Investigation Upon the Stability of Saturn Trojan Asteroids Around L4
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Astro2020 Science White Paper Modeling Debris Disk Evolution
Astro2020 Science White Paper Modeling Debris Disk Evolution Thematic Areas Planetary Systems Formation and Evolution of Compact Objects Star and Planet Formation Cosmology and Fundamental Physics Galaxy Evolution Resolved Stellar Populations and their Environments Stars and Stellar Evolution Multi-Messenger Astronomy and Astrophysics Principal Author András Gáspár Steward Observatory, The University of Arizona [email protected] 1-(520)-621-1797 Co-Authors Dániel Apai, Jean-Charles Augereau, Nicholas P. Ballering, Charles A. Beichman, Anthony Boc- caletti, Mark Booth, Brendan P. Bowler, Geoffrey Bryden, Christine H. Chen, Thayne Currie, William C. Danchi, John Debes, Denis Defrère, Steve Ertel, Alan P. Jackson, Paul G. Kalas, Grant M. Kennedy, Matthew A. Kenworthy, Jinyoung Serena Kim, Florian Kirchschlager, Quentin Kral, Sebastiaan Krijt, Alexander V. Krivov, Marc J. Kuchner, Jarron M. Leisenring, Torsten Löhne, Wladimir Lyra, Meredith A. MacGregor, Luca Matrà, Dimitri Mawet, Bertrand Mennes- son, Tiffany Meshkat, Amaya Moro-Martín, Erika R. Nesvold, George H. Rieke, Aki Roberge, Glenn Schneider, Andrew Shannon, Christopher C. Stark, Kate Y. L. Su, Philippe Thébault, David J. Wilner, Mark C. Wyatt, Marie Ygouf, Andrew N. Youdin Co-Signers Virginie Faramaz, Kevin Flaherty, Hannah Jang-Condell, Jérémy Lebreton, Sebastián Marino, Jonathan P. Marshall, Rafael Millan-Gabet, Peter Plavchan, Luisa M. Rebull, Jacob White Abstract Understanding the formation, evolution, diversity, and architectures of planetary systems requires detailed knowledge of all of their components. The past decade has shown a remarkable increase in the number of known exoplanets and debris disks, i.e., populations of circumstellar planetes- imals and dust roughly analogous to our solar system’s Kuiper belt, asteroid belt, and zodiacal dust. -
Discovery of Earth's Quasi-Satellite
Meteoritics & Planetary Science 39, Nr 8, 1251–1255 (2004) Abstract available online at http://meteoritics.org Discovery of Earth’s quasi-satellite Martin CONNORS,1* Christian VEILLET,2 Ramon BRASSER,3 Paul WIEGERT,4 Paul CHODAS,5 Seppo MIKKOLA,6 and Kimmo INNANEN3 1Athabasca University, Athabasca AB, Canada T9S 3A3 2Canada-France-Hawaii Telescope, P. O. Box 1597, Kamuela, Hawaii 96743, USA 3Department of Physics and Astronomy, York University, Toronto, ON M3J 1P3 Canada 4Department of Physics and Astronomy, University of Western Ontario, London, ON N6A 3K7, Canada 5Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA 6Turku University Observatory, Tuorla, FIN-21500 Piikkiö, Finland *Corresponding author. E-mail: [email protected] (Received 18 February 2004; revision accepted 12 July 2004) Abstract–The newly discovered asteroid 2003 YN107 is currently a quasi-satellite of the Earth, making a satellite-like orbit of high inclination with apparent period of one year. The term quasi- satellite is used since these large orbits are not completely closed, but rather perturbed portions of the asteroid’s orbit around the Sun. Due to its extremely Earth-like orbit, this asteroid is influenced by Earth’s gravity to remain within 0.1 AU of the Earth for approximately 10 years (1997 to 2006). Prior to this, it had been on a horseshoe orbit closely following Earth’s orbit for several hundred years. It will re-enter such an orbit, and make one final libration of 123 years, after which it will have a close interaction with the Earth and transition to a circulating orbit. -
Earth's Recurrent Quasi-Satellite?
2002 AA: Earth’s recurrent quasi-satellite ? Pawel Wajer To cite this version: Pawel Wajer. 2002 AA: Earth’s recurrent quasi-satellite ?. Icarus, Elsevier, 2009, 200 (1), pp.147. 10.1016/j.icarus.2008.10.018. hal-00510967 HAL Id: hal-00510967 https://hal.archives-ouvertes.fr/hal-00510967 Submitted on 23 Aug 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 2002 AA29: Earth’s recurrent quasi-satellite ? Paweł Wajer PII: S0019-1035(08)00381-3 DOI: 10.1016/j.icarus.2008.10.018 Reference: YICAR 8801 To appear in: Icarus Received date: 11 April 2008 Revised date: 20 October 2008 Accepted date: 23 October 2008 Please cite this article as: P. Wajer, 2002 AA29: Earth’s recurrent quasi-satellite ?, Icarus (2008), doi: 10.1016/j.icarus.2008.10.018 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. -
The Origin of the High-Inclination Neptune Trojan 2005 TN53 J
A&A 464, 775–778 (2007) Astronomy DOI: 10.1051/0004-6361:20066297 & c ESO 2007 Astrophysics The origin of the high-inclination Neptune Trojan 2005 TN53 J. Li, L.-Y. Zhou, and Y.-S. Sun Department of Astronomy, Nanjing University, Nanjing 210093, PR China e-mail: [email protected] Received 25 August 2006 / Accepted 20 November 2006 ABSTRACT Aims. We explore the formation and evolution of the highly inclined orbit of Neptune Trojan 2005 TN53. Methods. With numerical simulations, we investigated a possible mechanism for the origin of the high-inclination Neptune Trojans as captured into the Trojan-type orbits by an initially eccentric Neptune during its eccentricity damping and rapid inward migration, then migrating to the present locations locked in Neptune’s 1:1 mean motion resonance. ◦ Results. Two 2005 TN53-type Trojans out of our 2000 test particles were produced with inclinations above 20 , moving on tadpole orbits librating around Neptune’s leading Lagrange point. Key words. methods: numerical – celestial mechanics – minor planets, asteroids – solar system: formation 1. Introduction Table 1. Orbital elements of 2005 TN53 in heliocentric frame referred to the J2000.0 ecliptic plane at epoch 2005 October 7. The uncertainties Trojan asteroids are small objects that share the semimajor axis at the 3 σ level in a, e, i are ± 0.1 AU, ± 0.01, and ± 0.1◦, respectively. of their host planet. They orbit the Sun with the same period as the planet and are said to be settled in the planet’s 1:1 mean mo- a (AU) ei(◦) Ω (◦) ω (◦) M (◦) tion resonance (MMR). -
Long-Term Evolution of the Neptune Trojan 2001 QR322
Mon. Not. R. Astron. Soc. 347, 833Ð836 (2004) Long-term evolution of the Neptune Trojan 2001 QR322 R. Brasser,1 S. Mikkola,1 T.-Y. Huang,2 P. Wiegert3 and K. Innanen4 1Tuorla Observatory, University of Turku, Piikkio,¬ Finland 2Deptartment of Astronomy, Nanjing University, Nanjing, China 3Astronomy Unit, Queen’s University, Kingston, ON, Canada 4Deptartment of Physics and Astronomy, York University, Toronto, ON, Canada Accepted 2003 October 1. Received 2003 September 9; in original form 2003 April 23 ABSTRACT We simulated more than a hundred possible orbits of the Neptune Trojan 2001 QR322 for the age of the Solar system. The orbits were generated randomly according to the probability density derived from the covariance matrix of the orbital elements. The test trajectories librate ◦ ◦ around Neptune’s L4 point, with amplitudes varying from 40 to 75 and libration periods varying from 8900 to 9300 yr. The ν 18 secular resonance plays an important role. There is a separatrix of the resonance so that the resonant angle switches irregularly between libration and circulation. The orbits are chaotic, with observed Lyapunov times from 1.7 to 20 Myr, approximately. The probability of escape to a non-Trojan orbit in our simulations was low, and only occurred for orbits starting near the low-probability edge of the orbital element distribution (largest values of initial semimajor axis and small eccentricity). This suggests that the Trojan may well be a primordial object. Key words: celestial mechanics Ð minor planets, asteroids Ð Solar system: general. in the element vector q were computed as 1 INTRODUCTION According to the Minor Planet Center, 1571 Trojan asteroids have 6 been discovered. -
Report to the NSF AST Senior Review (July 2005)
NATIONAL ASTRONOMY & IONOSPHERE CENTER Operated by Cornell University under cooperative agreement with the National Science Foundation NAIC Science in the Twenty-First Century: Report to the NSF Senior Review El quien no ha visto el Observatorio de Arecibo no ha visto una maravilla. July 2005 NAIC Science in the Twenty-First Century: Report to the NSF Senior Review 1. Executive Summary 1 2. The Unique Role of NAIC in U.S. Astronomy 2 2.1 The “Millennium Questions” in Astrophysics 2 2.2 ALFA Surveys 3 2.3 Pulsar Timing 10 2.4 the High Sensitivity Array 11 2.5 S-Band Planetary Radar 14 2.6 SETI 18 3. NAIC Science in the Twenty-First Century: A New Model for a National Observatory 18 3.1 Partnerships in Detector and Digital Signal Processing Technology 20 3.2 Partnerships in Computation and Information Sharing Technology 21 3.3 ALFA Legacy Survey Consortia Organization 24 3.4 Management of the U.S. Square Kilometer Array Partnership for the Technology Development Project 25 4. NAIC General Facility Description 25 4.1 Overview of the Facility 25 4.2 NAIC Managing Institution and Organization 26 4.3 NAIC Funding Sources 26 4.4 Specifics of the Telescope and Instrumentation 26 4.5 New Capabilities Planned in the Next 5-10 Years 26 4.6 Science Overview 27 4.6.1 Current Forefront Scientific Programs 27 4.6.2 Major NAIC Astronomy Program Scientific Discoveries Made at the Arecibo Observatory 28 4.6.3 NAIC Astronomy Program Science Highlights of the Last Five Years 29 4.6.4 Focus on Future Astronomy Program Science Questions 29 5. -
Radar Detection of Asteroid 2002 AA29
Icarus 166 (2003) 271–275 www.elsevier.com/locate/icarus Radar detection of Asteroid 2002 AA29 Steven J. Ostro,a,∗ Jon D. Giorgini,a Lance A.M. Benner,a Alice A. Hine,b Michael C. Nolan,b Jean-Luc Margot,c Paul W. Chodas,a and Christian Veillet d a Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA b National Astronomy and Ionosphere Center, Arecibo Observatory, HC3 Box 53995, Arecibo, PR 00612, USA c California Institute of Technology, Pasadena, CA 91125, USA d Canada–France–Hawaii Telescope Corporation, 65-1238 Mamaloha Hwy, Kamuela, HI 96743, USA Received 24 June 2003; revised 27 August 2003 Abstract − Radar echoes from Earth co-orbital Asteroid 2002 AA29 yield a total-power radar cross section of 2.9 × 10 5 km2 ±25%, a circular polarization ratio of SC/OC = 0.26 ± 0.07, and an echo bandwidth of at least 1.5 Hz. Combining these results with the estimate of its visual absolute magnitude, HV = 25.23 ± 0.24, from reported Spacewatch photometry indicates an effective diameter of 25 ± 5 m, a rotation period − no longer than 33 min, and an average surface bulk density no larger than 2.0 g cm 3; the asteroid is radar dark and optically bright, and its statistically most likely spectral class is S. The HV estimate from LINEAR photometry (23.58 ± 0.38) is not compatible with either Spacewatch’s HV or our radar results. If a bias this large were generally present in LINEAR’s estimates of HV for asteroids it has discovered or observed, then estimates of the current completeness of the Spaceguard Survey would have to be revised downward. -
Arxiv:1611.07413V1
Noname manuscript No. (will be inserted by the editor) Trojan capture by terrestrial planets Schwarz, R. · Dvorak, R. the date of receipt and acceptance should be inserted later Abstract The paper is devoted to investigate the capture of asteroids by Venus, Earth and Mars into the 1:1 mean motion resonance especially into Trojan orbits. Current theoretical studies predict that Trojan asteroids are a frequent by-product of the planet formation. This is not only the case for the outer giant planets, but also for the terrestrial planets in the inner Solar System. By using numerical integrations, we investigated the capture efficiency and the stability of the captured objects. We found out that the capture efficiency is larger for the planets in the inner Solar System compared to the outer ones, but most of the captured Trojan asteroids are not long term stable. This temporary captures caused by chaotic behaviour of the objects were investigated without any dissipative forces. They show an interesting dynamical behaviour of mixing like jumping from one Lagrange point to the other one. Keywords Trojan capture · terrestrial planets · Near Earth asteroids · 1:1 mean motion resonance 1 Introduction In February 1906, Max Wolf [38] discovered the first Trojan asteroid named 588 Achilles, after the hero of the Trojan war. Almost a century later, in 1990, the first Martian Trojan (5261 Eureka) was observed by Bowell et al. [4]. In 2001 the first Neptune Trojan was discovered by the Lowell Observatory Deep Ecliptic R. Schwarz T¨urkenschanzstrasse 17, 1180 Vienna Tel.: +43-1-427751841 Fax: +43-1-42779518 E-mail: [email protected] R. -
Origin and Dynamical Evolution of Neptune Trojans – I: Formation and Planetary Migration
Origin and Dynamical Evolution of Neptune Trojans – I: Formation and Planetary Migration Patryk Sofia Lykawka,1* Jonathan Horner,2 Barrie W. Jones 2 and Tadashi Mukai1 1 Dept. of Earth and Planetary Sciences, Kobe University, 1-1 rokkodai-cho, nada-ku, Kobe 657- 8501, Japan 2 Dept. of Physics and Astronomy, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK ******* This paper was published in Monthly Notices of the Royal Astronomical Society 398, 1715-1729 (2009). [email protected] http://sites.google.com/site/patryksofialykawka/ ******* * Present address: International Center for Human Sciences (Planetary Sciences), Kinki University, 3-4-1 Kowakae, Higashiosaka-shi, Osaka-fu, 577-8502, Japan. E-mail address: [email protected] 1 of 25 ABSTRACT We present the results of detailed dynamical simulations of the effect of the migration of the four giant planets on both the transport of pre-formed Neptune Trojans, and the capture of new Trojans from a trans-Neptunian disk. The cloud of pre-formed Trojans consisted of thousands of massless particles placed on dynamically cold orbits around Neptune’s L4 and L5 Lagrange points, while the trans-Neptunian disk contained tens of thousands of such particles spread on dynamically cold orbits between the initial and final locations of Neptune. Through comparison of the results with previous work on the known Neptunian Trojans, we find that scenarios involving the slow migration of Neptune over a large distance (50 Myr to migrate from 18.1 AU to its current location, using an exponential-folding time of τ = 10 Myr) provide the best match to the properties of the known Trojans. -
Stability of Uranus and Neptune Trojans. the Case of 2001 QR322
A&A 410, 725–734 (2003) Astronomy DOI: 10.1051/0004-6361:20031275 & c ESO 2003 Astrophysics The MATROS project: Stability of Uranus and Neptune Trojans. The case of 2001 QR322 F. Marzari1, P. Tricarico1, and H. Scholl2 1 Dipartimento di Fisica, University of Padova, Via Marzolo 8, 35131 Padova, Italy 2 Observatoire de la Cˆote d’Azur, BP 4229, 06304 Nice Cedex 4, France Received 17 April 2003 / Accepted 8 August 2003 Abstract. We present in this paper an analysis of the long term stability of Trojan type orbits of both Uranus and Neptune. Employing the Frequency Map Analysis (hereinafter FMA) we measure the diffusion speed in the phase space for a large sample of Trojan orbits with short numerical integrations. High resolution diffusion maps are derived for different values of initial inclination. These maps outline where the most stable orbits can be found in the Trojan clouds of the two planets. The orbit of the newly discovered Neptune Trojan 2001 QR322 has been analysed in detail with the FMA method. In the phase space the body is located close to the border of a stable region for low inclination Neptune Trojans. Numerical integrations over 4.5 Gyr of clone orbits generated from the covariance matrix show that only 10% of the clones escape from the Trojan cloud. The proper frequencies of the Trojan motion computed with the FMA algorithm allow us to to derive a numerical secular theory. From this theory it is possible to locate in the phase space the main secular resonances that can perturb Trojan orbits of the two planets and lead to instability. -
Discovery Paper
Meteoritics & Planetary Science 39, Nr 8, 12511255 (2004) Abstract available online at http://meteoritics.org Discovery of Earth‘s quasi-satellite Martin CONNORS,1* Christian VEILLET,2 Ramon BRASSER,3 Paul WIEGERT,4 Paul CHODAS,5 Seppo MIKKOLA,6 and Kimmo INNANEN3 1Athabasca University, Athabasca AB, Canada T9S 3A3 2Canada-France-Hawaii Telescope, P. O. Box 1597, Kamuela, Hawaii 96743, USA 3Department of Physics and Astronomy, York University, Toronto, ON M3J 1P3 Canada 4Department of Physics and Astronomy, University of Western Ontario, London, ON N6A 3K7, Canada 5Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA 6Turku University Observatory, Tuorla, FIN-21500 Piikkiö, Finland *Corresponding author. E-mail: [email protected] (Received 18 February 2004; revision accepted 12 July 2004) AbstractœThe newly discovered asteroid 2003 YN107 is currently a quasi-satellite of the Earth, making a satellite-like orbit of high inclination with apparent period of one year. The term quasi- satellite is used since these large orbits are not completely closed, but rather perturbed portions of the asteroid‘s orbit around the Sun. Due to its extremely Earth-like orbit, this asteroid is influenced by Earth‘s gravity to remain within 0.1 AU of the Earth for approximately 10 years (1997 to 2006). Prior to this, it had been on a horseshoe orbit closely following Earth‘s orbit for several hundred years. It will re-enter such an orbit, and make one final libration of 123 years, after which it will have a close interaction with the Earth and transition to a circulating orbit. Chaotic effects limit our ability to determine the origin or fate of this object. -
Physical and Dynamical Study of Minor Bodies and Natural Satellites of the Solar System
PLANETARY SCIENCES: physical and dynamical study of minor bodies and natural satellites of the Solar System Monica Lazzarin The study of the minor bodies (asteroids, comets,trans-Neptunians, natural satellites etc.) is of particular relevance for understanding the formation process, the early phases and the subsequent dynamical, physical and chemical evolution of the Solar System. The lack of important modifications since their formation can give crucial clues on the status of the early solar nebula, and on the processes occurring some 4.5 billion years ago. Their observed diversity points to the existence of important thermal, dynamical and chemical gradients along the nebula that must also have affected the evolutionary history of the planets, and that requires a diversified approach for an overall vision. In particular, the following aspects that are subject of vast interest in the international community, constitute the scientific background of the present project (see references below of the research group and of other international groups on the subjects): A - Origin and nature of the Near Earth Asteroids/Objects (NEA/NEO). Their orbits come very close to that of the Earth, in several cases intersecting it and posing some impact threat. Their origin is not well known yet: they could be inactive/dormant comets, with a very pristine composition, but also more geologically processed asteroids. The NEA/NEOs population appears extremely heterogeneous in all their aspects: physical properties, shapes, albedos, surface compositions. A fraction (possibly large) of the total are binary systems; studies of their light curves demonstrate in some cases a complex rotational status, others show a long rotational period not easily explained in the framework of the current dynamical and collisional models.