Limits of Stability in Earth Co-orbital Motion of Asteroids Martin Connors, Athabasca University Christian Veillet, CFHT R. Greg Stacey, Athabasca University.

Slides:



Advertisements
Similar presentations
Lagrange Points Joseph Louis Lagrange was an 18th century mathematician who tackled the famous "three-body problem" in the late 1700s. The problem cannot.
Advertisements

How Many Planets… In Our Solar System? With the advent of powerful new telescopes on the ground and in space, recent new discoveries have been made of.
Multi-planetary systems:.  Binaries  Single Star and Single Planetary Systems  Multi-planetary systems.
Dynamics of the young Solar system Kleomenis Tsiganis Dept. of Physics - A.U.Th. Collaborators: Alessandro Morbidelli (OCA) Hal Levison (SwRI) Rodney Gomes.
Limits of Stability in Earth Co-orbital Motion of Asteroids Martin Connors, Athabasca University Christian Veillet, CFHT R. Greg Stacey, Athabasca University.
Some 3 body problems Kozai resonance 2 planets in mean motion resonance Lee, M. H
N U Neptune crossing 3:22:1 Plutinos classical KBOs scattered KBOs N U.
10Nov2006 Ge/Ay133 More on Jupiter, Neptune, the Kuiper belt, and the early solar system.
On the determination of the probability of collisons of NEAS with the planets MACE 2006 Rudolf Dvorak ADG, Institute of Astronomy University of Vienna.
Discovering Our Solar System Take a voyage that will guide you through the planets csun ENTER.
Trans-Neptunian Objects and Pluto Astronomy 311 Professor Lee Carkner Lecture 21.
The Solar System An Interactive Learning Station.
Based on the definition given by Kasting et al. (1993). The Habitable Zone.
Astronomy Picture of the Day. Question Which of the following provides the most useful information about the Earth's interior? A) drilling B) laser-ranging.
The Size and Distance Scale Of The Solar System Our Earth is just one of several Planets that revolve around our Sun, the primary and central object of.
COMETS, KUIPER BELT AND SOLAR SYSTEM DYNAMICS Silvia Protopapa & Elias Roussos Lectures on “Origins of Solar Systems” February 13-15, 2006 Part I: Solar.
Announcements Laboratory sections start this week. NASA will announce discovery of a new class of planets beyond our solar system on Tuesday, August 31.
The Size and Distance Scale Of The Solar System Our Earth is just one of several Planets that revolve around our Sun, the primary and central object of.
The Dwarf Planet Pluto & New Horizon Dr. Harold Williams Montgomery College Planetarium.
Observing the solar system
Lesson 8a Moons, Asteroids and Rings. Europa These interactions also keep Europa in a slight elliptical orbit as well. But since Europa is farther from.
Foundations of Astronomy
Our Solar System. Our solar system in order from the sun 1.Mercury 2.Venus 3.Earth 4.Mars 5.Asteroid Belt 6.Jupiter 7.Saturn 8.Uranus 9.Neptune 10.Kuiper.
9.2 Comets Our Goals for Learning How do comets get their tails? Where do comets come from?
What do you notice about the Orbit of the Planet’s compared to the Comet’s?
PLUTO AND THE KUIPER BELT Beyond Neptune, the most distant major planet, are a large number of smaller objects, all of which currently known are smaller.
Asteroids updated july 19, Titius-Bode Law (1766) The distances between the planets gets bigger as you go out. Titius & Bode came up with a law.
Asteroids Andrew Horne. What is an asteroid? Apophis.
The Estimated Population of Small NEOs Alan Harris MoreData! Inc. Target NEO 2 Washington, DC, July 9, 2013.
Constellations and Planets in the Night Sky Created for TCSS.
Uranus and Neptune Uranus: general information –Discovered in 1781 (Herschel) –Radius about 4x that of Earth –Mass about 14.5x that of Earth –Nearly featureless.
4 th Grade. Sun Our Brightest Star Approximately one million Earths can fit inside the Sun. The center of the Sun, is made of helium. There are dark blotches.
Orbits.
Kepler’s Laws of Planetary Motion. Debate on Planet Motions Geocentric or Heliocentric Universe.
Planetary Motion It’s what really makes the world go around.
Pluto is the most distant and smallest planet in the solar system. It takes 6 days 9 hours to rotate and 248 Earth years to orbit the Sun. The littlest.
Asteroids updated May 16, Titius-Bode Law (1766) The distances between the planets gets bigger as you go out. Titius & Bode came up with a law that.
Chaotic Dynamics of Near Earth Asteroids. Chaos Sensitivity of orbital evolution to a tiny change of the initial orbit is the defining property of chaos.
Worlds around Distant Suns Mini University June 16, 2003 Among the most significant discoveries of the 20th Century.
V.V.Sidorenko (Keldysh Institute of Applied Mathematics, Moscow, RUSSIA) A.V.Artemyev, A.I.Neishtadt, L.M.Zelenyi (Space Research Institute, Moscow, RUSSIA)
With the advent of powerful new telescopes on the ground and in space, recent new discoveries have been made of objects in the outer regions of our Solar.
Axis – an imaginary line through the center of Earth that connects the North Pole to the South Pole. Earth rotates about its axis once every 24 hours.
Exploring the Solar System GCSE Astronomy – Lesson 26.
Asteroids, Comets, and Meteoroids Asteroids are small, rocky objects. The name “asteroid” actually means ‘star-like bodies’.
Homework 8 Due: Monday, Nov. 28, 9:00 pm, Exam 2: Weds., Nov. 30.
Kepler Finds Earth’s Cousin
1 Interplanetary Magnetic Flux Enhancements as seen by STEREO C.T. Russell, L.K. Jian and J.G. Luhmann 18 th STEREO Science Working Group April Meudon,
The Organization of the Solar System and Planetary Motion
Space Sixth Grade SOL 6.8. Questions you must be able to answer 1. Describe the planets and their relative positions from the sun. 2. Compare the characteristics.
Asteroids: little worlds Space between orbits of Mars and Jupiter seems empty of planets.
THE SOLAR SYSTEM. The Solar System The Sun What does the Sun do for planet? 1. Energy from the sun heats up Earth’s water. 2. Plants use the Sun’s energy.
The outer solar system: some points of physics A few points of physics I didn’t deal with earlier.
Title your notes: Models of the Solar System
Some problems in the optimization of the LISA orbits Guangyu Li 1 , Zhaohua Yi 1,2 , Yan Xia 1 Gerhard Heinzel 3 Oliver Jennrich 4 1 、 Purple Mountain.
Kepler’s Laws of Planetary Motion - 3 Laws -. Elliptical Orbits Planets travel in elliptical orbits with the sun at one focus. Furthest point = Aphelion.
DYNAMICAL EVOLUTION OF THE SEINAJOKI ASTEROID FAMILY Vladimir Đošović Bojan Novaković The sixth Symposium "Mathematics and Applications" 17. October2015.
The Search for Another Earth Exoplanets and the Kepler Spacecraft.
The Solar System Chapter 29 Review.
Celestial Mechanics VI The N-body Problem: Equations of motion and general integrals The Virial Theorem Planetary motion: The perturbing function Numerical.
Chapter 4: Phases of the Moon & Planets © BRIEF
Unit 5 Lesson 2. Vocabulary  Solar System: A star and all the planets and other objects that revolve around it.  Planet: A body that revolves around.
Celestial Mechanics V Circular restricted three-body problem
Formation of the Solar System Section 28.1 Modeling the Solar System This geocentric, or Earth-centered, model could not readily explain some aspects of.
3-4. The Tisserand Relation
Astronomical Institute AS CR, Ondřejov Observatory, Czech Republic
MOON PHASES: Tonight's Moon phase (Image courtesy of U. S
Resonant and Co-orbital Asteroids Associated with Earth
The Size and Distance Scale Of The Solar System
Asteroids.
Planetary Orbits Recall eccentricity e defined by:
Presentation transcript:

Limits of Stability in Earth Co-orbital Motion of Asteroids Martin Connors, Athabasca University Christian Veillet, CFHT R. Greg Stacey, Athabasca University & UofA Ramon Brasser, Queen’s University Paul Wiegert, UWO Seppo Mikkola, Tuorla Observatory Kimmo A. Innanen, York University CASCA 2006, Calgary

There are presently 25 asteroids known with semimajor axis a between 0.99 and 1.01 AU and thus potentially affected by 1:1 resonant interaction with Earth. On average they follow Earth’s orbit so are called co-orbital. Of these, four are in horseshoe orbits, three are currently quasi-satellites, and at least one has a complex high-e high-i interaction (Cruithne).

2002 AA29 and 2003 YN107 move on low- eccentricity orbits very similar to that of the Earth, with moderate inclination i of 11 and 4 degrees. These objects both have horseshoe orbits with respect to Earth and are capable of being captured as quasisatellites (which 2003 YN107 currently is).

2002 AA29 has a horseshoe orbit, approaching Earth and being perturbed to move away. This is a classic example of Kepler’s third law with change in a. The full orbit is not shown, it passes the other side of the Sun. Libration period ca. 190 yr.

This results in a characteristic alternation of the semimajor axis around 1.0 AU

2003 YN107 has a similar horseshoe behavior at times but lower inclination. It is currently trapped as a quasi-satellite near Earth.

During QS the semimajor axis stays near 1.0 and eccentricity changes notably YN107 brief QS

Two other objects are known to have horseshoe orbits deviating further from Earth's orbit (2000 PH5) and short-arc object 2001 GO2 have eccentricities of about 0.2 and low inclinations. They move ‘in and out’ more and ‘up and down’ less than the preceding objects.

2001 GO2 (a short arc object) and 2000 PH5 have similar horseshoe orbits GO2 will do QS motion in the gap of its horseshoe (insert).

Motion of Quasi-Satellite – Inertial to Corotating Frames In the inertial frame the QS remains on one side of the planet. Relative to the planet the QS appears to ‘orbit’ once a year

Quasi-Satellite in the corotating frame appears to follow a bean-shaped orbit. In most known cases the apparent inclination is high (unlike in this clip). Google “Paul Wiegert UWO” for more info & animations.

2004 GU9 has a very regular quasi-satellite state resembling a high- inclination orbit of Earth. The heliocentric inclination is 13.6º and eccentricity This state lasts years. Top View – note closeness to Earth Side View – note high apparent i

2006 FV35 is a recently discovered quasi-satellite, already well-observed with a good orbit. Its inclination is 7.1º and eccentricity The high e guarantees a short lifetime as it is both Mars and Venus crossing. 600 years of motion – colour change at present to show libration

2006 FV 35 shows typical QS behaviour of a libration and change in e. The large e (0.377) makes it planet crossing. It encounters Venus in about 750 years and is scattered out of QS.

2004 FU 162 was our closest nonimpacting visitor. It is a short arc (1-night) object so the discussion is hypothetical based on the best orbit. The a behaviour shows horseshoe libration as does the complicated distance. Fear Factor – these can’t hit us, or can they…

The remaining objects have eccentricity higher than 0.2 and may have high inclinations. At least one such object, 3753 Cruithne, has a complex horseshoe-like orbit with respect to Earth, but most do not show resonant interaction.

We find that some of the co-orbital asteroids are suitable targets for space missions. The known objects on very Earth-like orbits are not energetically the most favorable, largely due to their inclinations. We follow Shoemaker & Helin 1978 for delta-Vs.

Among 2561 NEAs the delta-V needed for rendezvous is minimal at a=1.0. The sample is biased by e needed to discover if a<1.0.

Low-eccentricity target orbits are energetically favored, but the dependence is not strong. For example, Hayabusa target Itokawa has e=0.28 but is only 29 th on the list.

These considerations suggest low-e objects with semimajor axis close to 1.0 will be energetically favorable as targets. Earth horseshoe objects have these characteristics. Shoemaker already in 1978 suggested Earth Trojans would be favorable but none are known. We are looking….bad luck so far….

Unfortunately, known horseshoe objects have high e or i. If … 2002 AA29 had very low i, it could be one of the most energetically favored.

Intuitively it seems low-e low-i HS orbits should be less stable. A clone study of 2002 AA29 shows a stable band around i=5º and not lower.

We find that despite the interesting dynamics and naïve considerations that HS objects should make good targets, we are unlikely to find low-i HS objects as needed. We have not yet discussed Earth Trojans (ETs) since using only known objects or their clones. ETs could be good for long-duration missions. They potentially could have primordial material.

2002 AA Finding Co-orbitals and Earth Trojans Co-orbitals are currently usually found when near Earth (by LINEAR). Scanning high latitudes could be a good place to look and currently undersurveyed. For Trojans, the search region is smaller. CFHT searches for 1º/day objects in this region could find both types of object.

Advertisement: See poster by Shelton et al. for our Athabasca University Robotic Telescope (AURT) project to patrol high latitudes from a dark site. See Lerner et al. poster about our adaptation of Petit pipeline for faster-moving objects and use with CFHT and AURT.

If … somewhat better HS targets are found… Relatively long periods spent near Earth when at one end of a horseshoe orbit favor mission operations. Earth-like orbits can favor short missions (manned?). The small size of objects known to date would present a targeting challenge but may mean lack of regolith.

The co-orbital objects investigated to date have shown relatively short periods of stability in their current orbits and are thus not likely primordial. They likely are recent arrivals from the asteroid belt, which is also the case for most other NEAs. Earth Trojans could be the place to find primordial material from the Earth formation zone. Either one would be a great spacecraft target.

Acknowledgements and Reference Rob Whiteley kindly supplied rendezvous results used for comparison purposes. Initial parameters were taken from the MPC and NeoDys =================================== Shoemaker, E. M. & E. F. Helin, Earth- Approaching Asteroids as Targets for Exploration, in Asteroids: An Exploration Assessment, NASA, Washington, 1978.