SS1718 Example Exam
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Constraints on the Habitability of Extrasolar Moons
Formation, Detection, and Characterization of Extrasolar Habitable Planets Proceedings IAU Symposium No. 293, 2012 c International Astronomical Union 2014 N. Haghighipour, ed. doi:10.1017/S1743921313012738 Constraints on the Habitability of Extrasolar Moons Ren´e Heller1 and Rory Barnes2,3 1 Leibniz Institute for Astrophysics Potsdam (AIP), An der Sternwarte 16, 14482 Potsdam email: [email protected] 2 University of Washington, Dept. of Astronomy, Seattle, WA 98195, USA 3 Virtual Planetary Laboratory, NASA, USA email: [email protected] Abstract. Detections of massive extrasolar moons are shown feasible with the Kepler space telescope. Kepler’s findings of about 50 exoplanets in the stellar habitable zone naturally make us wonder about the habitability of their hypothetical moons. Illumination from the planet, eclipses, tidal heating, and tidal locking distinguish remote characterization of exomoons from that of exoplanets. We show how evaluation of an exomoon’s habitability is possible based on the parameters accessible by current and near-future technology. Keywords. celestial mechanics – planets and satellites: general – astrobiology – eclipses 1. Introduction The possible discovery of inhabited exoplanets has motivated considerable efforts towards estimating planetary habitability. Effects of stellar radiation (Kasting et al. 1993; Selsis et al. 2007), planetary spin (Williams & Kasting 1997; Spiegel et al. 2009), tidal evolution (Jackson et al. 2008; Barnes et al. 2009; Heller et al. 2011), and composition (Raymond et al. 2006; Bond et al. 2010) have been studied. Meanwhile, Kepler’s high precision has opened the possibility of detecting extrasolar moons (Kipping et al. 2009; Tusnski & Valio 2011) and the first dedicated searches for moons in the Kepler data are underway (Kipping et al. -
Happy New Year! MEMBERSHIP? IT’S NEVER TOO LATE to JOIN!
Vol. 42, No. 1 January 2011 Great Work at Sleaford Renovations to the Sleaford Observatory warm-up shelter progressed rapidly last fall with Rick Huziak and Darrell Chatfield spending many days and evenings there. A wall was removed to the cold storage area to make more room, which meant extensive rewiring, insulating and refinishing. Other volunteers came to cut grass, paint, clean, do repairs, and provide food. Thank you to every one who helped to make Sleaford a more usable and pleasant site. Photo by Jeff Swick In This Issue: Membership Information / Bottle Drive / Officers of the Centre 2 U of S Observatory Hours / Light Pollution Abatement Website 2 Calendar of Events / Meeting Announcement 3 Solstice Eclipse – Tenho Tuomi, Norma Jensen plus others 4 ‘Tis the Night Before… 5 President’s Message – Jeff Swick 5 GOTO Telescopes are not for Beginners – Tenho Tuomi 6 Ask AstroNut 7 Saskatoon Centre Observers Group Notes – Larry Scott, Jeff Swick 8 The Royal Astronomical Society of Canada The Planets This Month – Murray Paulson 9 P.O. Box 317, RPO University The Messier, H-400 & H-400-II, FNGC, Bino, Lunar & EtU Club 10 Saskatoon, SK S7N 4J8 Editor’s Corner – Tenho Tuomi 10 WEBSITE: http://www.rasc.ca/saskatoon To view Saskatoon Skies in colour, see our Website: E •MAIL: [email protected] http://homepage.usask.ca/~ges125/rasc/newsletters.html TELEPHONE: (306) 373-3902 Happy New Year! MEMBERSHIP? IT’S NEVER TOO LATE TO JOIN! Regular: $80.00 /year Youth: $41.00 /year Associate: $33 /year The Saskatoon Centre operates on a one-year revolving membership. -
Case Fil Copy
NASA TECHNICAL NASA TM X-3511 MEMORANDUM CO >< CASE FIL COPY REPORTS OF PLANETARY GEOLOGY PROGRAM, 1976-1977 Compiled by Raymond Arvidson and Russell Wahmann Office of Space Science NASA Headquarters NATIONAL AERONAUTICS AND SPACE ADMINISTRATION • WASHINGTON, D. C. • MAY 1977 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. TMX3511 4. Title and Subtitle 5. Report Date May 1977 6. Performing Organization Code REPORTS OF PLANETARY GEOLOGY PROGRAM, 1976-1977 SL 7. Author(s) 8. Performing Organization Report No. Compiled by Raymond Arvidson and Russell Wahmann 10. Work Unit No. 9. Performing Organization Name and Address Office of Space Science 11. Contract or Grant No. Lunar and Planetary Programs Planetary Geology Program 13. Type of Report and Period Covered 12. Sponsoring Agency Name and Address Technical Memorandum National Aeronautics and Space Administration 14. Sponsoring Agency Code Washington, D.C. 20546 15. Supplementary Notes 16. Abstract A compilation of abstracts of reports which summarizes work conducted by Principal Investigators. Full reports of these abstracts were presented to the annual meeting of Planetary Geology Principal Investigators and their associates at Washington University, St. Louis, Missouri, May 23-26, 1977. 17. Key Words (Suggested by Author(s)) 18. Distribution Statement Planetary geology Solar system evolution Unclassified—Unlimited Planetary geological mapping Instrument development 19. Security Qassif. (of this report) 20. Security Classif. (of this page) 21. No. of Pages 22. Price* Unclassified Unclassified 294 $9.25 * For sale by the National Technical Information Service, Springfield, Virginia 22161 FOREWORD This is a compilation of abstracts of reports from Principal Investigators of NASA's Office of Space Science, Division of Lunar and Planetary Programs Planetary Geology Program. -
18Th EANA Conference European Astrobiology Network Association
18th EANA Conference European Astrobiology Network Association Abstract book 24-28 September 2018 Freie Universität Berlin, Germany Sponsors: Detectability of biosignatures in martian sedimentary systems A. H. Stevens1, A. McDonald2, and C. S. Cockell1 (1) UK Centre for Astrobiology, University of Edinburgh, UK ([email protected]) (2) Bioimaging Facility, School of Engineering, University of Edinburgh, UK Presentation: Tuesday 12:45-13:00 Session: Traces of life, biosignatures, life detection Abstract: Some of the most promising potential sampling sites for astrobiology are the numerous sedimentary areas on Mars such as those explored by MSL. As sedimentary systems have a high relative likelihood to have been habitable in the past and are known on Earth to preserve biosignatures well, the remains of martian sedimentary systems are an attractive target for exploration, for example by sample return caching rovers [1]. To learn how best to look for evidence of life in these environments, we must carefully understand their context. While recent measurements have raised the upper limit for organic carbon measured in martian sediments [2], our exploration to date shows no evidence for a terrestrial-like biosphere on Mars. We used an analogue of a martian mudstone (Y-Mars[3]) to investigate how best to look for biosignatures in martian sedimentary environments. The mudstone was inoculated with a relevant microbial community and cultured over several months under martian conditions to select for the most Mars-relevant microbes. We sequenced the microbial community over a number of transfers to try and understand what types microbes might be expected to exist in these environments and assess whether they might leave behind any specific biosignatures. -
Pluto and Charon
National Aeronautics and Space Administration 0 300,000,000 900,000,000 1,500,000,000 2,100,000,000 2,700,000,000 3,300,000,000 3,900,000,000 4,500,000,000 5,100,000,000 5,700,000,000 kilometers Pluto and Charon www.nasa.gov Pluto is classified as a dwarf planet and is also a member of a Charon’s orbit around Pluto takes 6.4 Earth days, and one Pluto SIGNIFICANT DATES group of objects that orbit in a disc-like zone beyond the orbit of rotation (a Pluto day) takes 6.4 Earth days. Charon neither rises 1930 — Clyde Tombaugh discovers Pluto. Neptune called the Kuiper Belt. This distant realm is populated nor sets but “hovers” over the same spot on Pluto’s surface, 1977–1999 — Pluto’s lopsided orbit brings it slightly closer to with thousands of miniature icy worlds, which formed early in the and the same side of Charon always faces Pluto — this is called the Sun than Neptune. It will be at least 230 years before Pluto history of the solar system. These icy, rocky bodies are called tidal locking. Compared with most of the planets and moons, the moves inward of Neptune’s orbit for 20 years. Kuiper Belt objects or transneptunian objects. Pluto–Charon system is tipped on its side, like Uranus. Pluto’s 1978 — American astronomers James Christy and Robert Har- rotation is retrograde: it rotates “backwards,” from east to west Pluto’s 248-year-long elliptical orbit can take it as far as 49.3 as- rington discover Pluto’s unusually large moon, Charon. -
Solar System
Lecture 2 Solar system Beibei Liu (刘倍⻉) Introduction to Astrophysics, 2019 What is planet? Definition of planet 1. It orbits the sun (central star) 2. It has sufficient mass to have its self-gravity to overcome rigid bodies force, so that in a hydrostatic equilibrium (near round and stable shape) 3. Its perturbations have cleared away other objects in the neighbourhood of its orbit. asteroid, comet, moon, pluto? Moon-Earth system: Tidal force Tidal locking (tidal synchronisation): spin period of the moon is equal to the orbital period of the Earth-Moon system (~28 days). Moon-Earth system: Tidal force Earth rotation is only 24 hours Earth slowly decreases its rotation, and moon’s orbital distance gradually increases Lunar and solar eclipse Blood moon, sun’s light refracted by earth’s atmosphere. Due to Rayleigh scattering, red color is easy to remain Solar system Terrestrial planets Gas giant planets ice giant planets Heat source of the planet 1. Gravitational contraction: release potential energy 2. Decay of radioactive isotope，such as potassium, uranium 3. Giant impacts, planetesimal accretion Melting and differentiation of planet interior Originally homogeneous material begin to segregate into layers of different chemical composition. Heavy elements sink into the centre. Interior of planets Relative core size Interior of planets Metallic hydrogen: high pressure, H2 dissociate into atoms and become electronic conducting. Magnetic field is generated in this layer. Earth interior layers Crust (rigid): granite and basalt Silicate mantle: flow and convection Fe-Ni core: T~4000-9000K Magnetic field is generated by electric currents due to large convective motion of molten metal in outer core and mantle Earth interior layers Tectonics motion Large scale movement of plates in Earth’s lithosphere. -
Culpeper Astronomy Club Meeting February 26, 2018 Overview
The Moon: Our Neighbor Culpeper Astronomy Club Meeting February 26, 2018 Overview • Introductions • Radio Astronomy: The Basics • The Moon • Constellations: Monoceros, Canis Major, Puppis • Observing Session (Tentative) Radio Astronomy • Stars, galaxies and gas clouds emit visible light as well as emissions from other parts of the electromagnetic spectrum • Includes radio waves, gamma rays, X- rays, and infrared radiation • Radio astronomy is the study of the universe through analysis of celestial objects' radio emission • the longest-wavelength, least energetic form of radiation on the electromagnetic spectrum • The first detection of radio waves from an astronomical object was in 1932 • Karl Jansky at Bell Telephone Laboratories observed radiation coming from the Milky Way Radio Astronomy • A radio telescope has three basic components: • One or more antennas pointed to the sky, to collect the radio waves • A receiver and amplifier to boost the very weak radio signal to a measurable level, and • A recorder to keep a record of the signal Radio Astronomy • Subsequent observations have identified a number of different sources of radio emission • Include stars and galaxies, as well as entirely new classes of objects, such as: • Radio galaxies: nuclei emit jets of high- velocity gas (near the speed of light) above and below the galaxy -- the jets interact with magnetic fields and emit radio signals • Quasars: distant objects powered by black holes a billion times as massive as our sun • Pulsars: the rapidly spinning remnants of supernova explosions -
Det.,Class.,Lunar Rilles 1
UNIVERSITÀ DEGLI STUDI DI PERUGIA DIPARTIMENTO DI FISICA E GEOLOGIA Corso di Laurea Magistrale in Scienze e Tecnologie Geologiche TESI DI LAUREA DETECTION, CLASSIFICATION, AND ANALYSIS OF SINUOUS RILLES ON THE NEAR-SIDE OF THE MOON Laureando: Relatore: SOFIA FIORUCCI LAURA MELELLI Correlatore: MARIA TERESA BRUNETTI Anno Accademico 2019/2020 “I have not failed. I've just found 10,000 ways that won't work.” ― Thomas A. Edison Table of Contents 1 Chapter 1: Introduction .................................................................................. 1 1.1 The Moon Mapping Project ..................................................................................... 1 1.2 Chang’E missions ...................................................................................................... 4 1.3 Moon Mapping Topics ............................................................................................. 9 1.3.1 Topic 1 –Map of the solar wind .............................................................................................. 10 1.3.2 Topic 2 – Geomorphologic map of the Moon ....................................................................... 11 1.3.3 Topic 3 – Data processing of Chang’E-1 mission ................................................................. 13 1.3.4 Topic 4 –Map of element distribution ................................................................................... 14 1.3.5 Topic 5 – 3D Visualization system ......................................................................................... 14 -
The Moon and Eclipses
The Moon and Eclipses ASTR 101 September 14, 2018 • Phases of the moon • Lunar month • Solar eclipses • Lunar eclipses • Eclipse seasons 1 Moon in the Sky An image of the Earth and the Moon taken from 1 million miles away. Diameter of Moon is about ¼ of the Earth. www.nasa.gov/feature/goddard/from-a-million-miles-away-nasa-camera-shows-moon-crossing-face-of-earth • Moonlight is reflected sunlight from the lunar surface. Moon reflects about 12% of the sunlight falling on it (ie. Moon’s albedo is 12%). • Dark features visible on the Moon are plains of old lava flows, formed by ancient volcanic eruptions – When Galileo looked at the Moon through his telescope, he thought those were Oceans, so he named them as Marias. – There is no water (or atmosphere) on the Moon, but still they are known as Maria – Through a telescope large number of craters, mountains and other geological features visible. 2 Moon Phases Sunlight Sunlight full moon New moon Sunlight Sunlight Quarter moon Crescent moon • Depending on relative positions of the Earth, the Sun and the Moon we see different amount of the illuminated surface of Moon. 3 Moon Phases first quarter waxing waxing gibbous crescent Orbit of the Moon Sunlight full moon new moon position on the orbit View from the Earth waning waning gibbous last crescent quarter 4 Sun Earthshine Moon light reflected from the Earth Earth in lunar sky is about 50 times brighter than the moon from Earth. “old moon" in the new moon's arms • Night (shadowed) side of the Moon is not completely dark. -
Abstract Volume
T I I II I II I I I rl I Abstract Volume LPI LPI Contribution No. 1097 II I II III I • • WORKSHOP ON MERCURY: SPACE ENVIRONMENT, SURFACE, AND INTERIOR The Field Museum Chicago, Illinois October 4-5, 2001 Conveners Mark Robinbson, Northwestern University G. Jeffrey Taylor, University of Hawai'i Sponsored by Lunar and Planetary Institute The Field Museum National Aeronautics and Space Administration Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 1097 Compiled in 2001 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication .... This volume may be cited as Author A. B. (2001)Title of abstract. In Workshop on Mercury: Space Environment, Surface, and Interior, p. xx. LPI Contribution No. 1097, Lunar and Planetary Institute, Houston. This report is distributed by ORDER DEPARTMENT Lunar and Planetary institute 3600 Bay Area Boulevard Houston TX 77058-1113, USA Phone: 281-486-2172 Fax: 281-486-2186 E-mail: order@lpi:usra.edu Please contact the Order Department for ordering information, i,-J_,.,,,-_r ,_,,,,.r pA<.><--.,// ,: Mercury Workshop 2001 iii / jaO/ Preface This volume contains abstracts that have been accepted for presentation at the Workshop on Mercury: Space Environment, Surface, and Interior, October 4-5, 2001. -
Final Thoughts
Contents Part I Common Themes 1. The Discovery of Extraterrestrial Worlds........................ 3 Introduction ...................................................................... 3 Radial Velocity: The Pull of Extrasolar Planets .............. 5 Transit: The Shadow of a Planet Cast by Its Star ........... 11 Microlensing: The Ghosts of Hidden Worlds .................. 20 Now You See It, Now You Don’t: Formalhaut B and Beyond ................................................ 24 What Worlds Await Us? ................................................... 27 Conclusions ...................................................................... 38 2. The Formation of Stars and Planets ................................ 39 Introduction ...................................................................... 39 Gravity’s Role in Star and Planet Formation .................. 40 The Effects of Neighboring Stars ..................................... 43 Brown Dwarfs ................................................................... 44 The Planets of Red Dwarfs ............................................... 46 Alternative Routes to Rome ............................................ 47 Energy and Life ................................................................. 50 Planetary Heat .................................................................. 51 Atmosphere, Hydrosphere and Biosphere ....................... 58 Conclusions ...................................................................... 60 3. Stellar Evolution Near the Bottom of the Main Sequence -
Widespread Effusive Volcanism on Mercury Likely Ended by About 3.5 Ga
PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Widespread effusive volcanism on Mercury likely 10.1002/2016GL069412 ended by about 3.5Ga Key Points: Paul K. Byrne1,2, Lillian R. Ostrach3, Caleb I. Fassett4, Clark R. Chapman5, Brett W. Denevi6, • – Crater size frequency distributions for 5,7 2,8 9,10 11 all major volcanic plains units on Alexander J. Evans , Christian Klimczak , Maria E. Banks , James W. Head , 2,7 Mercury are similar and Sean C. Solomon • None of these units has a model age younger than about 3.5 Ga 1Planetary Research Group, Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University at • Interior cooling and contraction likely Raleigh, Raleigh, North Carolina, USA, 2Department of Terrestrial Magnetism, Carnegie Institution of Washington, inhibited widespread plains volcanism Washington, District of Columbia, USA, 3Solar System Exploration Division, NASA Goddard Space Flight Center, Greenbelt, on Mercury thereafter Maryland, USA, 4Department of Astronomy, Mount Holyoke College, South Hadley, Massachusetts, USA, 5Department of Space Studies, Southwest Research Institute, Boulder, Colorado, USA, 6The Johns Hopkins University Applied Physics Laboratory, Laurel, Maryland, USA, 7Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA, Correspondence to: 8Department of Geology, University of Georgia, Athens, Georgia, USA, 9Center for Earth and Planetary Studies, Smithsonian P. K. Byrne, National Air and Space Museum, Washington, District of Columbia, USA, 10Planetary Science Institute, Tucson, Arizona, USA, [email protected] 11Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, Rhode Island, USA Citation: Byrne, P. K., L. R. Ostrach, C. I. Fassett, Abstract Crater size–frequency analyses have shown that the largest volcanic plains deposits on Mercury C.