Exploring the Atmospheres of Diverse Worlds Beyond Our Solar System
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Phases of Venus and Galileo
Galileo and the phases of Venus I) Periods of Venus 1) Synodical period and phases The synodic period1 of Venus is 584 days The superior2 conjunction occured on 11 may 1610. Calculate the date of the quadrature, of the inferior conjunction and of the next superior conjunction, supposing the motions of the Earth and Venus are circular and uniform. In fact the next superior conjunction occured on 11 december 1611 and inferior conjunction on 26 february 1611. 2) Sidereal period The sidereal period of the Earth is 365.25 days. Calculate the sidereal period of Venus. II) Phases on Venus in geo and heliocentric models 1) Phases in differents models 1) Determine the phases of Venus in geocentric models, where the Earth is at the center of the universe and planets orbit around (Venus “above” or “below” the sun) * Pseudo-Aristoteles model : Earth (center)-Moon-Sun-Mercury-Venus-Mars-Jupiter-Saturne * Ptolemeo’s model : Earth (center)-Moon-Mercury-Venus-Sun-Mars-Jupiter-Saturne 2) Determine the phases of Venus in the heliocentric model, where planets orbit around the sun. Copernican system : Sun (center)-Mercury-Venus-Earth-Mars-Jupiter-Saturne 2) Observations of Galileo Galileo (1564-1642) observed Venus in 1610-1611 with a telescope. Read the letters of Galileo. May we conclude that the Copernican model is the only one available ? When did Galileo begins to observe Venus? Give the approximate dates of the quadrature and of the inferior conjunction? What are the approximate dates of the 5 observations of Galileo supposing the figure from the Essayer, was drawn in 1610-1611 1 The synodic period is the time that it takes for the object to reappear at the same point in the sky, relative to the Sun, as observed from Earth; i.e. -
Planetary Phase Variations of the 55 Cancri System
The Astrophysical Journal, 740:61 (7pp), 2011 October 20 doi:10.1088/0004-637X/740/2/61 C 2011. The American Astronomical Society. All rights reserved. Printed in the U.S.A. PLANETARY PHASE VARIATIONS OF THE 55 CANCRI SYSTEM Stephen R. Kane1, Dawn M. Gelino1, David R. Ciardi1, Diana Dragomir1,2, and Kaspar von Braun1 1 NASA Exoplanet Science Institute, Caltech, MS 100-22, 770 South Wilson Avenue, Pasadena, CA 91125, USA; [email protected] 2 Department of Physics & Astronomy, University of British Columbia, Vancouver, BC V6T1Z1, Canada Received 2011 May 6; accepted 2011 July 21; published 2011 September 29 ABSTRACT Characterization of the composition, surface properties, and atmospheric conditions of exoplanets is a rapidly progressing field as the data to study such aspects become more accessible. Bright targets, such as the multi-planet 55 Cancri system, allow an opportunity to achieve high signal-to-noise for the detection of photometric phase variations to constrain the planetary albedos. The recent discovery that innermost planet, 55 Cancri e, transits the host star introduces new prospects for studying this system. Here we calculate photometric phase curves at optical wavelengths for the system with varying assumptions for the surface and atmospheric properties of 55 Cancri e. We show that the large differences in geometric albedo allows one to distinguish between various surface models, that the scattering phase function cannot be constrained with foreseeable data, and that planet b will contribute significantly to the phase variation, depending upon the surface of planet e. We discuss detection limits and how these models may be used with future instrumentation to further characterize these planets and distinguish between various assumptions regarding surface conditions. -
On the Use of Planetary Science Data for Studying Extrasolar Planets a Science Frontier White Paper Submitted to the Astronomy & Astrophysics 2020 Decadal Survey
On the Use of Planetary Science Data for Studying Extrasolar Planets A science frontier white paper submitted to the Astronomy & Astrophysics 2020 Decadal Survey Thematic Area: Planetary Systems Principal Author Daniel J. Crichton Jet Propulsion Laboratory, California Institute of Technology [email protected] 818-354-9155 Co-Authors: J. Steve Hughes, Gael Roudier, Robert West, Jeffrey Jewell, Geoffrey Bryden, Mark Swain, T. Joseph W. Lazio (Jet Propulsion Laboratory, California Institute of Technology) There is an opportunity to advance both solar system and extrasolar planetary studies that does not require the construction of new telescopes or new missions but better use and access to inter-disciplinary data sets. This approach leverages significant investment from NASA and international space agencies in exploring this solar system and using those discoveries as “ground truth” for the study of extrasolar planets. This white paper illustrates the potential, using phase curves and atmospheric modeling as specific examples. A key advance required to realize this potential is to enable seamless discovery and access within and between planetary science and astronomical data sets. Further, seamless data discovery and access also expands the availability of science, allowing researchers and students at a variety of institutions, equipped only with Internet access and a decent computer to conduct cutting-edge research. © 2019 California Institute of Technology. Government sponsorship acknowledged. Pre-decisional - For planning -
Fantasy & Science Fiction V030n04
THE MA GAZINE Of Fantasy and JACK VANCE Science Fiction ISAAC ASIMOV J.T. MCINTOS NOVELETS We Can Remember It For You Wholesale Philip k. dick 4 The Sorcerer Pharesm JACK VANCE 79 SHORT STORIES Appoggiatura A. M, MARPLE 25 But Soft, What Light . CAROL EMSHWILLER 41 The Sudden Silence J. T. MCINTOSH 45 The Face Is Familiar GILBERT THOMAS 64 The Space Twins JAMES PULLEY 75 Bordered In Black LARRY NIVEN 112 FEATURES Cartoon GAHAN WILSON 24 Books JUDITH MERRIL 31 Injected Memory THEODORE L. THOMAS 62 Verse: The Octopus DORIS PITKIN BUCK 63 Science: The Nobelmen of Science ISAAC ASIMOV 101 F&SF Marketplace 129 Cover by Jack Gaughan (illustrating "The Sorcerer Pharesm”) Joseph W. Ferman, publishek Edward L. Ferman, editor Ted White, assistant editor Isaac Asimov, science editor Judith Merril, book editor Robert P. Mills, consulting editor Dale Beardale, aRCULATiON manager The Magazine of Fantasy and Science Fiction, Volume 30, No. 4, Whole No. 179, Apr. 1966. Published monthly by Mercury Press, Inc., at 504 o copy. Annual subscription $5.00; $5.50 in Canada and the Pan American Union, $6.00 in all other countries. Publication office, 10 Ferry Street, Concord, N. H. 03302. Editorial and general mail should be sent to 347 East 53rd St., New York, N. Y. 10022. Second Class postage paid at Concord, N. H. Printed in U.S.A. © 1966 by Mercury Press, Inc. All rights including translations into other languages, reserved. Submissions must be accompanied by stamped, self-addressed envelopes: the Publisher assumes no responsibility for return of unsolicited manuscripts. -
ON the INCLINATION DEPENDENCE of EXOPLANET PHASE SIGNATURES Stephen R
The Astrophysical Journal, 729:74 (6pp), 2011 March 1 doi:10.1088/0004-637X/729/1/74 C 2011. The American Astronomical Society. All rights reserved. Printed in the U.S.A. ON THE INCLINATION DEPENDENCE OF EXOPLANET PHASE SIGNATURES Stephen R. Kane and Dawn M. Gelino NASA Exoplanet Science Institute, Caltech, MS 100-22, 770 South Wilson Avenue, Pasadena, CA 91125, USA; [email protected] Received 2011 December 2; accepted 2011 January 5; published 2011 February 10 ABSTRACT Improved photometric sensitivity from space-based telescopes has enabled the detection of phase variations for a small sample of hot Jupiters. However, exoplanets in highly eccentric orbits present unique opportunities to study the effects of drastically changing incident flux on the upper atmospheres of giant planets. Here we expand upon previous studies of phase functions for these planets at optical wavelengths by investigating the effects of orbital inclination on the flux ratio as it interacts with the other effects induced by orbital eccentricity. We determine optimal orbital inclinations for maximum flux ratios and combine these calculations with those of projected separation for application to coronagraphic observations. These are applied to several of the known exoplanets which may serve as potential targets in current and future coronagraph experiments. Key words: planetary systems – techniques: photometric 1. INTRODUCTION and inclination for a given eccentricity. We further calculate projected separations at apastron as a function of inclination The changing phases of an exoplanet as it orbits the host star and determine their correspondence with maximum flux ratio have long been considered as a means for their detection and locations. -
1 Revisiting 154-Day Periodicity in the Occurrence of Hard Flares. A
Revisiting 154-day periodicity in the occurrence of hard flares. A planetary influence? Ian Edmonds 12 Lentara St, Kenmore, Brisbane, Australia 4069. Ph/Fax 61 7 3378 6586, [email protected] Keywords: flare periodicity; planetary model; sunspot emergence; Mercury-Earth conjunction. Abstract. Rieger et al (1984) reported observations of a 154 day periodicity in flares during solar cycle 21. This paper discusses the observations in the light of a simple empirical planetary model of sunspot emergence. The planetary model predicts sunspot emergence when Mercury and Earth approach conjunction and Mercury approaches the Sun. We show that the reported times of flare activity are coherent with the planetary model. While the base period of the model is 170 days, the average model period, over the interval of flare recordings, is 157 days due to a 180 degree phase change in the planetary forcing near the middle of the record interval. We conclude that the periodicity at 154 days arises when the phase change in planetary forcing and the resulting progressive phase change in total sunspot area emergence and flare occurrence shifts the major peak in the flare spectrum from the planetary forcing period, 170 days, to 154 days. 1. Introduction. The observation of an ~ 154 day periodicity in the occurrence of hard flares, Rieger et al (1984), hereafter R84, initiated a now 32 year long investigation of mid-range, 40 – 2000 day, periodicities in solar activity. R84 analysed 139 flares recorded by the gamma ray spectrometer on the Solar Maximum Mission (solar cycle 21) from February 1980 through to the end of 1983 when recording ceased. -
Distinguishing Between Stellar and Planetary Companions with Phase Monitoring
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln NASA Publications National Aeronautics and Space Administration 2012 Distinguishing between stellar and planetary companions with phase monitoring Stephen R. Kane NASA Exoplanet Science Institute, [email protected] Dawn M. Gelino NASA Exoplanet Science Institute, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/nasapub Kane, Stephen R. and Gelino, Dawn M., "Distinguishing between stellar and planetary companions with phase monitoring" (2012). NASA Publications. 116. https://digitalcommons.unl.edu/nasapub/116 This Article is brought to you for free and open access by the National Aeronautics and Space Administration at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in NASA Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Mon. Not. R. Astron. Soc. 424, 779–788 (2012) doi:10.1111/j.1365-2966.2012.21265.x Distinguishing between stellar and planetary companions with phase monitoring Stephen R. Kane andDawnM.Gelino NASA Exoplanet Science Institute, Caltech, MS 100-22, 770 South Wilson Avenue, Pasadena, CA 91125, USA Accepted 2012 May 8. Received 2012 May 8; in original form 2012 March 24 ABSTRACT Exoplanets which are detected using the radial velocity technique have a well-known ambiguity of their true mass, caused by the unknown inclination of the planetary orbit with respect to the plane of the sky. Constraints on the inclination are aided by astrometric follow-up in rare cases or, in ideal situations, through subsequent detection of a planetary transit. As the predicted inclination decreases, the mass of the companion increases leading to a change in the predicted properties. -
Comprehensive Wide-Band Magnitudes and Albedos for the Planets, with Applications to Exo-Planets and Planet Nine
Comprehensive Wide-Band Magnitudes and Albedos for the Planets, With Applications to Exo-Planets and Planet Nine Anthony Mallama 14012 Lancaster Lane, Bowie, MD, 20715, USA [email protected] Bruce Krobusek 5950 King Hill Drive, Farmington, NY, 14425, USA [email protected] Hristo Pavlov 9 Chad Place, St. Clair, NSW 2759, Australia [email protected] Prepared for Icarus Pages: 49 Figures: 1 Tables: 37 Original version submitted: 2016 April 22 Reviewer comments received: 2016 July 26 Revised manuscript submitted: 2016 August 30 Accepted for publication by Icarus: 2016 September 14 Abstract Complete sets of reference magnitudes in all 7 Johnson-Cousins bands (U, B, V, R, I, RC and IC) and the 5 principal Sloan bands (u’, g’, r’, i', and z’) are presented for the 8 planets. These data are accompanied by illumination phase functions and other formulas which characterize the instantaneous brightness of the planets. The main source of Johnson-Cousins magnitudes is a series of individualized photometric studies reported in recent years. Gaps in that dataset were filled with magnitudes synthesized in this study from published spectrophotometry. The planetary Sloan magnitudes, which are established here for the first time, are an average of newly recorded Sloan filter photometry, synthetic magnitudes and values transformed from the Johnson-Cousins system. Geometric albedos derived from these two sets of magnitudes are consistent within each photometric system and between the systems for all planets and in all bands. This consistency validates the albedos themselves as well as the magnitudes from which they were derived. In addition, a quantity termed the delta stellar magnitude is introduced to indicate the difference between the magnitude of a planet and that of its parent star. -
Heterogenization of Complexes with Redox Active Ligands for Hydrogen Evolution Reaction
University of Louisville ThinkIR: The University of Louisville's Institutional Repository Electronic Theses and Dissertations 12-2017 Heterogenization of complexes with redox active ligands for hydrogen evolution reaction. Wuyu Zhang University of Louisville Follow this and additional works at: https://ir.library.louisville.edu/etd Part of the Engineering Commons Recommended Citation Zhang, Wuyu, "Heterogenization of complexes with redox active ligands for hydrogen evolution reaction." (2017). Electronic Theses and Dissertations. Paper 2871. https://doi.org/10.18297/etd/2871 This Doctoral Dissertation is brought to you for free and open access by ThinkIR: The University of Louisville's Institutional Repository. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of ThinkIR: The University of Louisville's Institutional Repository. This title appears here courtesy of the author, who has retained all other copyrights. For more information, please contact [email protected]. HETEROGENIZATION OF COMPLEXES WITH REDOX ACTIVE LIGANDS FOR HYDROGEN EVOLUTION REACTION By Wuyu Zhang B.A., Changzhou University, 2006 M.S., Beijing University of Chemical Technology, 2010 A Dissertation Submitted to the Faculty of the College of Arts and Science of the University of Louisville in Fulfillment Of the Requirements for the Degree of Doctor of Philosophy in Chemistry Department of Chemistry University of Louisville Louisville, KY December 2017 © 2017 by Wuyu Zhang All Rights Reserved HETEROGENIZATION OF COMPLEXES WITH REDOX ACTIVE LIGANDS FOR HYDROGEN EVOLUTION REACTION By Wuyu Zhang B.A., Changzhou University, 2006 M.S., Beijing University of Chemical Technology, 2010 A Dissertation Approved on September 22, 2017 By the following Dissertation Committee Dr. -
Tidal Deformation of Planets and Satellites: Models and Methods for Laser- and Radar Altimetry
Tidal Deformation of Planets and Satellites: Models and Methods for Laser- and Radar Altimetry vorgelegt von Diplom Physiker Gregor Steinbr¨ugge geb. in Berlin von der Fakult¨atVI { Planen Bauen Umwelt der Technischen Universit¨atBerlin zur Erlangung des akademischen Grades Doktor der Naturwissenschaften - Dr. rer. nat. - genehmigte Dissertation Vorsitzender: Prof. Dr. Dr. h.c. Harald Schuh Gutachter: Prof. Dr. J¨urgenOberst Gutachter: Prof. Dr. Nicolas Thomas Gutachter: Prof. Dr. Tilman Spohn Tag der wissenschaftlichen Aussprache: 27.03.2018 Berlin 2018 2 Contents Title Page 1 Contents 3 List of Figures 7 List of Tables 9 1 Introduction 15 1.1 Structure of the Dissertation . 16 1.1.1 Icy Satellites . 17 1.1.2 Mercury . 20 1.2 Theory of Tides . 21 1.2.1 Tidal Potentials . 21 1.2.2 Response of Planetary Bodies to Tidal Forces . 23 1.3 Measuring Tidal Deformations . 25 1.3.1 Measurement Concepts . 25 1.3.2 Laser Altimetry . 25 1.3.3 Radar Altimetry . 26 1.4 Missions and Instruments . 27 1.4.1 REASON and the Europa Clipper Mission . 27 1.4.2 GALA and the JUICE Mission . 28 1.4.3 BELA and the BepiColombo Mission . 29 2 Research Paper I 31 2.1 Introduction . 32 2.2 Instrument Performance Modeling . 32 2.2.1 Link Budget . 32 2.2.2 Signal-to-Noise Ratio . 33 2.3 Expected Science Performance . 37 2.3.1 Topographic Coverage . 37 2.3.2 Slope and Roughness . 37 2.4 Tidal Deformation . 40 2.4.1 Covariance Analysis . 40 2.4.2 Numerical Simulation . -
GALILEO and the PHASES of VENUS Abstract
GALILEO AND THE PHASES OF VENUS Charles-Henri Eyraud Institut National de Recherche Pédagogique (France) Abstract In this article we use Galileo’s letters and drawings to understand his observations of the phases of Venus in 1610-1611. Our article is presented as an exercise for students to understand the conclusions of the great astronomer. PERIODS OF VENUS • Synodical period and phases The synodic period is the time that it takes for the object to reappear at the same point in the sky, relative to the Sun, as observed from Earth; i.e. returns to the same elongation and planetary phase. This is the time that elapses between two successive conjunctions with the Sun. An inferior conjunction occurs when Venus and the Earth lie in a line on the same side of the Sun. When Venus is on the opposite side of the Sun, it is a superior conjunction. The synodic period of Venus is 584 days. The superior conjunction occured on 11th May 1610. Calculate the date of the quadrature, of the inferior conjunction and of the next superior conjunction, supposing the motions of the Earth and Venus are circular and uniform (Figure 2). In fact the next superior conjunction occured on 11th December 1611 and inferior conjunction on 26th February 1611. • Sidereal period The sidereal period is the time that it takes the object to make one full orbit around the Sun, relative to the stars. The sidereal period of the Earth is 365.25 days. Calculate the sidereal period of Venus. PHASES OF VENUS IN GEO AND HELIOCENTRIC MODELS • Phases 1) Determine the phases of Venus in geocentric models, where the Earth is at the center of the universe and planets orbit around (Mercury and Venus “above” or “below” the Sun). -
Echo Exoplanet Characterisation Observatory
1 2 EChO Exoplanet Characterisation Observatory Contact person: Dr. Giovanna Tinetti, University College London, Dep. of Physics & Astronomy, Gower Street, London WC1E 6BT, UK Phone: +44 (0)7912509617, e-mail: [email protected] Proposing team Co-PIs J.P. Beaulieu T. Henning M. Meyer G. Micela I. Ribas D. Stam M. Swain G. Tinetti IAP MPIA ETH INAF IEEC SRON JPL UCL France Germany Switzerland Italy Spain Netherlands US UK Science core team and working group coordinators A. Aylward (UCL), R. van Boekel (MPIA), A. Coradini (INAF), T. Encrenaz (LESIA, Obs. Paris), I. Snellen (Un. Leiden), M. R. Zapatero-Osorio (CAB) J. Bouwman (MPIA), J. Cho (QMUL), V. Coude´ du Foresto (LESIA, Obs. Paris), T. Guillot (Obs. Nice), M. Lopez-Morales (IEEC), I. Mueller-Wodarg (Imperial College), E. Palle (IAC), F. Selsis (Un. Bordeaux), A. Sozzetti (INAF) Instrument working group coordinators O. Krause (MPIA), M. Ollivier (IAS), E. Pace (Un. Firenze), B. Swinyard (UCL) Science and Instrument working group members Ade P.A.R. (Cardiff ), Achilleos N. (UCL), Adriani A. (INAF), Agnor C. B. (QMUL), Afonso C. (MPIA), Allende Prieto C. (IAC), Bakos G. (CfA), Barber R. J. (UCL), Barlow M. (UCL), Bernath P. (Un. York), Bezard´ B. (LESIA), Borde´ P. (IAS), Brown L.R. (JPL), Cassan A. (IAP), Cavarroc C. (IAS), Ciaravella A. INAF), Cockell, C. O.U.), Coustenis A. (LESIA), Danielski C. (UCL), Decin L. (IvS), De Kok R. (SRON), Demangeon O. (IAS), Deroo P. (JPL), Doel P. (UCL), Drossart P. (LESIA), Fletcher L.N. (Oxford), Focardi M. (Un. Firenze), Forget F. (LMD), Fossey S. (UCL), Fouque´ P.