Space-Based “Probe Class” Missions for Exoplanet Research Jennifer
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Technology Development for Future Sparse Aperture Telescopes and Interferometers in Space
A Technology Whitepaper submitted to the 2010 Decadal Survey Technology Development for Future Sparse Aperture Telescopes and Interferometers in Space 24 March 2009 NASA Centers: GSFC: Kenneth G. Carpenter, Keith Gendreau, Jesse Leitner, Richard Lyon, Eric Stoneking MSFC: H. Philip Stahl Industrial Partners: Aurora Flight Systems: Joe Parrish LMATC: Carolus J. Schrijver, Robert Woodruff NGST – Amy Lo, Chuck Lillie Seabrook Engineering: David Mozurkewich University/Astronomical Institute Partners: College de France: Antoine Labeyrie MIT: David Miller NOAO: Ken Mighell SAO: Margarita Karovska, James Phillips STScI: Ronald J. Allen UCO/Boulder: Webster Cash Abstract We describe the major technology development efforts that need to occur throughout the 2010 decade in order to enable a wide variety of sparse aperture and interferometric missions in the following decade. These missions are critical to achieving the next major revolution in astronomical observations by dramatically increasing the achievable angular resolution by more than 2 orders of magnitude, over wavelengths stretching from the x-ray and ultraviolet into the infrared and sub-mm. These observations can only be provided by long-baseline interferometers or sparse aperture telescopes in space, since the aperture diameters required are in excess of 500m - a regime in which monolithic or segmented designs are not and will not be feasible - and since they require observations at wavelengths not accessible from the ground. The technology developments needed for these missions are challenging, but eminently feasible with a reasonable investment over the next decade to enable flight in the 2025+ timeframe. That investment would enable tremendous gains in our understanding of the structure of the Universe and of its individual components in ways both anticipated and unimaginable today. -
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. -
Exoplanet Community Report
JPL Publication 09‐3 Exoplanet Community Report Edited by: P. R. Lawson, W. A. Traub and S. C. Unwin National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, California March 2009 The work described in this publication was performed at a number of organizations, including the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (NASA). Publication was provided by the Jet Propulsion Laboratory. Compiling and publication support was provided by the Jet Propulsion Laboratory, California Institute of Technology under a contract with NASA. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not constitute or imply its endorsement by the United States Government, or the Jet Propulsion Laboratory, California Institute of Technology. © 2009. All rights reserved. The exoplanet community’s top priority is that a line of probeclass missions for exoplanets be established, leading to a flagship mission at the earliest opportunity. iii Contents 1 EXECUTIVE SUMMARY.................................................................................................................. 1 1.1 INTRODUCTION...............................................................................................................................................1 1.2 EXOPLANET FORUM 2008: THE PROCESS OF CONSENSUS BEGINS.....................................................2 -
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 -
Spectral Analysis of Atmospheres by Nulling Interferometry
Molecules in the Atmospheres of Extrasolar Planets ASP Conference Series, Vol. 450 J-P. Beaulieu, S. Dieters, and G. Tinetti, eds. c 2011 Astronomical Society of the Pacific Spectral Analysis of Atmospheres by Nulling Interferometry M. Ollivier and S. Jacquinod Institut d’Astrophysique Spatiale - Université de Paris-Sud 11 and CNRS (UMR 8617) Abstract. Nulling interferometry has often been considered as one of the most promising techniques to get spectra, in the thermal infrared spectral range, of exo- planet and particularly telluric ones. The required performance, in terms of nulling depth, spectral bandwidth and stability begins to be achievable in the laboratory. How- ever, concrete observatory projects have strong difficulties to emerge in space agencies programs, because of mission requirements complexity. In this paper, I present the per- formance various scientific objectives need and the state of the art of this technique, including mission aspects. I finally propose elements that could help defining a first space mission project. 1. Nulling Interferometry : Theoretical Aspects 1.1. Principle of Nulling Interferometry Nulling interferometry has been proposed in the late 70s as a possible technique to detect and spectroscopically characterize planets around nearby stars at wavelengths where diffraction prevents from the use of single aperture telescopes (Bracewell 1978). The principle of nulling interferometry in a 2-telescope configuration is described in figure 1 (left). The idea is to use two small telescopes, pointed in the direction of the star and to combine their beams. On the beam combiner the wavefronts from both star and planet create interferences. If we introduce a π phase-shift in one arm of the inter- ferometer, the stellar interference is destructive (the optical path difference is equal to zero). -
OLLI Talk on Exoplanets
OLLI SC211 SPACE EXPLORATION: THE SEARCH FOR LIFE BEYOND EARTH April 13, 2017 Michal Peri NASA Solar System Ambassador Exoplanet2 Detection • Methods • Missions • Discoveries • Resources Image: C. Pulliam & D. Aguilar/CfA A long history … in our imaginations 3 https://en.wikipedia.org/wiki/Giordano_Bruno#/media/File:Relief_Bruno_Campo_dei_Fiori_n1.jpg Giordano Bruno in his De l'infinito universo et mondi (1584) suggested that "stars are other suns with their own planets” that “have no less virtue nor a nature different to that of our earth" and, like Earth, "contain animals and inhabitants.” For this heresy, he was burned by the inquisition. 3 https://www.loc.gov/today/cyberlc/feature_wdesc.php?rec=7148 5 Detection Methods Radial Velocity 619 planets Gravitational Microlensing 44 planets Direct Imaging 44 planets Transit 2771 planets Velocity generates Doppler 7 Shift Sound star receding star approaching Light wave “stretched” → red shift wave “squashed” → blue shift Orbiting planet causes Doppler shift in starlight 8 https://exoplanets.nasa.gov/interactable/11/ Radial Velocity Method 9 • The most successful method of detecting exoplanets pre-2010 • Doppler shifts in the stellar spectrum reveal presence of planetary companion(s) • Measure lower limit of the planetary mass and orbital parameters Doppler Shift Time Nikole K. Lewis, STScI Radial Velocity Detections Radial Velocity 1992 Planetary Mass 10 Detection Methods Radial Velocity 619 planets Gravitational Microlensing 44 planets Direct Imaging 44 planets Transit 2771 planets • Microlens -
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. -
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.