Apollo 11: 50 Anni Sped
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Photometry of Asteroids: Lightcurves of 24 Asteroids Obtained in 1993–2005
ARTICLE IN PRESS Planetary and Space Science 55 (2007) 986–997 www.elsevier.com/locate/pss Photometry of asteroids: Lightcurves of 24 asteroids obtained in 1993–2005 V.G. Chiornya,b,Ã, V.G. Shevchenkoa, Yu.N. Kruglya,b, F.P. Velichkoa, N.M. Gaftonyukc aInstitute of Astronomy of Kharkiv National University, Sumska str. 35, 61022 Kharkiv, Ukraine bMain Astronomical Observatory, NASU, Zabolotny str. 27, Kyiv 03680, Ukraine cCrimean Astrophysical Observatory, Crimea, 98680 Simeiz, Ukraine Received 19 May 2006; received in revised form 23 December 2006; accepted 10 January 2007 Available online 21 January 2007 Abstract The results of 1993–2005 photometric observations for 24 main-belt asteroids: 24 Themis, 51 Nemausa, 89 Julia, 205 Martha, 225 Henrietta, 387 Aquitania, 423 Diotima, 505 Cava, 522 Helga, 543 Charlotte, 663 Gerlinde, 670 Ottegebe, 693 Zerbinetta, 694 Ekard, 713 Luscinia, 800 Kressmania, 1251 Hedera, 1369 Ostanina, 1427 Ruvuma, 1796 Riga, 2771 Polzunov, 4908 Ward, 6587 Brassens and 16541 1991 PW18 are presented. The rotation periods of nine of these asteroids have been determined for the first time and others have been improved. r 2007 Elsevier Ltd. All rights reserved. Keywords: Asteroids; Photometry; Lightcurve; Rotational period; Amplitude 1. Introduction telescope of the Crimean Astrophysics Observatory in Simeiz. Ground-based observations are the main source of knowledge about the physical properties of the asteroid 2. Observations and their reduction population. The photometric lightcurves are used to determine rotation periods, pole coordinates, sizes and Photometric observations of the asteroids were carried shapes of asteroids, as well as to study the magnitude-phase out in 1993–1994 using one-channel photoelectric photo- relation of different type asteroids. -
1950 Da, 205, 269 1979 Va, 230 1991 Ry16, 183 1992 Kd, 61 1992
Cambridge University Press 978-1-107-09684-4 — Asteroids Thomas H. Burbine Index More Information 356 Index 1950 DA, 205, 269 single scattering, 142, 143, 144, 145 1979 VA, 230 visual Bond, 7 1991 RY16, 183 visual geometric, 7, 27, 28, 163, 185, 189, 190, 1992 KD, 61 191, 192, 192, 253 1992 QB1, 233, 234 Alexandra, 59 1993 FW, 234 altitude, 49 1994 JR1, 239, 275 Alvarez, Luis, 258 1999 JU3, 61 Alvarez, Walter, 258 1999 RL95, 183 amino acid, 81 1999 RQ36, 61 ammonia, 223, 301 2000 DP107, 274, 304 amoeboid olivine aggregate, 83 2000 GD65, 205 Amor, 251 2001 QR322, 232 Amor group, 251 2003 EH1, 107 Anacostia, 179 2007 PA8, 207 Anand, Viswanathan, 62 2008 TC3, 264, 265 Angelina, 175 2010 JL88, 205 angrite, 87, 101, 110, 126, 168 2010 TK7, 231 Annefrank, 274, 275, 289 2011 QF99, 232 Antarctic Search for Meteorites (ANSMET), 71 2012 DA14, 108 Antarctica, 69–71 2012 VP113, 233, 244 aphelion, 30, 251 2013 TX68, 64 APL, 275, 292 2014 AA, 264, 265 Apohele group, 251 2014 RC, 205 Apollo, 179, 180, 251 Apollo group, 230, 251 absorption band, 135–6, 137–40, 145–50, Apollo mission, 129, 262, 299 163, 184 Apophis, 20, 269, 270 acapulcoite/ lodranite, 87, 90, 103, 110, 168, 285 Aquitania, 179 Achilles, 232 Arecibo Observatory, 206 achondrite, 84, 86, 116, 187 Aristarchus, 29 primitive, 84, 86, 103–4, 287 Asporina, 177 Adamcarolla, 62 asteroid chronology function, 262 Adeona family, 198 Asteroid Zoo, 54 Aeternitas, 177 Astraea, 53 Agnia family, 170, 198 Astronautica, 61 AKARI satellite, 192 Aten, 251 alabandite, 76, 101 Aten group, 251 Alauda family, 198 Atira, 251 albedo, 7, 21, 27, 185–6 Atira group, 251 Bond, 7, 8, 9, 28, 189 atmosphere, 1, 3, 8, 43, 66, 68, 265 geometric, 7 A- type, 163, 165, 167, 169, 170, 177–8, 192 356 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-1-107-09684-4 — Asteroids Thomas H. -
Detecting the Yarkovsky Effect Among Near-Earth Asteroids From
Detecting the Yarkovsky effect among near-Earth asteroids from astrometric data Alessio Del Vignaa,b, Laura Faggiolid, Andrea Milania, Federica Spotoc, Davide Farnocchiae, Benoit Carryf aDipartimento di Matematica, Universit`adi Pisa, Largo Bruno Pontecorvo 5, Pisa, Italy bSpace Dynamics Services s.r.l., via Mario Giuntini, Navacchio di Cascina, Pisa, Italy cIMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universits, UPMC Univ. Paris 06, Univ. Lille, 77 av. Denfert-Rochereau F-75014 Paris, France dESA SSA-NEO Coordination Centre, Largo Galileo Galilei, 1, 00044 Frascati (RM), Italy eJet Propulsion Laboratory/California Institute of Technology, 4800 Oak Grove Drive, Pasadena, 91109 CA, USA fUniversit´eCˆote d’Azur, Observatoire de la Cˆote d’Azur, CNRS, Laboratoire Lagrange, Boulevard de l’Observatoire, Nice, France Abstract We present an updated set of near-Earth asteroids with a Yarkovsky-related semi- major axis drift detected from the orbital fit to the astrometry. We find 87 reliable detections after filtering for the signal-to-noise ratio of the Yarkovsky drift esti- mate and making sure the estimate is compatible with the physical properties of the analyzed object. Furthermore, we find a list of 24 marginally significant detec- tions, for which future astrometry could result in a Yarkovsky detection. A further outcome of the filtering procedure is a list of detections that we consider spurious because unrealistic or not explicable with the Yarkovsky effect. Among the smallest asteroids of our sample, we determined four detections of solar radiation pressure, in addition to the Yarkovsky effect. As the data volume increases in the near fu- ture, our goal is to develop methods to generate very long lists of asteroids with reliably detected Yarkovsky effect, with limited amounts of case by case specific adjustments. -
Photometric Survey of 67 Near-Earth Objects S
A&A 615, A127 (2018) Astronomy https://doi.org/10.1051/0004-6361/201732154 & c ESO 2018 Astrophysics Photometric survey of 67 near-Earth objects S. Ieva1, E. Dotto1, E. Mazzotta Epifani1, D. Perna1,2, A. Rossi3, M. A. Barucci2, A. Di Paola1, R. Speziali1, M. Micheli1,4, E. Perozzi5, M. Lazzarin6, and I. Bertini6 1 INAF – Osservatorio Astronomico di Roma, Via Frascati 33, 00078 Monte Porzio Catone, Rome, Italy e-mail: [email protected] 2 LESIA – Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ. Paris 06, Univ. Paris Diderot, Sorbonne Paris Cité, 5 place Jules Janssen, 92195 Meudon, France 3 IFAC – CNR, Via Madonna del Piano 10, 50019 Sesto Fiorentino, Firenze, Italy 4 ESA SSA-NEO Coordination Centre„ Largo Galileo Galilei 1, 00044 Frascati (RM), Italy 5 Agenzia Spaziale Italiana, Via del Politecnico 1, 00100 Rome, Italy 6 Department of Physics and Astronomy “Galileo Galilei”, University of Padova, Vicolo dell’Osservatorio 3, 35122 Padova, Italy Received 23 October 2017 / Accepted 29 March 2018 ABSTRACT Context. The near-Earth object (NEO) population is a window into the original conditions of the protosolar nebula, and has the potential to provide a key pathway for the delivery of water and organics to the early Earth. In addition to delivering the crucial ingredients for life, NEOs can pose a serious hazard to humanity since they can impact the Earth. To properly quantify the impact risk, physical properties of the NEO population need to be studied. Unfortunately, NEOs have a great variation in terms of mitigation- relevant quantities (size, albedo, composition, etc.) and less than 15% of them have been characterized to date. -
Neodys (And Astdys and Priority List) Data Provision
NEODyS (and AstDyS and Priority List) Data Provision Fabrizio Bernardi CEO of SpaceDyS What is NEODyS • NEODyS is a web based service and stands for Near Earth Objects Dynamic Site: h@p://newton.dm.unipi.it/neodys • NEODyS provides informaon on the IMPACT PROBABILITY of Near Earth Objects (NEOs), typically for an horizon of 100 years • The most important output is the Risk Page: h@p://newton.dm.unipi.it/neodys2/index.php?pc=4.0 where a list of NEOs (459 on Nov 17th) with some chances of hing the Earth within the next century is posted for the public • Only JPL@NASA provides a similar service with SENTRY • NEODyS team has a technological leadership in Europe (and world) NEODyS background • NEODyS was born in 1999 at the Dep. of Mathemacs of the University of Pisa (Italy), within the CelesDal Mechanics Group (CMG) lead by Prof. Andrea Milani • The main moDvaon was the absence of a rigorous and systemac method for compuDng on a daily basis the probability that an asteroid is hing the Earth • The 1997XF11 case was a PR disaster, just for the lack of a well established system to perform such computaons NEODyS daily acDviDes • Since 1999 NEODyS is processing astrometric data of Near Earth Objects (NEOs) provided by the Minor Planet Center, the official enDty supported by the Internaonal Astronomical Union (IAU) that manages all the asteroids observaons and the official catalog of asteroids • The data are sent to NEODyS either by email or via web, through the Minor Planet Electronic Circulars (MPECs) • MPECs: – DOU à Daily Orbit Update: new observaons -
Near-Earth Objects
Near-Earth Objects 12/06/96 shows an elongated object about seen here in a NEAR spacecraft image 4.5 kilometers in extent. Veverka et al. (2000), Science, 289, Ostro et al. (1999), Icarus, 137: pp. 122-139. pp. 2088-2097. THE NEAR EARTH OBJECT POPULATION Near-Earth objects are an important area of study because they are relatively primitive bodies left over from the early solar system formation process, they can be utilized as raw materials for building future structures and habitats within the inner solar system, and their rare, but potentially catastrophic, collisions with Earth make them potential hazards. A comprehensive search for near-Earth objects (NEOs) not only ensures that there will be no surprises from Earth threatening objects but there will be new discoveries. During future close Earth approaches, these objects can be studied via ground-based programs including radar "imaging" characterizations and Earth orbital satellite observations (e.g., Hubble Space Telescope). In addition, these NE0 discoveries will provide future mission targets that are among the most accessible in terms of spacecraft energy requirements. Indeed, many near-Earth asteroids present easier rendezvous and landing opportunities than Earth's own Moon. While the vast majority of the rocky asteroids reside between the orbits of Mars and Jupiter and almost all the icy comets are resident in the so-called Kuiper belt and Oort cloud in the outer solar system, a significant number of these bodies reside in the Earth's neighborhood. Near-Earth asteroids and near-Earth comets make up the population of so-called near-Earth objects (NEOs). -
4 IAA Plane Etary Defen Nse C Onfer Rencee
4th IAA Planetary Defense Conference Assessing Impact Risk & Managing Response 13‐17 April 2015 Frascati, Italy PROGRAM 2015 IAA Planetary Defense Conference: PROGRAM Assessing Impact Risk & Managing Response PDC 2015 DAY April 13, 2015 1 0800 REGISTRATION 0900 WELCOMING REMARKS 0915 IAA‐PDC‐15‐00‐01 KEYNOTE: 15.02.2013 Chelyabinsk. Are we ready for O. Atkov a recurrence? 0945 BREAK SESSION 1: INTERNATIONAL PROGRAMS & ACTIVITIES Session Chairs: Detlef Koschny, Lindley Johnson 1000 IAA‐PDC‐15‐01‐01 The Near‐Earth Object Segment Of ESA’s SSA G. Drolshagen Programme 1020 IAA‐PDC‐15‐01‐02 Astronomical Aspects Of Building A System For B. Shustov Detecting And Monitoring Hazardous Space Objects 1040 IAA‐PDC‐15‐01‐03 The Achievements Of The NEOShield Project And The A. Harris (DLR) Promise Of NEOShield‐2 1100 IAA‐PDC‐15‐01‐04 Recent Enhancements To The NEO Observations L. Johnson Program: Implications For Planetary Defense 1120 IAA‐PDC‐15‐01‐05 Asia‐Pacific Asteroid Observation Network M. Yoshikawa 1140 INJECT 1: HYPOTHETICAL THREAT 1200 LUNCH SESSION 2: DISCOVERY, TRACKING, CHARACTERIZATION Session Chairs: Alan Harris (US), Alan Harris (DLR), Line Drube 1315 IAA‐PDC‐15‐02‐01 PAN‐STARRS Search For Near Earth Objects R. Wainscoat 1330 IAA‐PDC‐15‐02‐02 Design Characteristics Of An Optimized Ground S. Larson Based NEO Survey Telescope 1345 IAA‐PDC‐15‐02‐03 ATLAS – Warning For Impending Impact J. Tonry 1400 IAA‐PDC‐15‐02‐04 Sentinel Mission For Planetary Defense H. Reitsema 1415 IAA‐PDC‐15‐02‐05 Building On The NEOWISE Legacy With NEOCAM, The A. -
Aqueous Alteration on Main Belt Primitive Asteroids: Results from Visible Spectroscopy1
Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 1 LESIA, Observatoire de Paris, CNRS, UPMC Univ Paris 06, Univ. Paris Diderot, 5 Place J. Janssen, 92195 Meudon Pricipal Cedex, France 2 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris Cedex 13 3 Department of Physics and Astronomy of the University of Padova, Via Marzolo 8 35131 Padova, Italy Submitted to Icarus: November 2013, accepted on 28 January 2014 e-mail: [email protected]; fax: +33145077144; phone: +33145077746 Manuscript pages: 38; Figures: 13 ; Tables: 5 Running head: Aqueous alteration on primitive asteroids Send correspondence to: Sonia Fornasier LESIA-Observatoire de Paris arXiv:1402.0175v1 [astro-ph.EP] 2 Feb 2014 Batiment 17 5, Place Jules Janssen 92195 Meudon Cedex France e-mail: [email protected] 1Based on observations carried out at the European Southern Observatory (ESO), La Silla, Chile, ESO proposals 062.S-0173 and 064.S-0205 (PI M. Lazzarin) Preprint submitted to Elsevier September 27, 2018 fax: +33145077144 phone: +33145077746 2 Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 Abstract This work focuses on the study of the aqueous alteration process which acted in the main belt and produced hydrated minerals on the altered asteroids. Hydrated minerals have been found mainly on Mars surface, on main belt primitive asteroids and possibly also on few TNOs. These materials have been produced by hydration of pristine anhydrous silicates during the aqueous alteration process, that, to be active, needed the presence of liquid water under low temperature conditions (below 320 K) to chemically alter the minerals. -
Yarkovsky Effect Detection and Updated Impact Hazard Assessment
Yarkovsky effect detection and updated impact hazard assessment for Near-Earth Asteroid (410777) 2009 FD Alessio Del Vignaa,b, Javier Roac, Davide Farnocchiac, Marco Michelid,e, Dave Tholeni, Francesca Guerraa, Federica Spotof, Giovanni Battista Valsecchig,h aSpace Dynamics Services s.r.l., via Mario Giuntini, Navacchio di Cascina, Pisa, Italy bDipartimento di Matematica, Universit`adi Pisa, Largo Bruno Pontecorvo 5, Pisa, Italy cJet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, 91109 CA, USA dESA NEO Coordination Centre, Largo Galileo Galilei, 1, 00044 Frascati (RM), Italy eINAF - Osservatorio Astronomico di Roma, Via Frascati, 33, 00040 Monte Porzio Catone (RM), Italy fUniversit´eC^oted'Azur, Observatoire de la C^oted'Azur, CNRS, Laboratoire Lagrange, Boulevard de l'Observatoire, Nice, France gIAPS-INAF, via Fosso del Cavaliere 100, 00133 Roma, Italy hIFAC-CNR, via Madonna del Piano 10, 50019 Sesto Fiorentino, Italy iInstitute for Astronomy, University of Hawaii, 2680 Woodlawn Drive, Honolulu, HI 96822, USA Abstract Near-Earth Asteroid (410777) 2009 FD is a potentially hazardous asteroid with possible (though unlikely) impacts on Earth at the end of the 22nd century. The astrometry collected during the 2019 apparition provides information on the trajectory of (410777) by constraining the Yarkovsky effect, which is the main source of uncertainty for future predictions, and informing the impact hazard assessment. We included the Yarkovsky effect in the force model and estimated its magnitude from the fit to the (410777) optical and radar astrometric data. We performed the (410777) hazard assessment over 200 years by using two independent approaches: the NEODyS group adopted a generalisation of the Line Of Variations method in a 7-dimensional space, whereas the JPL team resorted to the Multilayer Clustered Sampling technique. -
EPSC2017-881-1, 2017 European Planetary Science Congress 2017 Eeuropeapn Planetarsy Science Ccongress C Author(S) 2017
EPSC Abstracts Vol. 11, EPSC2017-881-1, 2017 European Planetary Science Congress 2017 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2017 Impact Effects Calculator. Orbital Parameters. S.A. Naroenkov(2), D.O. Glazachev(1), A.P. Kartashova(2), I.S. Turuntaev(1), V.V. Svetsov (1), V.V. Shuvalov(1), O.P. Popova(1) and E.D. Podobnaya(1) (1)Institute for Dynamics of Geospheres RAS, Moscow, Russia ([email protected] / Fax: +7-499-1376511), (2)Institute of Astronomy RAS, Moscow, Russia Abstract the ground, formation of craters and plumes are simulated. Results obtained in these simulations will Next-generation Impact Calculator for quick be used to get interpolations for rapid assessment of assessment of impact consequences is being prepared. the impact effects. As an example, in the calculator [3] The estimates of impact effects are revised. The thermal damage from crater-forming impacts is possibility to manipulate with the orbital parameters considered based on nuclear explosions results and and to determine impact point is included. crater plume luminous efficiency estimates but the radiation from the objects decelerated in the atmosphere is not included [3]. For our calculator, the Introduction systematic modeling of the entry of asteroidal and The population of near-Earth objects (NEOs, both cometary bodies of various sizes (20-3000 m), asteroids and comets) contains a wide variety of including the determination of thermal fluxes and bodies with diverse physical and dynamical properties, exposures, was carried out [5], and scaling relations and presents a permanent threat to our civilization [1]. for thermal fluxes on the ground were found [6]. -
An Innovative Solution to NASA's NEO Impact Threat Mitigation Grand
Final Technical Report of a NIAC Phase 2 Study December 9, 2014 NASA Grant and Cooperative Agreement Number: NNX12AQ60G NIAC Phase 2 Study Period: 09/10/2012 – 09/09/2014 An Innovative Solution to NASA’s NEO Impact Threat Mitigation Grand Challenge and Flight Validation Mission Architecture Development PI: Dr. Bong Wie, Vance Coffman Endowed Chair Professor Asteroid Deflection Research Center Department of Aerospace Engineering Iowa State University, Ames, IA 50011 email: [email protected] (515) 294-3124 Co-I: Brent Barbee, Flight Dynamics Engineer Navigation and Mission Design Branch (Code 595) NASA Goddard Space Flight Center Greenbelt, MD 20771 email: [email protected] (301) 286-1837 Graduate Research Assistants: Alan Pitz (M.S. 2012), Brian Kaplinger (Ph.D. 2013), Matt Hawkins (Ph.D. 2013), Tim Winkler (M.S. 2013), Pavithra Premaratne (M.S. 2014), Sam Wagner (Ph.D. 2014), George Vardaxis, Joshua Lyzhoft, and Ben Zimmerman NIAC Program Executive: Dr. John (Jay) Falker NIAC Program Manager: Jason Derleth NIAC Senior Science Advisor: Dr. Ronald Turner NIAC Strategic Partnerships Manager: Katherine Reilly Contents 1 Hypervelocity Asteroid Intercept Vehicle (HAIV) Mission Concept 2 1.1 Introduction ...................................... 2 1.2 Overview of the HAIV Mission Concept ....................... 6 1.3 Enabling Space Technologies for the HAIV Mission . 12 1.3.1 Two-Body HAIV Configuration Design Tradeoffs . 12 1.3.2 Terminal Guidance Sensors/Algorithms . 13 1.3.3 Thermal Protection and Shield Issues . 14 1.3.4 Nuclear Fuzing Mechanisms ......................... 15 2 Planetary Defense Flight Validation (PDFV) Mission Design 17 2.1 The Need for a PDFV Mission ............................ 17 2.2 Preliminary PDFV Mission Design by the MDL of NASA GSFC . -
Small Near-Earth Asteroids As a Source of Meteorites
Small Near-Earth Asteroids as a Source of Meteorites Jiří Borovička and Pavel Spurný Astronomical Institute of the Czech Academy of Sciences Peter Brown University of Western Ontario __________________________________________________________________________ Small asteroids intersecting Earth’s orbit can deliver extraterrestrial rocks to the Earth, called meteorites. This process is accompanied by a luminous phenomena in the atmosphere, called bolides or fireballs. Observations of bolides provide pre-atmospheric orbits of meteorites, physical and chemical properties of small asteroids, and the flux (i.e. frequency of impacts) of bodies at the Earth in the centimeter to decameter size range. In this chapter we explain the processes occurring during the penetration of cosmic bodies through the atmosphere and review the methods of bolide observations. We compile available data on the fireballs associated with 22 instrumentally observed meteorite falls. Among them are the heterogeneous falls Almahata Sitta (2008 TC3) and Benešov, which revolutionized our view on the structure and composition of small asteroids, the Příbram-Neuschwanstein orbital pair, carbonaceous chondrite meteorites with orbits on the asteroid-comet boundary, and the Chelyabinsk fall, which produced a damaging blast wave. While most meteoroids disrupt into fragments during atmospheric flight, the Carancas meteoroid remained nearly intact and caused a crater-forming explosion on the ground. 1. INTRODUCTION Well before the first asteroid was discovered, people unknowingly had asteroid samples in their hands. Could stones fall from the sky? For many centuries, the official answer was: NO. Only at the end of the 18th century and the beginning of the 19th century did the evidence that rocks did fall from the sky become so overwhelming that this fact was accepted by the scientific community.