Echo Exoplanet Characterisation Observatory
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
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 -
The Atacama Pathfinder Experiment — Reaching New Heights in Submillimetre Astronomy
The Atacama Pathfinder Experiment — Reaching New Heights in Submillimetre Astronomy European Southern Observatory APEX on watch at Chajnantor. Credit: ESO/B. Tafreshi (twanight.org) The Atacama Pathfinder Experiment — Reaching New Heights in Submillimetre Astronomy ESO operates the Atacama Pathfinder “thermometers” known as bolometers submillimeter Array, a revolutionary new Experiment telescope, APEX, at one of to detect submillimetre light. In order to telescope that ESO, together with its the highest observatory sites on Earth, at be able to detect the tiny temperature international partners, is now operating an elevation of 5100 metres, high on the changes caused by the faint submillimetre on the Chajnantor Plateau. APEX is based Chajnantor Plateau in Chile’s Atacama radiation, each of these thermometers on a prototype antenna constructed for region. is cooled to less than 0.3 degrees above the ALMA project, and it will find many absolute zero — a frigid –272.85 °C. targets that ALMA will be able to study in APEX is a 12-metre diameter telescope, LABOCA’s high sensi tivity, together with great detail. operating at millimetre and submillimetre its wide field of view (one third of the wavelengths — between infrared light diameter of the full Moon), make it an APEX is a collaboration between the and radio waves. Submillimetre astronomy invaluable tool for imaging the submilli- Max Planck Institute for Radio Astronomy, opens a window into the cold, dusty metre Universe. the Onsala Space Observatory and ESO. and distant Universe, but the faint signals The telescope is operated by ESO. from space are heavily absorbed by APEX was developed as a pathfinder for water vapour in the Earth’s atmosphere. -
Site Testing for Submillimetre Astronomy at Dome C, Antarctica
A&A 535, A112 (2011) Astronomy DOI: 10.1051/0004-6361/201117345 & c ESO 2011 Astrophysics Site testing for submillimetre astronomy at Dome C, Antarctica P. Tremblin1, V. Minier1, N. Schneider1, G. Al. Durand1,M.C.B.Ashley2,J.S.Lawrence2, D. M. Luong-Van2, J. W. V. Storey2,G.An.Durand3,Y.Reinert3, C. Veyssiere3,C.Walter3,P.Ade4,P.G.Calisse4, Z. Challita5,6, E. Fossat6,L.Sabbatini5,7, A. Pellegrini8, P. Ricaud9, and J. Urban10 1 Laboratoire AIM Paris-Saclay (CEA/Irfu, Univ. Paris Diderot, CNRS/INSU), Centre d’études de Saclay, 91191 Gif-Sur-Yvette, France e-mail: [pascal.tremblin;vincent.minier]@cea.fr 2 University of New South Wales, 2052 Sydney, Australia 3 Service d’ingénierie des systèmes, CEA/Irfu, Centre d’études de Saclay, 91191 Gif-Sur-Yvette, France 4 School of Physics & Astronomy, Cardiff University, 5 The Parade, Cardiff, CF24 3AA, UK 5 Concordia Station, Dome C, Antarctica 6 Laboratoire Fizeau (Obs. Côte d’Azur, Univ. Nice Sophia Antipolis, CNRS/INSU), Parc Valrose, 06108 Nice, France 7 Departement of Physics, University of Roma Tre, Italy 8 Programma Nazionale Ricerche in Antartide, ENEA, Rome Italy 9 Laboratoire d’Aérologie, UMR 5560 CNRS, Université Paul-Sabatier, 31400 Toulouse, France 10 Chalmers University of Technology, Department of Earth and Space Sciences, 41296 Göteborg, Sweden Received 25 May 2011 / Accepted 17 October 2011 ABSTRACT Aims. Over the past few years a major effort has been put into the exploration of potential sites for the deployment of submillimetre astronomical facilities. Amongst the most important sites are Dome C and Dome A on the Antarctic Plateau, and the Chajnantor area in Chile. -
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](https://docslib.b-cdn.net/cover/5900/arxiv-1711-02098v2-astro-ph-ep-13-jan-2018-1475900.webp)
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. -
Roger Angel University of Arizona
NIAC Fellows meeting Atlanta March 7 2007 Phase I report Practicality of a solar shield in space to counter global warming Roger Angel University of Arizona Pete Worden and Kevin Parkin NASA Ames Research Center Dave Miller MIT Planet Earth driver’s test 1) You are zipping along happily, when you see warning lights ahead in the distance but visibility is not so great. What should you do? a) Just floor it b) take you foot off the accelerator c) apply the brakes 2) You find you have no brakes. What should you do now? The warning CO2 in atmosphere works just like water vapor • Lets in warming sunlight in the day • when humidity is high heat is trapped and nights stay warm • when humidity is low heat escapes and nights are cold • But unlike water vapor, CO2 hangs around – added CO2 in the atmosphere takes a century or two to dissipate Geoengineering solutions could be really useful • Needed if current CO2 level already beyond “tipping point” • Even extreme conservation may not be able to stop abrupt and disastrous changes e.g. – changes in ocean circulation – Greenland melts (20’ permanent sea level rise) • Many leading scientists seriously worried • Probability of disaster 10% - 20%? – Geoengineering like taking out insurance against unlikely but catastrophic event) Geoengineering has been taboo • People worry it will take off the pressure for permanent solution of not burning fossil fuel – Administration pointed to possibility of geoengineering and space mirrors just before recent IPCC report • If used for an extended period, would lead to seriously unstable planet Earth, ever more hooked on carbon • But if we don’t look at it, we have no insurance Heating reversible by reducing solar flux • Govindasamy, B. -
Eao Submillimetre Futures Paper Series, 2019
EAO SUBMILLIMETRE FUTURES PAPER SERIES, 2019 The East Asian Observatory∗ James Clerk Maxwell Telescope 660 N. A‘ohok¯ u¯ Place, Hilo, Hawai‘i, USA, 96720 1 About This Series Submillimetre astronomy is an active and burgeoning field that is poised to answer some of the most pressing open questions about the universe. The James Clerk Maxwell Telescope, operated by the East Asian Observatory, is at the forefront of discovery as it is the largest single-dish submillimetre telescope in the world. Situated at an altitude of 4,092 metres on Maunakea, Hawai‘i, USA, the facility capitalises on the 850 µm observing window that offers crucial insights into the cold dust that forms stars and galaxies. In 1997, the Submillimetre Common User Bolometer Array (SCUBA) was commissioned, allowing astronomers to detect the furthest galaxies ever recorded (so-called SCUBA galaxies) and develop our understanding of the earliest stages of star formation. Since 2011, its successor, SCUBA-2, has revolutionised submillimetre wavelength surveys by mapping the sky hundreds of times faster than SCUBA. The extensive data collected spans a wealth of astronomy sub-fields and has inspired world-wide collaborations and innovative analysis methods for nearly a decade. Building on the successes of these instruments, the East Asian Observatory is constructing a third generation 850 µm wide-field camera with intrinsic polarisation capabilities for deployment on the James Clerk Maxwell Telescope. In May, 2019, the “EAO Submillimetre Futures” meeting was held in Nanjing, China to discuss the science drivers of future instrumentation and the needs of the submillimetre astronomy community. A central focus of the meeting was the new 850 µm camera. -
Workshop Report on Managing Solar Radiation
NASA/CP–2007-214558 April 2007 Workshop Report on Managing Solar Radiation Compiled and Edited by: Lee Lane Consultant, CRA International, Boston, Massachusetts Ken Caldeira Department of Global Ecology, Carnegie Institution of Washington, at Stanford, California Robert Chatfield Earth Sciences Division, NASA Ames Research Center, Moffett Field, California Stephanie Langhoff Chief Scientist, NASA Ames Research Center, Moffett Field, California Report of a workshop jointly sponsored by NASA Ames Research Center and the Carnegie Institution of Washington Department of Global Ecology held at Ames Research Center, Moffett Field, California on November 18 - 19, 2006 The NASA STI Program Office . in Profile Since its founding, NASA has been dedicated to the • CONFERENCE PUBLICATION. Collected advancement of aeronautics and space science. The papers from scientific and technical confer- NASA Scientific and Technical Information (STI) ences, symposia, seminars, or other meetings Program Office plays a key part in helping NASA sponsored or cosponsored by NASA. maintain this important role. • SPECIAL PUBLICATION. Scientific, technical, The NASA STI Program Office is operated by or historical information from NASA programs, Langley Research Center, the Lead Center for projects, and missions, often concerned with NASA’s scientific and technical information. The subjects having substantial public interest. NASA STI Program Office provides access to the NASA STI Database, the largest collection of • TECHNICAL TRANSLATION. English‑ aeronautical and space