The Quasi-Hilda Subgroup of Ecliptic Comets – an Update (Research Note)
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Asteroid Shape and Spin Statistics from Convex Models J
Asteroid shape and spin statistics from convex models J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen To cite this version: J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen. Asteroid shape and spin statistics from convex models. Icarus, Elsevier, 2008, 198 (1), pp.91. 10.1016/j.icarus.2008.07.014. hal-00499092 HAL Id: hal-00499092 https://hal.archives-ouvertes.fr/hal-00499092 Submitted on 9 Jul 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Asteroid shape and spin statistics from convex models J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen PII: S0019-1035(08)00283-2 DOI: 10.1016/j.icarus.2008.07.014 Reference: YICAR 8734 To appear in: Icarus Received date: 18 September 2007 Revised date: 3 July 2008 Accepted date: 7 July 2008 Please cite this article as: J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen, Asteroid shape and spin statistics from convex models, Icarus (2008), doi: 10.1016/j.icarus.2008.07.014 This is a PDF file of an unedited manuscript that has been accepted for publication. -
Color Study of Asteroid Families Within the MOVIS Catalog David Morate1,2, Javier Licandro1,2, Marcel Popescu1,2,3, and Julia De León1,2
A&A 617, A72 (2018) Astronomy https://doi.org/10.1051/0004-6361/201832780 & © ESO 2018 Astrophysics Color study of asteroid families within the MOVIS catalog David Morate1,2, Javier Licandro1,2, Marcel Popescu1,2,3, and Julia de León1,2 1 Instituto de Astrofísica de Canarias (IAC), C/Vía Láctea s/n, 38205 La Laguna, Tenerife, Spain e-mail: [email protected] 2 Departamento de Astrofísica, Universidad de La Laguna, 38205 La Laguna, Tenerife, Spain 3 Astronomical Institute of the Romanian Academy, 5 Cu¸titulde Argint, 040557 Bucharest, Romania Received 6 February 2018 / Accepted 13 March 2018 ABSTRACT The aim of this work is to study the compositional diversity of asteroid families based on their near-infrared colors, using the data within the MOVIS catalog. As of 2017, this catalog presents data for 53 436 asteroids observed in at least two near-infrared filters (Y, J, H, or Ks). Among these asteroids, we find information for 6299 belonging to collisional families with both Y J and J Ks colors defined. The work presented here complements the data from SDSS and NEOWISE, and allows a detailed description− of− the overall composition of asteroid families. We derived a near-infrared parameter, the ML∗, that allows us to distinguish between four generic compositions: two different primitive groups (P1 and P2), a rocky population, and basaltic asteroids. We conducted statistical tests comparing the families in the MOVIS catalog with the theoretical distributions derived from our ML∗ in order to classify them according to the above-mentioned groups. We also studied the background populations in order to check how similar they are to their associated families. -
The Minor Planet Bulletin 44 (2017) 142
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 44, NUMBER 2, A.D. 2017 APRIL-JUNE 87. 319 LEONA AND 341 CALIFORNIA – Lightcurves from all sessions are then composited with no TWO VERY SLOWLY ROTATING ASTEROIDS adjustment of instrumental magnitudes. A search should be made for possible tumbling behavior. This is revealed whenever Frederick Pilcher successive rotational cycles show significant variation, and Organ Mesa Observatory (G50) quantified with simultaneous 2 period software. In addition, it is 4438 Organ Mesa Loop useful to obtain a small number of all-night sessions for each Las Cruces, NM 88011 USA object near opposition to look for possible small amplitude short [email protected] period variations. Lorenzo Franco Observations to obtain the data used in this paper were made at the Balzaretto Observatory (A81) Organ Mesa Observatory with a 0.35-meter Meade LX200 GPS Rome, ITALY Schmidt-Cassegrain (SCT) and SBIG STL-1001E CCD. Exposures were 60 seconds, unguided, with a clear filter. All Petr Pravec measurements were calibrated from CMC15 r’ values to Cousins Astronomical Institute R magnitudes for solar colored field stars. Photometric Academy of Sciences of the Czech Republic measurement is with MPO Canopus software. To reduce the Fricova 1, CZ-25165 number of points on the lightcurves and make them easier to read, Ondrejov, CZECH REPUBLIC data points on all lightcurves constructed with MPO Canopus software have been binned in sets of 3 with a maximum time (Received: 2016 Dec 20) difference of 5 minutes between points in each bin. -
VITA David Jewitt Address Dept. Earth, Planetary and Space
VITA David Jewitt Address Dept. Earth, Planetary and Space Sciences, UCLA 595 Charles Young Drive East, Box 951567 Los Angeles, CA 90095-1567 [email protected], http://www2.ess.ucla.edu/~jewitt/ Education B. Sc. University College London 1979 M. S. California Institute of Technology 1980 Ph. D. California Institute of Technology 1983 Professional Experience Summer Student Royal Greenwich Observatory 1978 Anthony Fellowship California Institute of Technology 1979-1980 Research Assistant California Institute of Technology 1980-1983 Assistant Professor Massachusetts Institute of Technology 1983-1988 Associate Professor and Astronomer University of Hawaii 1988-1993 Professor and Astronomer University of Hawaii 1993-2009 Professor Dept. Earth, Planetary & Space Sciences, UCLA 2009- Inst. of Geophys & Planetary Physics, UCLA 2009-2011 Dept. Physics & Astronomy, UCLA 2010- Director Institute for Planets & Exoplanets, UCLA, 2011- Honors Regent's Medal, University of Hawaii 1994 Scientist of the Year, ARCS 1996 Exceptional Scientific Achievement Award, NASA 1996 Fellow of University College London 1998 Fellow of the American Academy of Arts and Sciences 2005 Fellow of the American Association for the Advancement of Science 2005 Member of the National Academy of Sciences 2005 National Observatory, Chinese Academy of Sciences, Honorary Professor 2006-2011 National Central University, Taiwan, Adjunct Professor 2007 The Shaw Prize for Astronomy 2012 The Kavli Prize for Astrophysics 2012 Foreign Member, Norwegian Academy of Sciences & Letters 2012 Research -
Asteroid Family Identification 613
Bendjoya and Zappalà: Asteroid Family Identification 613 Asteroid Family Identification Ph. Bendjoya University of Nice V. Zappalà Astronomical Observatory of Torino Asteroid families have long been known to exist, although only recently has the availability of new reliable statistical techniques made it possible to identify a number of very “robust” groupings. These results have laid the foundation for modern physical studies of families, thought to be the direct result of energetic collisional events. A short summary of the current state of affairs in the field of family identification is given, including a list of the most reliable families currently known. Some likely future developments are also discussed. 1. INTRODUCTION calibrate new identification methods. According to the origi- nal papers published in the literature, Brouwer (1951) used The term “asteroid families” is historically linked to the a fairly subjective criterion to subdivide the Flora family name of the Japanese researcher Kiyotsugu Hirayama, who delineated by Hirayama. Arnold (1969) assumed that the was the first to use the concept of orbital proper elements to asteroids are dispersed in the proper-element space in a identify groupings of asteroids characterized by nearly iden- Poisson distribution. Lindblad and Southworth (1971) cali- tical orbits (Hirayama, 1918, 1928, 1933). In interpreting brated their method in such a way as to find good agree- these results, Hirayama made the hypothesis that such a ment with Brouwer’s results. Carusi and Massaro (1978) proximity could not be due to chance and proposed a com- adjusted their method in order to again find the classical mon origin for the members of these groupings. -
Aas 14-267 Design of End-To-End Trojan Asteroid
AAS 14-267 DESIGN OF END-TO-END TROJAN ASTEROID RENDEZVOUS TOURS INCORPORATING POTENTIAL SCIENTIFIC VALUE Jeffrey Stuart,∗ Kathleen Howell,y and Roby Wilsonz The Sun-Jupiter Trojan asteroids are celestial bodies of great scientific interest as well as potential natural assets offering mineral resources for long-term human exploration of the solar system. Previous investigations have addressed the auto- mated design of tours within the asteroid swarm and the transition of prospective tours to higher-fidelity, end-to-end trajectories. The current development incorpo- rates the route-finding Ant Colony Optimization (ACO) algorithm into the auto- mated tour generation procedure. Furthermore, the potential scientific merit of the target asteroids is incorporated such that encounters with higher value asteroids are preferentially incorporated during sequence creation. INTRODUCTION Near Earth Objects (NEOs) are currently under consideration for manned sample return mis- sions,1 while a recent NASA feasibility assessment concludes that a mission to the Trojan asteroids can be accomplished at a projected cost of less than $900M in fiscal year 2015 dollars.2 Tour concepts within asteroid swarms allow for a broad sampling of interesting target bodies either for scientific investigation or as potential resources to support deep-space human missions. However, the multitude of asteroids within the swarms necessitates the use of automated design algorithms if a large number of potential mission options are to be surveyed. Previously, a process to automatically and rapidly generate sample tours within the Sun-Jupiter L4 Trojan asteroid swarm with a mini- mum of human interaction has been developed.3 This scheme also enables the automated transition of tours of interest into fully optimized, end-to-end trajectories using a variety of electrical power sources.4,5 This investigation extends the automated algorithm to use ant colony optimization, a heuristic search algorithm, while simultaneously incorporating a relative ‘scientific importance’ ranking into tour construction and analysis. -
Origin of the Near-Earth Asteroid Phaethon and the Geminids Meteor Shower
University of Central Florida STARS Faculty Bibliography 2010s Faculty Bibliography 1-1-2010 Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower J. de León H. Campins University of Central Florida K. Tsiganis A. Morbidelli J. Licandro Find similar works at: https://stars.library.ucf.edu/facultybib2010 University of Central Florida Libraries http://library.ucf.edu This Article is brought to you for free and open access by the Faculty Bibliography at STARS. It has been accepted for inclusion in Faculty Bibliography 2010s by an authorized administrator of STARS. For more information, please contact [email protected]. Recommended Citation de León, J.; Campins, H.; Tsiganis, K.; Morbidelli, A.; and Licandro, J., "Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower" (2010). Faculty Bibliography 2010s. 92. https://stars.library.ucf.edu/facultybib2010/92 A&A 513, A26 (2010) Astronomy DOI: 10.1051/0004-6361/200913609 & c ESO 2010 Astrophysics Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower J. de León1,H.Campins2,K.Tsiganis3, A. Morbidelli4, and J. Licandro5,6 1 Instituto de Astrofísica de Andalucía-CSIC, Camino Bajo de Huétor 50, 18008 Granada, Spain e-mail: [email protected] 2 University of Central Florida, PO Box 162385, Orlando, FL 32816.2385, USA e-mail: [email protected] 3 Department of Physics, Aristotle University of Thessaloniki, 54 124 Thessaloniki, Greece 4 Departement Casiopée: Universite de Nice - Sophia Antipolis, Observatoire de la Cˆote d’Azur, CNRS 4, 06304 Nice, France 5 Instituto de Astrofísica de Canarias (IAC), C/Vía Láctea s/n, 38205 La Laguna, Spain 6 Department of Astrophysics, University of La Laguna, 38205 La Laguna, Tenerife, Spain Received 5 November 2009 / Accepted 26 January 2010 ABSTRACT Aims. -
Widespread Water Among Primitive Asteroid Families: New Insights from the Main Belt Comets
EPSC Abstracts Vol. 13, EPSC-DPS2019-892-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. Widespread water among primitive asteroid families: new insights from the main belt comets Bojan Novakovic´ (1) and Henry Hsieh (2,3) (1) University of Belgrade, Serbia, (2) Planetary Science Institute, USA, (3) Academia Sinica Institute of Astronomy and Astrophysics, Taiwan, ([email protected]) Abstract The obtained results are summarized in Table 1. For the first time we found active asteroids associated to We present new results regarding the association of the Pallas and Luthera families, namely P/2017 S8 and main belt comets to asteroid families. We find three P/2019 A7, respectively. new firm links, and three potential associations. These results further strengthen the link between the main Table 1: A list of asteroid family associations of newly belt comets and compositionally primitive asteroid discovered main belt comet candidates. families. MBC candidate Family 1. Introduction P/2016 P1 (PANSTARRS) Euphrosyne? P/2017 S8 (PANSTARRS) Pallas Main belt comets (MBCs) are a subgroup of active as- P/2017 S5 (PANSTARRS) Theobalda teroids, which exhibit visible mass loss activity yet P/2017 S9 (PANSTARRS) Theobalda? are dynamically asteroidal, for which it is believed P/2019 A3 (PANSTARRS) Theobalda? that observed activity is driven by the sublimation of P/2019 A4 (PANSTARRS) None? volatile ices [1, 2]. Our recent work has demonstrated P/2019 A7 (PANSTARRS) Luthera that all MBCs associated to collisional families be- P/2019 A8 (PANSTARRS) None? long to families with primitive taxonomic classifica- tions [3]. -
Planetary Astronomy (Nasw-4266)
N89- 16639 NATIONAL AERONAUTICS AN0 SPACE AOMlNlSTAATlON RESEARCH AND TECHNOLOGY RESUME TITLE PLANETARY ASTRONOMY (NASW-4266) PERFORMING ORGANIZATION Planetary Science Institute -_~ 2030 East Speedway, Suite 201 -- Tucson, Arizona 85719 INV EST1 G AZO R’S NAME Dr. Clark R. Chapman I OESCRIPTION la. Brief rtolcmenl on shatepy of inuerti#alion; b. Pro;mrr and accomplichmenlr of prior year; C. What will be occompllrhed fhu yew. 0s wrII as hoy-!_end why; and d. Summay bibllorraphy) a. s’trateqy: rhe above-referenced Flanefary Astronomy contract supports iivE 5enicr rese3Fchers at the Planetary Science Institute !firs. Campins, Chapman, Davis. Hartnann. and Weidenschilling! with some involvement of other staff members. The goal i; to use a varietv of observational techniques and instruments to redi-ice, interpret. 3nd syn+hesiro groundbased astronosicai data concerning the comets. asteroids, and other small bodies af the solar svstem in order to 5tiidv the compositinns, physical characteristics, popuiaticrn properties, and evolution of th~:? bodies. have performed a variety of programmatic tasks, as well, including Chapman’s cast chairmanship of the Planetary Astronomy MDWG. 1 : d. Summary biblioqraphy !attached) I 29 SUMMARY BIBLIOGRAPHY Ahrens. T.J., Campins. H. and 20 other authors (1987). Report of the Joint EStVNASA Science Definition Team, Rosetta: The Comet Nucleus Sample Return Mission. Campins, H.. Rieke. M.J.. and Rieke, G.H. (1988). An Infrared Color Gradient in the Inner Coma of Comet Halley, submitted to Icarus. Chapman, C.R. (1987). Distributions of Asteroid Compositional Types with Solar Distance, Body Diameter, and Family Membership, Meteoritics 22. 353-354. Chapman, C.R. (1987). The Asteroid Belt: Compositional Structure and Size Distributions, DPS abstract. -
8 Asteroid–Meteoroid Complexes
“9781108426718c08” — 2019/5/13 — 16:33 — page 187 — #1 8 Asteroid–Meteoroid Complexes Toshihiro Kasuga and David Jewitt 8.1 Introduction Jenniskens, 2011)1 and asteroid 3200 Phaethon are probably the best-known examples (Whipple, 1983). In such cases, it Physical disintegration of asteroids and comets leads to the appears unlikely that ice sublimation drives the expulsion of production of orbit-hugging debris streams. In many cases, the solid matter, raising following general question: what produces mechanisms underlying disintegration are uncharacterized, or the meteoroid streams? Suggested alternative triggers include even unknown. Therefore, considerable scientific interest lies in thermal stress, rotational instability and collisions (impacts) tracing the physical and dynamical properties of the asteroid- by secondary bodies (Jewitt, 2012; Jewitt et al., 2015). Any meteoroid complexes backwards in time, in order to learn how of these, if sufficiently violent or prolonged, could lead to the they form. production of a debris trail that would, if it crossed Earth’s orbit, Small solar system bodies offer the opportunity to understand be classified as a meteoroid stream or an “Asteroid-Meteoroid the origin and evolution of the planetary system. They include Complex”, comprising streams and several macroscopic, split the comets and asteroids, as well as the mostly unseen objects fragments (Jones, 1986; Voloshchuk and Kashcheev, 1986; in the much more distant Kuiper belt and Oort cloud reservoirs. Ceplecha et al., 1998). Observationally, asteroids and comets are distinguished princi- The dynamics of stream members and their parent objects pally by their optical morphologies, with asteroids appearing may differ, and dynamical associations are not always obvious. -
Introducing the Eulalia and New Polana Asteroid Families: Re-Assessing the Source Regions of Primitive Near-Earth Asteroids
44th Lunar and Planetary Science Conference (2013) 2835.pdf INTRODUCING THE EULALIA AND NEW POLANA ASTEROID FAMILIES: RE-ASSESSING THE SOURCE REGIONS OF PRIMITIVE NEAR-EARTH ASTEROIDS. K. J. Walsh1, M. Delbó2, W. F. Bottke1, D. Vokrouhlický3 and D. S. Lauretta4, 1Southwest Research Institute, Boulder, CO, 2Laboratoire Lagrange, UNS- CNRS-Observatoire de la Côte d’Azur, Nice, France, 3Institute of Astronomy, Charles University, V Holěsovičkaćh 2, Prague 8, Czech Republic, 4Lunar & Planetary Laboratory, University of Arizona, Tucson, AZ, USA. Introduction: The inner main asteroid belt (2.15 AU < times due to the Yarkovsky effect [1]. This effect a < 2.5 AU) is the dominant source region of near- causes a secular drift of the semi-major axis of the or- Earth objects (NEOs). Of those asteroids from this bit due to the emission of the thermal radiation. region that become NEOs, most are delivered via the Whether this effect causes an increase or decrease of ν6 secular resonance located at ∼2.15 AU. In particular, an asteroid’s semimajor axis depends on its rotation this pathway is the most likely delivery source for state, whereby prograde rotators drift outward and ret- NEOs on low Δ-velocity orbits, such as the proposed rograde rotators drift inward. Thus, radial drift into a space mission targets 1996 RQ36 and 1999 JU3. These resonance, followed by rapid increase in orbital eccen- missions are specifically targeting primitive asteroids - tricity and the eventual interaction with terrestrial those asteroids of C- or B-type taxonomies that are planets, is the typical pathway for Main Belt asteroids thought to be related to Carbonaceous Chondrite mete- to become NEOs [1]. -
XV Congresso Nazionale Di Scienze Planetarie PRESIDENTE DEL CONGRESSO: Giovanni Pratesi
https://doi.org/10.3301/ABSGI.2019.01 Firenze, 4-8 Febbraio 2019 ABSTRACT BOOK a cura della Società Geologica Italiana XV Congresso Nazionale di Scienze Planetarie PRESIDENTE DEL CONGRESSO: Giovanni Pratesi. COMITATO SCIENTIFICO: Giovanni Pratesi, Emanuele Pace, Marco Benvenuti, John Brucato, Fabrizio Capaccioni, Sandro Conticelli, Aldo Dell’Oro, Carlo Alberto Garzonio, Daniele Gardiol, Monica Lazzarin, Alessandro Marconi, Lucia Mari- nangeli, Giuseppina Micela, Ettore Perozzi, Alessandro Rossi, Alessandra Rotundi. COMITATO ORGANIZZATORE: Cristian Carli, Mario Di Martino, Livia Giacomini, Vanni Moggi Cecchi, Emanuele Pace, Giovanni Pratesi, Giovanni Valsecchi. CURATORI DEL VOLUME Giovanni Pratesi, Fabrizio Capaccioni, Emanuele Pace, John Brucato, Marco Benvenuti, Sandro Conti- celli, Aldo Dell’Oro, Daniele Gardiol, Carlo Alberto Garzonio, Monica Lazzarin, Alessandro Marconi, Lucia Marinangeli, Giuseppina Micela, Ettore Perozzi, Alessandro Rossi, Alessandra Rotundi. Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. ABSTRACT INDEX EDUCARE ALLA