Particles and Fields in the Interplanetary Medium M
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From: "MESSENGER, SCOTT R
The Starting Materials In: Meteorites and the Early Solar System II S. Messenger Johnson Space Center S. Sandford Ames Research Center D. Brownlee University of Washington Combined information from observations of interstellar clouds and star forming regions and studies of primitive solar system materials give a first order picture of the starting materials for the solar system’s construction. At the earliest stages, the presolar dust cloud was comprised of stardust, refractory organic matter, ices, and simple gas phase molecules. The nature of the starting materials changed dramatically together with the evolving solar system. Increasing temperatures and densities in the disk drove molecular evolution to increasingly complex organic matter. High temperature processes in the inner nebula erased most traces of presolar materials, and some fraction of this material is likely to have been transported to the outermost, quiescent portions of the disk. Interplanetary dust particles thought to be samples of Kuiper Belt objects probably contain the least altered materials, but also contain significant amounts of solar system materials processed at high temperatures. These processed materials may have been transported from the inner, warmer portions of the disk early in the active accretion phase. 1. Introduction A principal constraint on the formation of the Solar System was the population of starting materials available for its construction. Information on what these starting materials may have been is largely derived from two approaches, namely (i) the examination of other nascent stellar systems and the dense cloud environments in which they form, and (ii) the study of minimally altered examples of these starting materials that have survived in ancient Solar System materials. -
Mars Express Orbiter Radio Science
MaRS: Mars Express Orbiter Radio Science M. Pätzold1, F.M. Neubauer1, L. Carone1, A. Hagermann1, C. Stanzel1, B. Häusler2, S. Remus2, J. Selle2, D. Hagl2, D.P. Hinson3, R.A. Simpson3, G.L. Tyler3, S.W. Asmar4, W.I. Axford5, T. Hagfors5, J.-P. Barriot6, J.-C. Cerisier7, T. Imamura8, K.-I. Oyama8, P. Janle9, G. Kirchengast10 & V. Dehant11 1Institut für Geophysik und Meteorologie, Universität zu Köln, D-50923 Köln, Germany Email: [email protected] 2Institut für Raumfahrttechnik, Universität der Bundeswehr München, D-85577 Neubiberg, Germany 3Space, Telecommunication and Radio Science Laboratory, Dept. of Electrical Engineering, Stanford University, Stanford, CA 95305, USA 4Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91009, USA 5Max-Planck-Instuitut für Aeronomie, D-37189 Katlenburg-Lindau, Germany 6Observatoire Midi Pyrenees, F-31401 Toulouse, France 7Centre d’etude des Environnements Terrestre et Planetaires (CETP), F-94107 Saint-Maur, France 8Institute of Space & Astronautical Science (ISAS), Sagamihara, Japan 9Institut für Geowissenschaften, Abteilung Geophysik, Universität zu Kiel, D-24118 Kiel, Germany 10Institut für Meteorologie und Geophysik, Karl-Franzens-Universität Graz, A-8010 Graz, Austria 11Observatoire Royal de Belgique, B-1180 Bruxelles, Belgium The Mars Express Orbiter Radio Science (MaRS) experiment will employ radio occultation to (i) sound the neutral martian atmosphere to derive vertical density, pressure and temperature profiles as functions of height to resolutions better than 100 m, (ii) sound -
A Deep Learning Framework for Solar Phenomena Prediction
FlareNet: A Deep Learning Framework for Solar Phenomena Prediction FDL 2017 Solar Storm Team: Sean McGregor1, Dattaraj Dhuri1,2, Anamaria Berea1,3, and Andrés Muñoz-Jaramillo1,4 1NASA’s 2017 Frontier Development Laboratory 2Tata Institute of Fundamental Research (TIFR), Mumbai, India 3Center for Complexity in Business, University of Maryland, College Park, MD, USA 4SouthWest Research Institute, Boulder, CO, USA Abstract Solar activity can interfere with the normal operation of GPS satellites, the power grid, and space operations, but inadequate predictive models mean we have little warning for the arrival of newly disruptive solar activity. Petabytes of data col- lected from satellite instruments aboard the Solar Dynamics Observatory (SDO) provide a high-cadence, high-resolution, and many-channeled dataset of solar phenomena. Several challenging deep learning problems may be derived from the data, including space weather forecasting (i.e., solar flares, solar energetic particles, and coronal mass ejections). This work introduces a software framework, FlareNet, for experimentation within these problems. FlareNet includes compo- nents for the downloading and management of SDO data, visualization, and rapid experimentation. The system architecture is built to enable collaboration between heliophysicists and machine learning researchers on the topics of image regres- sion, image classification, and image segmentation. We specifically highlight the problem of solar flare prediction and offer insights from preliminary experiments. 1 Introduction The violent release of solar magnetic energy – collectively referred to as “space weather" – is responsible for a variety of phenomena that can disrupt technological assets. In particular, solar flares (sudden brightenings of the solar corona) and coronal mass ejections (CMEs; the violent release of solar plasma) can disrupt long-distance communications, reduce Global Positioning System (GPS) accuracy, degrade satellites, and disrupt the power grid [5]. -
Asteroidal Dust 423
Dermott et al.: Asteroidal Dust 423 Asteroidal Dust Stanley F. Dermott University of Florida Daniel D. Durda Southwest Research Institute Keith Grogan NASA Goddard Space Flight Center Thomas J. J. Kehoe University of Florida There is good evidence that the high-speed, porous, anhydrous chondritic interplanetary dust particles (IDPs) collected in Earth’s stratosphere originated from short-period comets. How- ever, by considering the structure of the solar-system dust bands discovered by IRAS, we are able to show that asteroidal collisions are probably the dominant source of particles in the zodiacal cloud. It follows that a significant and probably the dominant fraction of the IDPs collected in Earth’s stratosphere also originated from asteroids. IDPs are the most primitive particles in the inner solar system and represent a class of material quite different from that in our meteorite collections. The structure, mineralogy, and high C content of IDPs dictate that they cannot have originated from the grinding down of known meteorite types. We argue that the asteroidal IDPs were probably formed as a result of prolonged mechanical mixing in the deep regoliths of asteroidal rubble piles in the outer main belt. 1. INTRODUCTION information on the nature of the particles in the preplanetary solar nebula (Bradley, 1999). Observations of microcraters In our collections on Earth, we have an abundance of on the Long Duration Exposure Facility (LDEF) confirmed meteorite samples from three major sources of extraterres- that each year Earth accretes 3 × 107 kg of dust particles, a trial material: the asteroid belt, the Moon, and Mars. Some mass influx ~100× greater than the influx associated with of the source bodies of these meteorites have experienced the much larger meteorites that have masses between 100 g major physical, chemical, and mineralogical changes since and 1000 kg. -
+ New Horizons
Media Contacts NASA Headquarters Policy/Program Management Dwayne Brown New Horizons Nuclear Safety (202) 358-1726 [email protected] The Johns Hopkins University Mission Management Applied Physics Laboratory Spacecraft Operations Michael Buckley (240) 228-7536 or (443) 778-7536 [email protected] Southwest Research Institute Principal Investigator Institution Maria Martinez (210) 522-3305 [email protected] NASA Kennedy Space Center Launch Operations George Diller (321) 867-2468 [email protected] Lockheed Martin Space Systems Launch Vehicle Julie Andrews (321) 853-1567 [email protected] International Launch Services Launch Vehicle Fran Slimmer (571) 633-7462 [email protected] NEW HORIZONS Table of Contents Media Services Information ................................................................................................ 2 Quick Facts .............................................................................................................................. 3 Pluto at a Glance ...................................................................................................................... 5 Why Pluto and the Kuiper Belt? The Science of New Horizons ............................... 7 NASA’s New Frontiers Program ........................................................................................14 The Spacecraft ........................................................................................................................15 Science Payload ...............................................................................................................16 -
Urea, Glycolic Acid, and Glycerol in an Organic Residue Produced by Ultraviolet Irradiation of Interstellar=Pre-Cometary Ice Analogs
ASTROBIOLOGY Volume 10, Number 2, 2010 ª Mary Ann Liebert, Inc. DOI: 10.1089=ast.2009.0358 Urea, Glycolic Acid, and Glycerol in an Organic Residue Produced by Ultraviolet Irradiation of Interstellar=Pre-Cometary Ice Analogs Michel Nuevo,1,2 Jan Hendrik Bredeho¨ft,3 Uwe J. Meierhenrich,4 Louis d’Hendecourt,1 and Wolfram H.-P. Thiemann3 Abstract More than 50 stable organic molecules have been detected in the interstellar medium (ISM), from ground-based and onboard-satellite astronomical observations, in the gas and solid phases. Some of these organics may be prebiotic compounds that were delivered to early Earth by comets and meteorites and may have triggered the first chemical reactions involved in the origin of life. Ultraviolet irradiation of ices simulating photoprocesses of cold solid matter in astrophysical environments have shown that photochemistry can lead to the formation of amino acids and related compounds. In this work, we experimentally searched for other organic molecules of prebiotic interest, namely, oxidized acid labile compounds. In a setup that simulates conditions relevant to the ISM and Solar System icy bodies such as comets, a condensed CH3OH:NH3 ¼ 1:1 ice mixture was UV irradiated at *80 K. The molecular constituents of the nonvolatile organic residue that remained at room temperature were separated by capillary gas chromatography and identified by mass spectrometry. Urea, glycolic acid, and glycerol were detected in this residue, as well as hydroxyacetamide, glycerolic acid, and glycerol amide. These organics are interesting target molecules to be searched for in space. Finally, tentative mechanisms of formation for these compounds under interstellar=pre-cometary conditions are proposed. -
Mariner to Mercury, Venus and Mars
NASA Facts National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109 Mariner to Mercury, Venus and Mars Between 1962 and late 1973, NASA’s Jet carry a host of scientific instruments. Some of the Propulsion Laboratory designed and built 10 space- instruments, such as cameras, would need to be point- craft named Mariner to explore the inner solar system ed at the target body it was studying. Other instru- -- visiting the planets Venus, Mars and Mercury for ments were non-directional and studied phenomena the first time, and returning to Venus and Mars for such as magnetic fields and charged particles. JPL additional close observations. The final mission in the engineers proposed to make the Mariners “three-axis- series, Mariner 10, flew past Venus before going on to stabilized,” meaning that unlike other space probes encounter Mercury, after which it returned to Mercury they would not spin. for a total of three flybys. The next-to-last, Mariner Each of the Mariner projects was designed to have 9, became the first ever to orbit another planet when two spacecraft launched on separate rockets, in case it rached Mars for about a year of mapping and mea- of difficulties with the nearly untried launch vehicles. surement. Mariner 1, Mariner 3, and Mariner 8 were in fact lost The Mariners were all relatively small robotic during launch, but their backups were successful. No explorers, each launched on an Atlas rocket with Mariners were lost in later flight to their destination either an Agena or Centaur upper-stage booster, and planets or before completing their scientific missions. -
The Analysis of Interplanetary Dust Particles
WORKSHOP ON THE ANALYSIS OF INTERPLANETARY DUST PARTICLES LPI Technical Report Number 94-02 Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPIITR--94-02 WORKSHOP ON THE ANALYSIS OF INTERPLANETARY DUST PARTICLES Edited by M. Zolensky Held at Lunar and Planetary Institute May 15-17, 1993 Sponsored by Lunar and Planetary Institute Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Technical Report Number 94-02 LPIITR--94-02 Compiled in 1994 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the University 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 report may be cited as M. Zolensky, ed. (1994) Workshop on the Analysis ofInterplanetary Dust Particles. LPI Tech. Rpt. 94-02, Lunar and Planetary Institute, Houston. 62 pp. This report is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Mail order requestors will be invoiced for the cost of shipping and handling. Cover. Backscattered electron image of a hydrated, chondritic interplanetary dust particle, measuring 17).1m across. LPT Technical Report 94-02 iii Program Saturday, May 15, 1993 7:30-8:30 a.m. Registration and Continental Breakfast 8:30 a.m.-5:00 p.m. INVITED PRESENTATIONS AND DISCUSSION TOPICS An Overview ofthe Origin and Role ofDust in the Early Solar System D. -
Space Weather Lecture 2: the Sun and the Solar Wind
Space Weather Lecture 2: The Sun and the Solar Wind Elena Kronberg (Raum 442) [email protected] Elena Kronberg: Space Weather Lecture 2: The Sun and the Solar Wind 1 / 39 The radiation power is '1.5 kW·m−2 at the distance of the Earth The Sun: facts Age = 4.5×109 yr Mass = 1.99×1030 kg (330,000 Earth masses) Radius = 696,000 km (109 Earth radii) Mean distance from Earth (1AU) = 150×106 km (215 solar radii) Equatorial rotation period = '25 days Mass loss rate = 109 kg·s−1 It takes sunlight 8 min to reach the Earth Elena Kronberg: Space Weather Lecture 2: The Sun and the Solar Wind 2 / 39 The Sun: facts Age = 4.5×109 yr Mass = 1.99×1030 kg (330,000 Earth masses) Radius = 696,000 km (109 Earth radii) Mean distance from Earth (1AU) = 150×106 km (215 solar radii) Equatorial rotation period = '25 days Mass loss rate = 109 kg·s−1 It takes sunlight 8 min to reach the Earth The radiation power is '1.5 kW·m−2 at the distance of the Earth Elena Kronberg: Space Weather Lecture 2: The Sun and the Solar Wind 2 / 39 The Solar interior Core: 1H +1 H !2 H + e+ + n + 0.42 MeV 1H +2 He !3 H + g + 5.5 MeV 3He +3 He !4 He + 21H + 12.8 MeV The radiative zone: electromagnetic radiation transports energy outwards The convection zone: energy is transported by convection The photosphere – layer which emits visible light The chromosphere is the Sun’s atmosphere. -
DSCOVR Magnetometer Observations Adam Szabo, Andriy Koval NASA Goddard Space Flight Center
DSCOVR Magnetometer Observations Adam Szabo, Andriy Koval NASA Goddard Space Flight Center 1 Locations of the Instruments Faraday Cup EPIC Omni Antenna Star Tracker Thruster Modules Digital Sun Sensor Electron Spectrometer +Z +X Magnetometer +Y 2 Goddard Fluxgate Magnetometer The Fluxgate Magnetometer measures the interplanetary vector magnetic field It is located at the tip of a 4.0 m boom to minimize the effect of spacecraft fields Requirement Value Method Performance Magnetometer Range 0.1-100 nT Test 0.004-65,500 nT Accuracy +/- 1 nT Measured +/- 0.2 nT Cadence 1 min Measured 50 vector/sec 3 Pre-flight Calibration • Determined the magnetometer zero levels, scale factors, and magnetometer orthogonalization matrix. • Determined the spacecraft generated magnetic fields – Subsystem level magnetic tests. Reaction wheels, major source of dynamic field, were shielded – Spacecraft unpowered magnetic test in the GSFC 40’ magnetic facility In-Flight Boom Deployment • Nominal deployment on 2/15/15, seen as 4.4 rotations in the magnetometer components Mostly spacecraft Boom deployment Interplanetary magnetic field induced fields 5 Alfven Waves in the Solar Wind • The solar wind contains magnetic field rotations that preserve the magnitude of the field, so called Alfven waves. • Alfven waves are ubiquitous and are possible to identify with automated routines. • Systematic deviations from a constant field magnitude during these waves are an indication of spacecraft induced offsets. • Minimizing the deviations with slowly changing offsets allows in-flight calibrations. 6 In-Flight Magnetometer Calibrations Z Magnetometer Zero Offsets X • X axis Roll and Z axis Slew data is Y consistent with ground calibration estimates X • Independent zero offset determination by rolls, slews and using solar wind Alfvenicity give consistent values Z • Time variation is consistent with yearly orbital change. -
Multi-Spacecraft Analysis of the Solar Coronal Plasma
Multi-spacecraft analysis of the solar coronal plasma Von der Fakultät für Elektrotechnik, Informationstechnik, Physik der Technischen Universität Carolo-Wilhelmina zu Braunschweig zur Erlangung des Grades einer Doktorin der Naturwissenschaften (Dr. rer. nat.) genehmigte Dissertation von Iulia Ana Maria Chifu aus Bukarest, Rumänien eingereicht am: 11.02.2015 Disputation am: 07.05.2015 1. Referent: Prof. Dr. Sami K. Solanki 2. Referent: Prof. Dr. Karl-Heinz Glassmeier Druckjahr: 2016 Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.d-nb.de abrufbar. Dissertation an der Technischen Universität Braunschweig, Fakultät für Elektrotechnik, Informationstechnik, Physik ISBN uni-edition GmbH 2016 http://www.uni-edition.de © Iulia Ana Maria Chifu This work is distributed under a Creative Commons Attribution 3.0 License Printed in Germany Vorveröffentlichung der Dissertation Teilergebnisse aus dieser Arbeit wurden mit Genehmigung der Fakultät für Elektrotech- nik, Informationstechnik, Physik, vertreten durch den Mentor der Arbeit, in folgenden Beiträgen vorab veröffentlicht: Publikationen • Mierla, M., Chifu, I., Inhester, B., Rodriguez, L., Zhukov, A., 2011, Low polarised emission from the core of coronal mass ejections, Astronomy and Astrophysics, 530, L1 • Chifu, I., Inhester, B., Mierla, M., Chifu, V., Wiegelmann, T., 2012, First 4D Recon- struction of an Eruptive Prominence -
An Approach to Magnetic Cleanliness for the Psyche Mission M
An Approach to Magnetic Cleanliness for the Psyche Mission M. de Soria-Santacruz J. Ream K. Ascrizzi ([email protected]), ([email protected]), ([email protected]) M. Soriano R. Oran University of Michigan Ann Arbor ([email protected]), ([email protected]), 500 S State St O. Quintero B. P. Weiss Ann Arbor, MI 48109 ([email protected]), ([email protected]) F. Wong Department of Earth, Atmospheric, ([email protected]), and Planetary Sciences S. Hart Massachusetts Institute of Technology ([email protected]), 77 Massachusetts Avenue M. Kokorowski Cambridge, MA 02139 ([email protected]) B. Bone ([email protected]), B. Solish ([email protected]), D. Trofimov ([email protected]), E. Bradford ([email protected]), C. Raymond ([email protected]), P. Narvaez ([email protected]) Jet Propulsion Laboratory, California Institute of Technology 4800 Oak Grove Drive Pasadena, CA 91109 C. Keys C. Russell L. Elkins-Tanton ([email protected]), ([email protected]), ([email protected]) P. Lord University of California Los Angeles Arizona State University ([email protected]) 405 Hilgard Avenue PO Box 871404 Maxar Technologies Inc. Los Angeles, CA 90095 Tempe, AZ 85287 3825 Fabian Avenue Palo Alto, CA 94303 Abstract— Psyche is a Discovery mission that will visit the fields. Limiting and characterizing spacecraft-generated asteroid (16) Psyche to determine if it is the metallic core of a magnetic fields is therefore essential to the mission. This is the once larger differentiated body or otherwise was formed from objective of the Psyche’s magnetics control program described accretion of unmelted metal-rich material.