imager as well as an updated L P (3.76 μm) and new M S (4.67 μm) photometry from the NIRC2 Narrow camera. The new data were combined with J (1.13-1.35 μm) and H (1.50-1.80 μm) spectra from the discovery epoch with the goal of better characterizing the planet properties. The 51 Eri b photometry is redder than field brown dwarfs as well as known young T-dwarfs with similar spectral type (between T4 and 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. The model fits suggest that 51 Eri b has an effective temperature ranging between 605 and 737 K, a solar metallicity, and a surface gravity of log(g) = 3.5-4.0 dex, and the atmosphere requires a patchy cloud atmosphere to model the spectral energy distribution (SED). From the model atmospheres, we infer a luminosity for the planet of -5.83 to -5.93 (logL/L⊙), leaving 51 Eri b in the unique position of being one of the only directly imaged planets consistent with having formed via a cold-start scenario. Comparisons of the planet SED against warm-start models indicate that the planet luminosity is best reproduced by a planet formed via core accretion with a core mass between 15 and 127 M⊕.