Detection of a Transit of the Super-Earth 55 Cancri E with Warm Spitzer .” A&A 533 (September 2011): A114

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Detection of a Transit of the Super-Earth 55 Cancri E with Warm Spitzer .” A&A 533 (September 2011): A114 Detection of a transit of the super- Earth 55Cancrie with warm Spitzer The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Demory, B.-O., M. Gillon, D. Deming, D. Valencia, S. Seager, B. Benneke, C. Lovis, et al. “ Detection of a Transit of the Super-Earth 55 Cancri e with Warm Spitzer .” A&A 533 (September 2011): A114. © ESO, 2011 As Published http://dx.doi.org/10.1051/0004-6361/201117178 Publisher EDP Sciences Version Final published version Citable link http://hdl.handle.net/1721.1/86109 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. A&A 533, A114 (2011) Astronomy DOI: 10.1051/0004-6361/201117178 & c ESO 2011 Astrophysics Detection of a transit of the super-Earth 55 Cancri e with warm Spitzer B.-O. Demory1, M. Gillon2,D.Deming3, D. Valencia1, S. Seager1,B.Benneke1,C.Lovis4, P. Cubillos5, J. Harrington5,K.B.Stevenson5, M. Mayor4,F.Pepe4,D.Queloz4, D. Ségransan4,andS.Udry4 1 Department of Earth, Atmospheric and Planetary Sciences, Department of Physics, Massachusetts Institute of Technology, 77 Massachusetts Ave., Cambridge, MA 02139, USA e-mail: [email protected] 2 Institut d’Astrophysique et de Géophysique, Université de Liège, Allée du 6 Août 17, Bat. B5C, 4000 Liège, Belgium 3 Department of Astronomy, University of Maryland, College Park, MD 20742-2421, USA 4 Observatoire de Genève, Université de Genève, 51 Chemin des Maillettes, 1290 Sauverny, Switzerland 5 Planetary Science Group, Department of Physics, University of Central Florida, Orlando, FL 32816-2385, USA Received 3 May 2011 / Accepted 31 July 2011 ABSTRACT We report on the detection of a transit of the super-Earth 55 Cnc e with warm Spitzer in IRAC’s 4.5 μm band. Our MCMC analysis includes an extensive modeling of the systematic effects affecting warm Spitzer photometry, and yields a transit depth of 410±63 ppm, +0.16 +0.58 which translates to a planetary radius of 2.08−0.17 R⊕ as measured in IRAC 4.5 μm channel. A planetary mass of 7.81−0.53 M⊕ is derived +1.31 −3 from an extensive set of radial-velocity data, yielding a mean planetary density of 4.78−1.20 gcm . Thanks to the brightness of its host star (V = 6, K = 4), 55 Cnc e is a unique target for the thorough characterization of a super-Earth orbiting around a solar-type star. Key words. binaries: eclipsing – planetary systems – stars: individual: 55 Cnc – techniques: photometric 1. Introduction (Borucki et al. 2010b), are similar to Neptune and GJ 436 b. Kepler-11 c (Lissauer et al. 2011) seems to be a smaller version Radial velocity (RV), microlensing and transit surveys have re- of Neptune, while HAT-P-26 b (Hartman et al. 2010)hasamuch vealed the existence in our Galaxy of a large population of plan- ± −3 −3 ∼ lower density (0.4 0.10 g cm vs. 1.64 g cm for Neptune) ets with a mass of a few to 20 Earth masses (Lovis et al. 2009; that is consistent with a significantly larger H/He fraction. The Sumi et al. 2010; Borucki et al. 2011). Based on their mass super-Earths CoRoT-7 b (Léger et al. 2009; Hatzes et al. 2010) (or minimum mass for RV planets), these planets are loosely ≤ and Kepler-10 b (Batalha et al. 2011) are probably massive rocky classified as “super-Earths” (Mp 10 M⊕) and “Neptunes” planets formed in the inner part of their protoplanetary disks. (Mp > 10 M⊕). This classification is based on the theoretical The super-Earth GJ 1214 b (Charbonneau et al. 2009) is still limit for gravitational capture of H/He, ∼10 M⊕ (e.g., Rafikov mysterious in nature. Its large radius (R = 2.44±0.21R⊕,Carter 2006), and thus implicitly assumes that Neptunes are predomi- p / et al. 2011) suggests a significant gaseous envelope that could nantly ice giants with a significant H He envelope, and that most originate from the outgassing of the rocky/icy surface material of super-Earths are massive terrestrial planets. Still, the diversity of a terrestrial planet or that could be of primordial origin, making it this planetary population is probably much larger than sketched a kind of “mini-Neptune” (Rogers & Seager 2010). Recent tran- by this simple division, as we can expect from the stochastic na- sit transmission spectrophotometric measurements for GJ 1214 b ture of planetary formation. seem to rule out a cloud-free atmosphere composed primarily of The first transit of one of these low-mass planets, GJ 436 b, hydrogen (Bean et al. 2010;Désertetal.2011), but more atmo- was detected in 2007 (Gillon et al. 2007). Thanks to its transit- spheric measurements are needed to determine the exact nature ing nature, the actual mass (Mp = 23.2 ± 0.8 M⊕) and radius = ± of its envelope. The case of GJ 1214 b shows nicely that under- (Rp 4.22 0.10 R⊕) of GJ 436 b could be accurately deter- standing the true nature of a low-mass exoplanet could require mined (Torres 2007), indicating for this “hot Neptune” a mass, not only precise measurements of its mass and radius, but also a radius and density indeed very similar to the ice giant plan- study of its atmospheric properties. ets Uranus and Neptune. More recently, several other transit- ing low-mass planets were detected. While many more planet Among all the low-mass transiting exoplanets detected so candidates detected by the Kepler mission are waiting for con- far, only GJ 1214 b and GJ 436 b, and to a lesser extent HAT- firmation (Borucki et al. 2011), the first confirmed low-mass P-11 b and HAT-P-26 b, orbit around stars small enough and transiting planets already show a large diversity. Some of these bright enough in the infrared to make possible a thorough at- planets, like HAT-P-11b (Bakos et al. 2010) and Kepler-4 b mospheric characterization with existing or future facilities like The photometric time series used in this work are only avail- JWST (e.g., Shabram et al. 2011). Improving our understand- able at the CDS via anonymous ftp to cdsarc.u-strasbg.fr ing of the low-mass planet population orbiting around solar-type (130.79.128.5) or via stars requires that such planets are detected in transit in front of http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/533/A114 much nearer/brighter host stars than the targets of surveys like Article published by EDP Sciences A114, page 1 of 7 A&A 533, A114 (2011) CoRoT (Barge et al. 2008)orKepler (Borucki et al. 2010a). This In addition to some basic parameters for the host star, the ori- is the main goal of two ambitious space mission projects in de- gin of the RVs used as input data, and a description of our warm velopment: PLATO (Catala et al. 2010) and TESS (Ricker et al. Spitzer observations, Table 1 provides the most relevant results 2010). Still, another and more straightforward possibility exists. of our MCMC analysis for 55 Cnc e. The large transit probabil- Doppler surveys target bright nearby stars, and they have now ity, ∼29%, and the very well constrained transit ephemeris (1σ detected enough nearby low-mass planets to make highly proba- error <1 h in 2011) of this super-Earth (Mp = 7.8±0.6 M⊕)made ble that a few of them transit their parent stars. This motivated us it an extremely interesting target for our transit search program. to search with Spitzer for transits of low-mass Doppler planets having the highest transit probability. In a previous paper (Gillon et al. 2010, hereafer G10), we described the reasons that have 3. Data analysis led us to conclude that Spitzer and its Infra-Red Array Camera (IRAC, Fazio et al. 2004) were the best instrumental choice for 3.1. Data description this transit search, and presented the results of our Spitzer cycle 55 Cnc was observed by Spitzer on 6 January 2011 from 9h41 5 program targeting HD 40307 b (Mayor et al. 2009). The rest of to 14h39 UT. The data consist of 5240 sets of 64 individ- our program consist of a cycle 6 DDT program (ID 60027) of ual subarray images obtained by the IRAC detector at 4.5 μm 100 h that targeted ten other low-mass planets. Spitzer’s cryogen with an integration time of 0.01s, and calibrated by the Spitzer was depleted at the end of cycle 5, and these observations were pipeline version S18.18.0. They are available on the Spitzer thus carried out in non-cryogenic mode (“warm Spitzer”). Heritage Archive database1 under the form of 5240 basic cal- The recent announcement of 55 Cnc e transits detection by ibrated data (BCD) files. We first converted fluxes from the the MOST satellite (Winn et al. 2011) motivated the publica- Spitzer units of specific intensity (MJy/sr) to photon counts, then tion of this paper. Our initial analysis of the warm Spitzer data performed aperture photometry on each subarray image with taken in last January concluded a transit detection but also that the IRAF/DAOPHOT2 software (Stetson 1987). We tested differ- several sources of instrumental effects needed to be fully charac- ent aperture radii and background annuli, the best result being terized before securing the detection. We only recently obtained obtained with an aperture radius of 3 pixels and a background a satisfactory instrumental model for warm Spitzer photometry, annulus extending from 11 to 15.5 pixels from the point-spread through a global analysis of calibration data and of all the ob- function (PSF) center.
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