283 research outputs found

    Code to reproduce Ranjan et al. (2017), ApJ, submitted

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    <p> </p> <p>This repository holds all the code, auxiliary files, and intermediate files used in Ranjan, Wordsworth & Sasselov 2017b. Using this material, one can replicate every one of the figures used in our paper, as well as run models of one's own formulation.<br> <br> The anticipated use cases are:<br> 1. Testing/validating the findings of Ranjan, Wordsworth & Sasselov (2017)<br> 2. Using the Ranjan, Wordsworth & Sasselov radiative transfer model to compute UV surface fluence for user-defined atmospheres and surfaces.<br> <br> If making use of this code or the generated auxiliary files, please cite the descriptor paper:<br> Ranjan, S, Wordsworth, Robin D. and Sasselov, Dimitar D. "The Surface UV Environment on Prebiotic Planets Orbiting M-dwarfs: Implications for Prebiotic Chemistry & Need for Experimental Follow-Up". Submitted to the Astrophysical Journal (2017). arXiv: 1705.02350<br>  </p> <p>This version represents the state of the code at the time of paper acceptance.</p>If making use of this code or the generated auxiliary files, please cite the descriptor paper: Ranjan, S, Wordsworth, Robin D. and Sasselov, Dimitar D. "The Surface UV Environment on Prebiotic Planets Orbiting M-dwarfs: Implications for Prebiotic Chemistry & Need for Experimental Follow-Up". Submitted to the Astrophysical Journal (2017). arXiv: 1705.0235

    The mass of Kepler-93b and the composition of terrestrial planets

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    Kepler-93b is a 1.478 ± 0.019 R ⊕ planet with a 4.7 day period around a bright (V = 10.2), astroseismically characterized host star with a mass of 0.911 ± 0.033 M ☉ and a radius of 0.919 ± 0.011 R ☉. Based on 86 radial velocity observations obtained with the HARPS-N  spectrograph on the Telescopio Nazionale Galileo and 32 archival Keck/HIRES observations, we present a precise mass estimate of 4.02 ± 0.68 M ⊕. The corresponding high density of 6.88 ± 1.18 g cm–3 is consistent with a rocky composition of primarily iron and magnesium silicate. We compare Kepler-93b to other dense planets with well-constrained parameters and find that between 1 and 6 M ⊕, all dense planets including the Earth and Venus are well-described by the same fixed ratio of iron to magnesium silicate. There are as of yet no examples of such planets with masses >6 M ⊕. All known planets in this mass regime have lower densities requiring significant fractions of volatiles or H/He gas. We also constrain the mass and period of the outer companion in the Kepler-93 system from the long-term radial velocity trend and archival adaptive optics images. As the sample of dense planets with well-constrained masses and radii continues to grow, we will be able to test whether the fixed compositional model found for the seven dense planets considered in this paper extends to the full population of 1-6 M ⊕ planets.Peer reviewe

    The Kepler-454 system : A small, not-rocky inner planet, a Jovian world, and a distant companion

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    Kepler-454 (KOI-273) is a relatively bright (V = 11.69 mag), Sun-like starthat hosts a transiting planet candidate in a 10.6 d orbit. From spectroscopy, we estimate the stellar temperature to be 5687 +/- 50 K, its metallicity to be [m/H] = 0.32 +/- 0.08, and the projected rotational velocity to be v sin i 10 years and mass >12.1M_J . The twelve exoplanets with radii <2.7 R_Earth and precise mass measurements appear to fall into two populations, with those <1.6 R_Earth following an Earth-like composition curve and larger planets requiring a significant fraction of volatiles. With a density of 2.76 +/- 0.73 g cm-3, Kepler-454b lies near the mass transition between these two populations and requires the presence of volatiles and/or H/He gas.Peer reviewe

    A Precise Estimate of the Radius of HD 149026b

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    We present Spitzer 8 μm transit observations of the extrasolar planet system HD 149026b. At this wavelength, transit light curves are weakly affected by stellar limb-darkening, allowing for a simpler and more accurate determination of planetary parameters. We measure a planet-star radius ratio of R_p/R∗=0.05158±0.00077, and in combination with ground-based data and independent constraints on the stellar mass and radius, we derive an orbital inclination of i = 85°.4^(+0°.9)_(−0°.8) and a planet radius of 0.755 ± 0.040 R_J. These measurements further support models in which the planet is greatly enriched in heavy elements

    Characterizing the Atmospheres of Hot Jupiters: From Spectra to Multi-Color Maps

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    We present new observations of the emission spectrum of the hot Jupiter TrES-4 designed to test the theory that the presence of temperature inversions in the atmospheres of these planets are correlated with the amount of radiation received by the planet. Our observations reveal that TrES-4 has an emission spectrum similar to that of HD 209458b, which requires the presence of an inversion layer high in the atmosphere and water emission bands in order to explain the observed features, providing additional support for that theory. We also present new observations of the thermal phase curve of HD 189733b at 24 μm, which we combine with our previous observations at 8 μm to examine how circulation in this planet’s atmosphere varies as a function of depth. We discuss the relationship between the strength of the day-night circulation on both planets and their other observable properties, in particular their emission spectra
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