The "Horseshoe" Orbit of Near-Earth Object 2013 BS45 1. Earth-Based
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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. -
Origin and Evolution of Trojan Asteroids 725
Marzari et al.: Origin and Evolution of Trojan Asteroids 725 Origin and Evolution of Trojan Asteroids F. Marzari University of Padova, Italy H. Scholl Observatoire de Nice, France C. Murray University of London, England C. Lagerkvist Uppsala Astronomical Observatory, Sweden The regions around the L4 and L5 Lagrangian points of Jupiter are populated by two large swarms of asteroids called the Trojans. They may be as numerous as the main-belt asteroids and their dynamics is peculiar, involving a 1:1 resonance with Jupiter. Their origin probably dates back to the formation of Jupiter: the Trojan precursors were planetesimals orbiting close to the growing planet. Different mechanisms, including the mass growth of Jupiter, collisional diffusion, and gas drag friction, contributed to the capture of planetesimals in stable Trojan orbits before the final dispersal. The subsequent evolution of Trojan asteroids is the outcome of the joint action of different physical processes involving dynamical diffusion and excitation and collisional evolution. As a result, the present population is possibly different in both orbital and size distribution from the primordial one. No other significant population of Trojan aster- oids have been found so far around other planets, apart from six Trojans of Mars, whose origin and evolution are probably very different from the Trojans of Jupiter. 1. INTRODUCTION originate from the collisional disruption and subsequent reaccumulation of larger primordial bodies. As of May 2001, about 1000 asteroids had been classi- A basic understanding of why asteroids can cluster in fied as Jupiter Trojans (http://cfa-www.harvard.edu/cfa/ps/ the orbit of Jupiter was developed more than a century lists/JupiterTrojans.html), some of which had only been ob- before the first Trojan asteroid was discovered. -
Horsing Around on Saturn
Horsing Around on Saturn Robert J. Vanderbei Operations Research and Financial Engineering, Princeton University [email protected] ABSTRACT Based on simple statistical mechanical models, the prevailing view of Sat- urn’s rings is that they are unstable and must therefore have been formed rather recently. In this paper, we argue that Saturn’s rings and inner moons are in much more stable orbits than previously thought and therefore that they likely formed together as part of the initial formation of the solar system. To make this argument, we give a detailed description of so-called horseshoe orbits and show that this horseshoeing phenomenon greatly stabilizes the rings of Saturn. This paper is part of a collaborative effort with E. Belbruno and J.R. Gott III. For a description of their part of the work, see their papers in these proceedings. 1. Introduction The currently accepted view (see, e.g., Goldreich and Tremaine (1982)) of the formation of Saturn’s rings is that a moon-sized object wandered inside Saturn’s Roche limit and was torn apart by tidal forces. The resulting array of remnant masses was dispersed and formed the rings we see today. In this model, the system dynamics are treated as a turbulent flow with no explicit mention of the law of gravitation. The ring shape is presumed to be maintained by the coralling effect of a few of the inner moons acting as so-called shepherds. Of course, a simpler explanation would be that the rings formed along with the planets and their moons as they condensed out of the solar nebula. -
Arxiv:1304.1048V2 [Astro-Ph.EP] 26 Apr 2013 and Murray (1981A), General Properties of the Tadpole and Horseshoe Orbits Are Described in the Quasi- Circular Case
On the co-orbital motion of two planets in quasi-circular orbits Philippe Robutel and Alexandre Pousse IMCCE, Observatoire de Paris, UPMC, CNRS UMR8028, 77 Av. Denfert-Rochereau, 75014 Paris, France August 27, 2018 ABSTRACT We develop an analytical Hamiltonian formalism adapted to the study of the motion of two planets in co-orbital resonance. The Hamiltonian, averaged over one of the planetary mean lon- gitude, is expanded in power series of eccentricities and inclinations. The model, which is valid in the entire co-orbital region, possesses an integrable approximation modeling the planar and quasi-circular motions. First, focusing on the fixed points of this approximation, we highlight re- lations linking the eigenvectors of the associated linearized differential system and the existence of certain remarkable orbits like the elliptic Eulerian Lagrangian configurations, the Anti-Lagrange (Giuppone et al., 2010) orbits and some second sort orbits discovered by Poincar´e. Then, the variational equation is studied in the vicinity of any quasi-circular periodic solution. The funda- mental frequencies of the trajectory are deduced and possible occurrence of low order resonances are discussed. Finally, with the help of the construction of a Birkhoff normal form, we prove that the elliptic Lagrangian equilateral configurations and the Anti-Lagrange orbits bifurcate from the same fixed point L4. Subject headings: Co-orbitals; Resonance; Lagrange; Euler; Planetary problem; Three-body prob- lem 1. Introduction The co-orbital resonance has been extensively studied for more than one hundred years in the framework of the restricted three-body problem (RTBP). In most of the analytical works, the emphasis has been placed on the tadpole orbits, trajectories surrounding one of the two Lagrangian triangular equilibrium points, since these describe the motion of the Jovian Trojans. -
Arxiv:1901.07250V1
Astronomy & Astrophysics manuscript no. coorb_trans_arXiv c ESO 2019 January 23, 2019 Co-orbital exoplanets from close period candidates: The TOI-178 case A. Leleu1???, J. Lillo-Box2, M. Sestovic3, P. Robutel4, A. C. M. Correia5;4, N. Hara6??, D. Angerhausen3;7, S. L. Grimm3, J. Schneider8 1 Physikalisches Institut, Universität Bern, Gesellschaftsstr. 6, 3012 Bern, Switzerland. 2 European Southern Observatory, Alonso de Cordova 3107, Vitacura Casilla 19001, Santiago 19, Chile. 3 Center for Space and Habitability, University of Bern, Gesellschaftsstr. 6, 3012 Bern, Switzerland. 4 IMCCE, Observatoire de Paris - PSL Research University, UPMC Univ. Paris 06, Univ. Lille 1, CNRS, 77 Avenue Denfert-Rochereau, 75014 Paris, France. 5 CFisUC, Department of Physics, University of Coimbra, 3004-516 Coimbra, Portugal. 6 Observatoire de Genève, Université de Genève, 51 ch. des Maillettes, 1290 Versoix, Switzerland. 7 Blue Marble Space Institute of Science, 1001 4th Ave Suite 3201, Seattle, WA 98154, USA. 8 Paris Observatory, LUTh UMR 8102, 92190 Meudon,France. January 23, 2019 ABSTRACT Despite the existence of co-orbital bodies in the solar system, and the prediction of the formation of co-orbital planets by planetary system formation models, no co-orbital exoplanets (also called trojans) have been detected thus far. Here we study the signature of co-orbital exoplanets in transit surveys when two planet candidates in the system orbit the star with similar periods. Such pair of candidates could be discarded as false positives because they are not Hill-stable. However, horseshoe or long libration period tadpole co-orbital configurations can explain such period similarity. This degeneracy can be solved by considering the Transit Timing Variations (TTVs) of each planet. -
The “Horseshoe” Orbit of Near-Earth Object 2013 BS45 DANIEL R
Page 20 Astrodynamics The “Horseshoe” Orbit of Near-Earth Object 2013 BS45 DANIEL R. ADAMO, ASTRODYNAMICS CONSULTANT 1. Earth-Based Discovery million km) on 12 February inbound towards the Sun. It 2013. reaches perihelion on 29 April Discovered by the Space- 2013 at 0.92 AU or 92% of watch 1.8 m telescope (see As is typical among NEO Earth’s mean distance from Figure 1) on 20 January 2013, discoveries made in the night the Sun. Figure 2 is a plot of near-Earth object (NEO) 2013 sky prior to closest Earth ap- 2013 BS45, Earth, and Mars as BS45 closely encountered proach with observations of they orbit the Sun during Earth at a range of 0.0126 AU our planet’s night sky, 2013 2013. (4.9 lunar distances or 1.88 BS45 crosses Earth’s orbit Figure 1. The 1.8 m Space- watch telescope is pictured inside its protective dome at Kitt Peak, Arizona (photograph by Robert S. McMillan). Figure 2. Orbits of 2013 BS45 (blue), Earth (green), and Mars (red) are plotted during year 2013 in a non-rotating (inertial) Sun-centered (heliocentric) coordinate system. The plot plane coincides with that of Earth’s orbit, the ecliptic, and 2013 BS45’s orbit is inclined to the ecliptic by less than 1°. Before moving into Earth’s BS45 ephemerides with maxi- planetary radar observations daytime sky circa 9 February mum position uncertainties conducted at Goldstone, CA 2013, about 80 optical obser- equivalent to hundreds of had reduced this uncertainty vations were being processed minutes in heliocentric mo- to the order of 10 minutes. -
Preliminary Lander Cubesat Design for Small Asteroid Detumbling Mission
DEGREE PROJECT IN VEHICLE ENGINEERING, SECOND CYCLE, 30 CREDITS STOCKHOLM, SWEDEN 2018 Preliminary Lander CubeSat Design for Small Asteroid Detumbling Mission AGNE PASKEVICIUTE KTH ROYAL INSTITUTE OF TECHNOLOGY SCHOOL OF ENGINEERING SCIENCES Preliminary Lander CubeSat Design for Small Asteroid Detumbling Mission AgnėPaökevičiūtė Department of Aeronautical and Vehicle Engineering KTH Royal Institute of Technology This thesis is submitted for the degree of Master of Science October 2018 Skiriu ö˛ darbπsavo mamai Graûinai ir tėčiui Algirdui. Acknowledgements This thesis would have not been possible without the encouragement and support of numerous people in my life. I would especially like to thank Dr Michael C. F. Bazzocchi for his support and constructive advice throughout my research. In addition, I would like to express my gratitude to researchers, professors and staffat Luleå University of Technology, Space Campus, for their ideas and help in practical matters. I would like to sincerely thank my family, boyfriend, and friends for believing in me, encour- aging me to reach for my dreams, and loving me without any expectations. Last but not least, I am truly grateful for the opportunities KTH Royal Institute of Technol- ogy provided. Sammanfattning Gruvdrift på asteroider förväntas att bli verklighet inom en snar framtid. Det första steget är att omdirigera en asteroid till en stabil omloppsbana runt jorden så att gruvteknik kan demon- streras. Bromsning av asteroidens tumlande är en av de viktigaste stegen i ett rymduppdrag där en asteroid ska omdirigeras. I detta examensarbete föreslås en preliminär asteroidlandare baserad på CubeSat-teknik för ett rymduppdrag där en asteroid ska omdirigeras. En asteroid av Arjuna-typ, 2014 UR, med en diameter på mellan 10.6 och 21.2 m är vald som kandidat för rymduppdraget. -
The Palomar Transient Factory (PTF) Survey & Discovery of Small
The Palomar Transient Factory (PTF) Survey & Discovery of Small Mission-Accessible NEAs Adam Waszczak Graduate Student Division of Geological & Planetary Sciences California Institute of Technology The Palomar Transient Factory (PTF) 48-inch (1.2-m) “Oschin” robotic wide-field imaging [r-band] exposure time: 60s field-of-view: 7.3 deg2 / 11 CCDs limiting mag: r 20.5 resolution: 1.0 arcsec/pixel typical seeing: 2.0 arcsec FWHM The Palomar Transient Factory (PTF) 48-inch (1.2-m) “Oschin” robotic wide-field imaging [r-band] exposure time: 60s field-of-view: 7.3 deg2 / 11 CCDs limiting mag: r 20.5 resolution: 1.0 arcsec/pixel typical seeing: 2.0 arcsec FWHM The Palomar Transient Factory (PTF) 60-inch (1.5-m) robotic imaging follow-up [ugriz-bands & SED machine] 48-inch (1.2-m) “Oschin” robotic wide-field imaging [r-band] The Palomar Transient Factory (PTF) 60-inch (1.5-m) robotic imaging follow-up [ugriz-bands & SED machine] 48-inch (1.2-m) “Oschin” 200-inch (5.2-m) “Hale” robotic wide-field imaging spectroscopic follow-up [DBSP] [r-band] The Palomar Transient Factory (PTF) 60-inch (1.5-m) robotic imaging follow-up [ugriz-bands & SED machine] 48-inch (1.2-m) “Oschin” 200-inch (5.2-m) “Hale” robotic wide-field imaging spectroscopic follow-up [DBSP] [r-band] PTF is a world leader in the discovery and spectroscopic follow-up of extragalactic transients (e.g., supernovae). PTF detections of asteroids in general In past year, PTF submitted over 500,000 observations to the Minor Planet Center. -
Looking for Lurkers: Objects Co-Orbital with Earth As SETI Observables
Looking for Lurkers: Objects Co-orbital with Earth as SETI Observables James Benford Microwave Sciences, 1041 Los Arabis Lane, Lafayette, CA 94549 USA [email protected] Abstract A recently discovered group of nearby co-orbital objects is an attractive location for extraterrestrial intelligence (ETI) to locate a probe to observe Earth while not being easily seen. These near-Earth objects provide an ideal way to watch our world from a secure natural object. That provides resources an ETI might need: materials, a firm anchor, concealment. These have been little studied by astronomy and not at all by SETI or planetary radar observations. I describe these objects found thus far and propose both passive and active observations of them as possible sites for ET probes. 1. Introduction Alien astronomy at our present technical level may have detected our biosphere many millennia ago. Perhaps one or more such alien civilization was drawn in recently, by radio signals emanating from our world. Or maybe it has resided in our solar system for centuries, millennia or longer. Long-lived robotic lurkers could have been sent to observe Earth long ago. If properly powered, and capable of self- repair (von Neumann probes), they could report science and intelligence bacK to their origin over very long time scales. Long-lived alien societies may do this to gather science for the larger communicating societies in our galaxy. I will call such a probe a ‘LurKer’, a hidden observing probe which may respond to an intentional signal and may not, depending on unKnown alien motivations. (Here Lurkers are assumed to be robotic.) Observing ‘nearer-Earth objects’ would explore the possibility that there are nearby ‘exotic’ probes that we could discover or excite. -
A Resonant Family of Dynamically Cold Small Bodies in the Near-Earth Asteroid Belt
MNRASL 434, L1–L5 (2013) doi:10.1093/mnrasl/slt062 Advance Access publication 2013 June 18 A resonant family of dynamically cold small bodies in the near-Earth asteroid belt C. de la Fuente Marcos‹ and R. de la Fuente Marcos Universidad Complutense de Madrid, Ciudad Universitaria, E-28040 Madrid, Spain Accepted 2013 May 13. Received 2013 May 10; in original form 2013 February 25 Downloaded from https://academic.oup.com/mnrasl/article/434/1/L1/1163370 by guest on 27 September 2021 ABSTRACT Near-Earth objects (NEOs) moving in resonant, Earth-like orbits are potentially important. On the positive side, they are the ideal targets for robotic and human low-cost sample return missions and a much cheaper alternative to using the Moon as an astronomical observatory. On the negative side and even if small in size (2–50 m), they have an enhanced probability of colliding with the Earth causing local but still significant property damage and loss of life. Here, we show that the recently discovered asteroid 2013 BS45 is an Earth co-orbital, the sixth horseshoe librator to our planet. In contrast with other Earth’s co-orbitals, its orbit is strikingly similar to that of the Earth yet at an absolute magnitude of 25.8, an artificial origin seems implausible. The study of the dynamics of 2013 BS45 coupled with the analysis of NEO data show that it is one of the largest and most stable members of a previously undiscussed dynamically cold group of small NEOs experiencing repeated trappings in the 1:1 commensurability with the Earth. -
ORIGIN and EVOLUTION of the NATURAL SATELLITES S. J. Peale
P1: fne/FGM/FGG/FGP P2: FDR/fgm QC: FDR/Arun T1: Fhs September 9, 1999 20:54 Annual Reviews AR088-13 Annu. Rev. Astron. Astrophys. 1999. 37:533–602 Copyright 1999 by Annual Reviews. All rights reserved ORIGIN AND EVOLUTION OF THE NATURAL SATELLITES S. J. Peale Department of Physics, University of California, Santa Barbara, California 93117; e-mail: [email protected] Key Words tides, dissipation, dynamics, solar system, planets 1. INTRODUCTION The natural satellites of planets in the solar system display a rich variety of orbital configurations and surface characteristics that have intrigued astronomers, physi- cists, and mathematicians for several centuries. As detailed information about satellite properties have become available from close spacecraft reconnaissance, geologists and geophysicists have also joined the study with considerable enthu- siasm. This paper summarizes our ideas about the origin of the satellites in the context of the origin of the solar system itself, and it highlights the peculiarities of various satellites and the configurations in which we find them as a motiva- tion for constraining the satellites’ evolutionary histories. Section 2 describes the processes involved in forming our planetary system and points out how many of these same processes allow us to understand the formation of the regular satellites (those in nearly circular, equatorial orbits) as miniature examples of planetary systems. The irregular satellites, the Moon, and Pluto’s satellite, Charon, require special circumstances as logical additions to the more universal method of origin. Section 3 gives a brief description of tidal theory and a discussion of various ap- plications showing how dissipation of tidal energy effects secular changes in the orbital and spin configurations and how it deposits sufficient frictional heat into individual satellites to markedly change their interior and surface structures. -
Deep-Space Cubesats: Thinking Inside the Box
CUBESATS Deep-space CubeSats: thinking inside the box Roger Walker and colleagues CubeSats: small but perfectly formed consider the potential for sending Downloaded from https://academic.oup.com/astrogeo/article-abstract/59/5/5.24/5099069 by guest on 22 September 2018 nanospacecraft into deep space. CubeSats are modular spacecraft, using multiple standard-sized units of 10 x 10 x 10 cm ince the introduction of the CubeSat (figure 1); the size of the resulting spacecraft standard in the early 2000s, there has is measured by the number of units, e.g. 3U Sbeen a proliferation of nano-/small or 6U. The capabilities of these satellites have microsatellites in low Earth orbit, with increased significantly in recent years, notably 100–300 or more launched annually and at in pointing, propulsion and communications a growing rate (according to reports from as well as the availability of compact optical/ SpaceWorks and Euroconsult). CubeSats radio frequency/environment payloads. have reduced entry-level costs for space CubeSats are launched inside a standard missions in low Earth orbit (LEO) by container which simplifies launcher more than an order of magnitude (see box accommodation while ensuring safety for “CubeSats: small but perfectly formed”). the primary passenger, thus facilitating 1 Example of a 1U CubeSat shell. There is a This has brought new players into the widespread low-cost piggyback launch weight standard too – the finished launch unit space sector and launch opportunities for opportunities on many different launch must not exceed 1.33 kg. (ESA/G Porter) CubeSats have increased significantly in vehicles worldwide. At the same time, the the last decade to address the associated extensive use of miniaturized electronics, entry-level costs mean that the true power of demand.