Combined Transcripts: Exoplanets Course
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Echo Exoplanet Characterisation Observatory
Exp Astron (2012) 34:311–353 DOI 10.1007/s10686-012-9303-4 ORIGINAL ARTICLE EChO Exoplanet characterisation observatory G. Tinetti · J. P. Beaulieu · T. Henning · M. Meyer · G. Micela · I. Ribas · D. Stam · M. Swain · O. Krause · M. Ollivier · E. Pace · B. Swinyard · A. Aylward · R. van Boekel · A. Coradini · T. Encrenaz · I. Snellen · M. R. Zapatero-Osorio · J. Bouwman · J. Y-K. Cho · V. Coudé du Foresto · T. Guillot · M. Lopez-Morales · I. Mueller-Wodarg · E. Palle · F. Selsis · A. Sozzetti · P. A. R. Ade · N. Achilleos · A. Adriani · C. B. Agnor · C. Afonso · C. Allende Prieto · G. Bakos · R. J. Barber · M. Barlow · V. Batista · P. Bernath · B. Bézard · P. Bordé · L. R. Brown · A. Cassan · C. Cavarroc · A. Ciaravella · C. Cockell · A. Coustenis · C. Danielski · L. Decin · R. De Kok · O. Demangeon · P. Deroo · P. Doel · P. Drossart · L. N. Fletcher · M. Focardi · F. Forget · S. Fossey · P. Fouqué · J. Frith · M. Galand · P. Gaulme · J. I. González Hernández · O. Grasset · D. Grassi · J. L. Grenfell · M. J. Griffin · C. A. Griffith · U. Grözinger · M. Guedel · P. Guio · O. Hainaut · R. Hargreaves · P. H. Hauschildt · K. Heng · D. Heyrovsky · R. Hueso · P. Irwin · L. Kaltenegger · P. Kervella · D. Kipping · T. T. Koskinen · G. Kovács · A. La Barbera · H. Lammer · E. Lellouch · G. Leto · M. A. Lopez Valverde · M. Lopez-Puertas · C. Lovis · A. Maggio · J. P. Maillard · J. Maldonado Prado · J. B. Marquette · F. J. Martin-Torres · P. Maxted · S. Miller · S. Molinari · D. Montes · A. Moro-Martin · J. I. Moses · O. Mousis · N. Nguyen Tuong · R. -
In-System'' Fission-Events: an Insight Into Puzzles of Exoplanets and Stars?
universe Review “In-System” Fission-Events: An Insight into Puzzles of Exoplanets and Stars? Elizabeth P. Tito 1,* and Vadim I. Pavlov 2,* 1 Scientific Advisory Group, Pasadena, CA 91125, USA 2 Faculté des Sciences et Technologies, Université de Lille, F-59000 Lille, France * Correspondence: [email protected] (E.P.T.); [email protected] (V.I.P.) Abstract: In expansion of our recent proposal that the solar system’s evolution occurred in two stages—during the first stage, the gaseous giants formed (via disk instability), and, during the second stage (caused by an encounter with a particular stellar-object leading to “in-system” fission- driven nucleogenesis), the terrestrial planets formed (via accretion)—we emphasize here that the mechanism of formation of such stellar-objects is generally universal and therefore encounters of such objects with stellar-systems may have occurred elsewhere across galaxies. If so, their aftereffects may perhaps be observed as puzzling features in the spectra of individual stars (such as idiosyncratic chemical enrichments) and/or in the structures of exoplanetary systems (such as unusually high planet densities or short orbital periods). This paper reviews and reinterprets astronomical data within the “fission-events framework”. Classification of stellar systems as “pristine” or “impacted” is offered. Keywords: exoplanets; stellar chemical compositions; nuclear fission; origin and evolution Citation: Tito, E.P.; Pavlov, V.I. “In-System” Fission-Events: An 1. Introduction Insight into Puzzles of Exoplanets As facilities and techniques for astronomical observations and analyses continue to and Stars?. Universe 2021, 7, 118. expand and gain in resolution power, their results provide increasingly detailed information https://doi.org/10.3390/universe about stellar systems, in particular, about the chemical compositions of stellar atmospheres 7050118 and structures of exoplanets. -
Mineralogy of Super-Earth Planets
This article was originally published in Treatise on Geophysics, Second Edition, published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who you know, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier's permissions site at: http://www.elsevier.com/locate/permissionusematerial Duffy T., Madhusudhan N. and Lee K.K.M Mineralogy of Super-Earth Planets. In: Gerald Schubert (editor-in-chief) Treatise on Geophysics, 2nd edition, Vol 2. Oxford: Elsevier; 2015. p. 149-178. Author's personal copy 2.07 Mineralogy of Super-Earth Planets T Duffy, Princeton University, Princeton, NJ, USA N Madhusudhan, University of Cambridge, Cambridge, UK KKM Lee, Yale University, New Haven, CT, USA ã 2015 Elsevier B.V. All rights reserved. 2.07.1 Introduction 149 2.07.2 Overview of Super-Earths 150 2.07.2.1 What Is a Super-Earth? 150 2.07.2.2 Observations of Super-Earths 151 2.07.2.3 Interior Structure and Mass–Radius Relationships 151 2.07.2.4 Selected Super-Earths 154 2.07.2.5 Super-Earth Atmospheres 155 2.07.3 Theoretical -
Terrestrial Planets
Terrestrial Planets First ever ‘whole Earth’ picture from deep space, taken by Bill Anders on Apollo 8 Apollo 8 crew, Bill Anders centre: The Earth is just a planet courtesy Nasa 1- 4 from the Sun Image courtesy: http://commons.wikimedia.org/wiki/Image:Terrestrial_planet_size_comparisons_edit.jpg Mercury, Venus, Earth and Mars are four astonishingly different planets Mercury and Venus have only been seen in any detail within the last 30 years Mercury in sight Courtesy NASA (Mariner 10) Mercury is visible only soon after the setting sun or shortly before dawn the Mariner 10 probe (1974/75) is the source of most information about Mercury – Messenger, launched 2004, first flypast in 2008 and orbit Mercury in 2011. ESA’s BepiColombo, to be launched in 2013 Mercury Mercury is like the Earth inside and the Moon outside Mercury has had a cooling and bombardment history similar to the moon It appears as cratered lava with scarps Its rocks are Earth-like Mariner 10 image Messenger images ↑ Double-ringed crater – a Mercury feature courtesy: http://messenger.jhuapl.edu/gallery/sciencePhotos/pics/S trom02.jpg ← Courtesy: http://messenger.jhuapl.edu/gal lery/sciencePhotos/pics/EN010 8828161M.jpg Messenger image Courtesy: http://messenger.jhuapl.edu/gallery/sciencePhotos/pics/Prockter06.jpg Mercury Close-up Mercury’s topography was formed under stronger gravity than on the Moon The Caloris basin is an impact crater ~1400 km across, beneath which is thought to be a dense mass 2 Mercury’s rotation period is exactly /3 of its orbital period -
Using an Energy Balance Model to Determine Exoplanetary Climates
Using an Energy Balance Model to Determine Exoplanetary Climates that Support Liquid Water By Macgregor Sullivan Presented to the Faculty of Wheaton College in Partial Fulfillment of the Requirements for Graduation with Departmental Honors in Physics May 14, 2018 1 Abstract The purpose of this thesis is to modify an energy balance atmospheric model created by R. Pierrehumbert (Pierrehumbert 2011). His energy balance model gave an estimate of Gliese 581g’s, a tidally locked exoplanet, atmosphere. Using an energy balance model, the surface and air temperatures can be found for a planet in equilibrium, when the amount incoming energy is equal to the amount of outgoing energy. Starting from Pierrehumbert’s model, we have added for a greenhouse effect and an ice-albedo feedback. We have also modified the model to test a rotating planet (similar to Earth) in addition to a tidally locked planet. This model, by varying the planet’s surface pressure, stellar flux, and the atmosphere's emissivity, can find which conditions leads to the planet having the temperatures needed to support liquid water. Surface pressure affects how efficient the planet is at redistributing heat leading to uniform temperatures across its surface. As the incoming stellar flux or the emissivity increase, the planet’s surface temperatures rise due the increase in absorbed energy from the planet’s surface. We have also found that the orbital distances that are able to support liquid water depend heavily on the pressure of the planet’s atmosphere. In future work, this model will produce the planet’s IR emission to determine if the planet is detectable using telescopes like the James Webb Space Telescope. -
Recipe for a Habitable Planet
Recipe for a Habitable Planet Aomawa Shields Clare Boothe Luce Associate Professor Shields Center for Exoplanet Climate and Interdisciplinary Education (SCECIE) University of California, Irvine ASU School of Earth and Space Exploration (SESE) December 2, 2020 A moment to pause… Leading effectively during COVID-19 • Employees Need Trust and Compassion: Be Present, Even When You're Distant • Employees Need Stability: Prioritize Wellbeing Amid Disruption • Employees Need Hope: Anchor to Your "True North" From “3 strategies for leading effectively during COVID-19” (https://www.gallup.com/workplace/306503/strategies-leading-effectively-amid-covid.aspx) Hobbies: reading movies, shows knitting mixed media/collage violin tea yoga good restaurants spa days the beach hiking smelling flowers hanging with family BINGO Ill. Niklas Elmehed. Ill. Niklas Elmehed. © Nobel Media. © Nobel Media. RadialVelocity (m/s) Nobel Prize in Physics 2019 Mayor & Queloz 1995 https://exoplanets.nasa.gov/ As of December 2, 2020 Aomawa Shields Recipe for a Habitable World Credit: NASA NNASA’sASA’s KKeplerepler MMissionission TESS Transiting Exoplanet Survey Satellite Credit: NASA-JPL/Caltech Proxima Centauri b Credit: ESO/M. Kornmesser LHS 1140b Credit: ESO TOI 700d Credit: NASA TESS planets in the Earth-sized regime Credit: NASA’s Goddard Space Flight Center Which ones do we follow up on? 20 The Habitable Zone (Kasting et al. 1993, Kopparapu et al. 2013) ) Runaway greenhouse Maximum CO2 greenhouse Stellar Mass (M Mass Stellar Distance from Star (AU) Snowball Earth Many factors can affect planetary habitability Aomawa Shields Recipe for a Habitable World Liquid water Aomawa Shields Recipe for a Habitable World Isotopic Birth Tides Orbit Abundance Environ. -
From Dust to Dust: Protoplanetary Disk Accretion, Hot Jupiter Climates, and the Evaporation of Rocky Planets
UC Berkeley UC Berkeley Electronic Theses and Dissertations Title From Dust to Dust: Protoplanetary Disk Accretion, Hot Jupiter Climates, and the Evaporation of Rocky Planets Permalink https://escholarship.org/uc/item/9jq3136f Author Perez-Becker, Daniel Alonso Publication Date 2013 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California From Dust to Dust: Protoplanetary Disk Accretion, Hot Jupiter Climates, and the Evaporation of Rocky Planets By Daniel Alonso Perez-Becker A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Physics in the Graduate Division of the University of California, Berkeley Committee in charge: Professor Eugene Chiang, Co-chair Professor Christopher McKee, Co-chair Professor Eliot Quataert Professor Geoffrey Marcy Fall 2013 From Dust to Dust: Protoplanetary Disk Accretion, Hot Jupiter Climates, and the Evaporation of Rocky Planets Copyright 2013 by Daniel Alonso Perez-Becker 1 Abstract From Dust to Dust: Protoplanetary Disk Accretion, Hot Jupiter Climates, and the Evaporation of Rocky Planets by Daniel Alonso Perez-Becker Doctor of Philosophy in Physics University of California, Berkeley Professor Eugene Chiang, Co-chair Professor Christopher McKee, Co-chair This dissertation is composed of three independent projects in astrophysics concerning phenomena that are concurrent with the birth, life, and death of planets. In Chapters 1 & 2, we study surface layer accretion in protoplanetary disks driven stellar X-ray and far-ultraviolet (FUV) radiation. In Chapter 3, we identify the dynamical mechanisms that control atmospheric heat redistribution on hot Jupiters. Finally, in Chapter 4, we characterize the death of low-mass, short-period rocky planets by their evaporation into a dusty wind. -
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland)
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland) American Astronomical Society August, 2019 100 — New Discoveries scope (JWST), as well as other large ground-based and space-based telescopes coming online in the next 100.01 — Review of TESS’s First Year Survey and two decades. Future Plans The status of the TESS mission as it completes its first year of survey operations in July 2019 will bere- George Ricker1 viewed. The opportunities enabled by TESS’s unique 1 Kavli Institute, MIT (Cambridge, Massachusetts, United States) lunar-resonant orbit for an extended mission lasting more than a decade will also be presented. Successfully launched in April 2018, NASA’s Tran- siting Exoplanet Survey Satellite (TESS) is well on its way to discovering thousands of exoplanets in orbit 100.02 — The Gemini Planet Imager Exoplanet Sur- around the brightest stars in the sky. During its ini- vey: Giant Planet and Brown Dwarf Demographics tial two-year survey mission, TESS will monitor more from 10-100 AU than 200,000 bright stars in the solar neighborhood at Eric Nielsen1; Robert De Rosa1; Bruce Macintosh1; a two minute cadence for drops in brightness caused Jason Wang2; Jean-Baptiste Ruffio1; Eugene Chiang3; by planetary transits. This first-ever spaceborne all- Mark Marley4; Didier Saumon5; Dmitry Savransky6; sky transit survey is identifying planets ranging in Daniel Fabrycky7; Quinn Konopacky8; Jennifer size from Earth-sized to gas giants, orbiting a wide Patience9; Vanessa Bailey10 variety of host stars, from cool M dwarfs to hot O/B 1 KIPAC, Stanford University (Stanford, California, United States) giants. 2 Jet Propulsion Laboratory, California Institute of Technology TESS stars are typically 30–100 times brighter than (Pasadena, California, United States) those surveyed by the Kepler satellite; thus, TESS 3 Astronomy, California Institute of Technology (Pasadena, Califor- planets are proving far easier to characterize with nia, United States) follow-up observations than those from prior mis- 4 Astronomy, U.C. -
Arxiv:1711.02098V2 [Astro-Ph.EP] 13 Jan 2018
Draft version January 16, 2018 Typeset using LATEX twocolumn style in AASTeX61 SIMULATED JWST/NIRISS TRANSIT SPECTROSCOPY OF ANTICIPATED TESS PLANETS COMPARED TO SELECT DISCOVERIES FROM SPACE-BASED AND GROUND-BASED SURVEYS Dana R. Louie,1 Drake Deming,1, 2 Loic Albert,3 L. G. Bouma,4 Jacob Bean,5, 2 and Mercedes Lopez-Morales6, 2 1Department of Astronomy, University of Maryland, College Park, MD 20742, USA 2TESS Atmospheric Characterization Working Group 3Institut de recherche sur les exoplanetes (iREx), Universite de Montreal, Montreal, Quebec, Canada 4Department of Astrophysical Sciences, Princeton University, Princeton, NJ 08540, USA 5Department of Astronomy and Astrophysics, University of Chicago, IL 60637, USA 6Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA Submitted to PASP ABSTRACT The Transiting Exoplanet Survey Satellite (TESS) will embark in 2018 on a 2-year wide-field survey mission, discov- ering over a thousand terrestrial, super-Earth and sub-Neptune-sized exoplanets (Rpl ≤ 4R⊕) potentially suitable for follow-up observations using the James Webb Space Telescope (JWST). This work aims to understand the suitability of anticipated TESS planet discoveries for atmospheric characterization by JWST's Near InfraRed Imager and Slitless Spectrograph (NIRISS) by employing a simulation tool to estimate the signal-to-noise (S/N) achievable in transmission spectroscopy. We applied this tool to Monte Carlo predictions of the TESS expected planet yield and then compared the S/N for anticipated TESS discoveries to our estimates of S/N for 18 known exoplanets. We analyzed the sensitivity of our results to planetary composition, cloud cover, and presence of an observational noise floor. -
Part 1: the 1.7 and 3.9 Earth Radii Rule
Hi this is Steve Nerlich from Cheap Astronomy www.cheapastro.com and this is What are exoplanets made of? Part 1: The 1.7 and 3.9 earth Radii rule. As of August 2016, the current count of confirmed exoplanets is up around 3,400 in 2,617 systems – with 590 of those systems confirmed to be multiplanet systems. And the latest thinking is that if you want to understand what exoplanets are made of you need to appreciate the physical limits of planet-hood, which are defined by the boundaries of 1.7 and 3.9 Earth radii . Consider that the make-up of an exoplanet is largely determined by the elemental make up of its protoplanetary disk. While most material in the Universe is hydrogen and helium – these are both tenuous gases. In order to generate enough gravity to hang on to them, you need a lot of mass to start with. So, if you’re Earth, or anything up to 1.7 times the radius of Earth – you’ve got no hope of hanging onto more than a few traces of elemental hydrogen and helium. Indeed, any exoplanet that’s less than 1.7 Earth radii has to be primarily composed of non-volatiles – that is, things that don’t evaporate or blow away easily – to have any chance of gravitationally holding together. A non-volatile exoplanet might be made of rock – which for our Solar System is a primarily silicon/oxygen based mineral matrix, but as we’ll hear, small sub-1.7 Earth radii exoplanets could be made of a whole range of other non-volatile materials. -
Super-Dense Remnants of Gas Giant Exoplanets
EPSC Abstracts Vol. 8, EPSC2013-986-1, 2013 European Planetary Science Congress 2013 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2013 Super-dense remnants of gas giant exoplanets A. Mocquet (1), O. Grasset (1) and C. Sotin (2) (1) Laboratoire de Planétologie et Géodynamique UMR 6112, Nantes University, France ([email protected] / Fax:+33-2-51125268, (2) Jet Propulsion Laboratory, Caltech, Pasadena, California, USA Abstract of metallic materials is performed through the Mie- Grüneisen-Debye theory, which provides comparable The masses that have been observed for three large results to both ANEOS and Thomas-Fermi-Dirac exoplanets, Kepler-52b, Kepler-52c, and Kepler-57b, formulations up to a few tens of TPa [2]. The are between 30 and 100 times the Earth mass, which mechanical effects induced by the loss of the massive implies densities higher than iron planets of the same atmosphere are described by a pressure unloading of sizes. We propose that these planets could represent the solid core surface, and by a consequent increase the naked solid cores of gas giants that would have of volume and decrease of the density. Following the lost their atmospheres, for instance during their methods employed to investigate the deformation of migration towards their star, and investigate the the Earth’s mantle by surface loads [4], the evolution conditions under which the density of these cores of the unloading and associated decompression could remain close to their initial highly pressurized processes, is assessed by the convolution of a time- state. dependent source, the extensive surface stress, with the time varying viscoelastic response of the 1. -
Composition and Fate of Short-Period Super-Earths: the Case of Corot-7B
Astronomy & Astrophysics manuscript no. corot7b_Rv7pdf c ESO 2018 November 12, 2018 Composition and fate of short-period super-Earths The case of CoRoT-7b D. Valencia1, M. Ikoma1;2, T. Guillot1, and N. Nettelmann3 1 Observatoire de la C^oted'Azur, Universit´ede Nice-Sophia Antipolis, CNRS UMR 6202, BP 4229, F-06304 Nice Cedex 4, France 2 Dept. of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama, Meguro-ku, Tokyo 152-8551, Japan 3 Institut f¨urPhysik, Universit¨atRostock, D-18051 Rostock, Germany Preprint online version: November 12, 2018 ABSTRACT Context. The discovery of CoRoT-7b, a planet of radius 1:68 ± 0:09 R⊕, mass 4:8 ± 0:8; M⊕ and orbital period of 0:854 days demonstrates that small planets can orbit extremely close to their star. Aims. Several questions arise concerning this planet, in particular concerning its possible composition, and fate. Methods. We use knowledge of hot Jupiters, mass loss estimates and models for the interior structure and evolution of planets to understand its composition, structure and evolution. Results. The inferred mass and radius of CoRoT-7b are consistent with a rocky planet that would be significantly depleted in iron relative to the Earth. However, a one sigma increase in mass (5:6 M⊕) and one sigma decrease in size (1:59 R⊕) would make the planet compatible with an Earth-like composition (33% iron, 67% silicates). Alternatively, it is possible that CoRoT-7b contains a significant amount of volatiles. For a planet made of an Earth-like interior and an outer volatile-rich vapor envelope, an equally good fit to the measured mass and radius is found for a mass of the vapor envelope equal to 3% (and up to 10% at most) of the planetary mass.