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LETTER                                                                                                                                                          doi:10.1038/nature10233




Earth’s Trojan asteroid
Martin Connors1,2, Paul Wiegert3 & Christian Veillet4


It was realized in 1772 that small bodies can stably share the same                               between Earth and L3. Interaction with Earth at the near-Earth end of
orbit as a planet if they remain near ‘triangular points’ 606 ahead of                            the tadpole results in a rapid decrease in the object’s semimajor axis, a,
or behind it in the orbit1. Such ‘Trojan asteroids’ have been found co-                           making it increase its angular speed (Kepler’s third law) and outpace
orbiting with Jupiter2, Mars3 and Neptune4. They have not hitherto                                Earth. This is currently taking place. Slow resonant interaction at the
been found associated with Earth, where the viewing geometry poses                                other parts of the tadpole increases a, making the object slow gradually
difficulties for their detection5, although other kinds of co-orbital                             such that it again approaches Earth. In the current cycle, this will take
asteroid (horseshoe orbiters6 and quasi-satellites7) have been                                    place in the years AD 2050–2350, approximately. Repetition of this cycle
observed8. Here we report an archival search of infrared data for                                 leads to a sawtooth pattern in a as a function of time (Fig. 1c).
possible Earth Trojans, producing the candidate 2010 TK7. We sub-                                    The present motion of 2010 TK7 is well established, but there are
sequently made optical observations which established that 2010                                   inherent limits on our ability to compute orbits into the past or future.
TK7 is a Trojan companion of Earth, librating around the leading                                  Chaos limits the accuracy of computations of this asteroid’s position
Lagrange triangular point, L4. Its orbit is stable over at least ten                              over timescales18 greater than about 250 yr. However, we can still
thousand years.                                                                                   discuss the basic nature of its orbit with confidence by computing
   The existence of Trojan asteroids of other planets raises the question                         the motion of many ‘dynamical clones’ whose orbital parameters vary7
of whether such companions could exist for Earth. Despite studies                                 within the limits set by observations. Approximately 1,800 yr in the
showing that such bodies could be relatively stable9 and may wander                               past, and more than 5,000 yr in the future, the 100 clone orbits we
relatively far from the Lagrange points5, they would dwell mostly in the
daylight sky as seen from Earth, making detection difficult. Indeed,                              a         (AU)
they hitherto have not been observed10,11. The launch of the Wide-field                                     1.0
Infrared Survey Explorer (WISE) by NASA in 200912 provided                                                                                                         L4
improved viewing circumstances that made possible new detections
of over 500 near-Earth objects13. WISE searched large areas of sky
always 90u from the Sun, with high efficiency for asteroidal bodies
                                                                                                            0.5
and good astrometric accuracy. Examining WISE discoveries in the
expectation that Earth co-orbital objects, possibly including a Trojan,
could be found, resulted in two promising candidates, 2010 SO16 and
2010 TK7. Both are larger than most co-orbital objects, being several                                                 L3                           Sun                   Earth
                                                                                                            0.0
hundred metres in diameter, and 2010 SO16 is a horseshoe orbiter14.
We identified 2010 TK7 as probably being an Earth Trojan, on the basis                                             −1.0         −0.5            0.0             0.5              1.0 (AU)
of positions measured over a six-day arc in late 2010. Observations
                                                                                                  b                                                                                    360
made at the University of Hawaii (D. Tholen, personal communica-                                             L5                                                                        300




                                                                                                                                                                                               θ – θE (°)
tion) and the Canada–France–Hawaii Telescope15 in April 2011, after                                                                                                                    240
                                                                                                             L3                                                                        180
the object had for months been in an unfavourable position as seen                                                                                                                     120
                                                                                                             L4                                                                         60
from Earth, so greatly improved the knowledge of its orbit that we can                                                                                                                   0
                                                                                                  c        1.003
state with certainty that 2010 TK7 is an Earth Trojan.                                                     1.002
   The ‘tadpole’ motion of 2010 TK7, which is characteristic of Trojan                                     1.001
                                                                                                  a (AU)




                                                                                                           1.000
asteroids, is shown in Fig. 1 in the frame co-rotating with Earth (see                                     0.999
Supplementary Information for three-dimensional depictions of the                                          0.998
                                                                                                           0.997
motion). The 1-yr-averaged curve shows the centre of motion librating                                          –400   0    400 800 1200 1600 2000 2400 2800 3200 3600 4000
about L4, the Lagrange point 60u ahead of Earth. The period of this                                                                            Year
motion is at present 395 yr. Superposed on this is an annual motion or                            Figure 1 | Orbital parameters of asteroid 2010 TK7. a, Path over one Trojan
epicycle2,16,17 (not shown for clarity). This mode of display emphasizes                          libration from AD 2010 to 2405 in the co-rotating reference frame. In this frame,
the longitudinal motion despite the enhanced radial scale: the asteroid’s                         Earth is stationary and the average position of the asteroid librates about L4 in a
mean position drifts along the red line, from the ‘head’ of the tadpole,                          ‘tadpole’ orbit. Both Earth and the asteroid revolve about the Sun with periods
near Earth, to the far ‘tail’, where it is nearly on the opposite side of the                     close to 1 yr, and slow changes in their relative positions are best seen in the co-
Sun from the Earth. The relatively large eccentricity, of e 5 0.191, results                      rotating frame. The difference between the asteroid’s semimajor axis, a, and a
in an annual heliocentric radial motion between roughly 0.81 and                                  circle of radius 1 AU (an astronomical unit (AU) is the Earth–Sun distance) is
                                                                                                  multiplied by a factor of 20 for clarity, and Earth and the Sun are not shown to
1.19 AU. The inclination of 2010 TK7 is about i 5 20.9u, so there is
                                                                                                  scale. Black lines indicate a and longitude relative to Earth daily; the red curve
significant motion perpendicular to Earth’s orbital plane. The asteroid’s                         shows the annual average. b, Longitude relative to Earth, h 2 hE, over the period
eccentricity and inclination produce a large epicycle, which is respons-                          420 BC to AD 4200. A ‘jump’ from L5 libration to the present L4 libration took
ible for the visibility of the object at the solar elongation of 90u, as                          place in around AD 400. Black and red lines indicate daily and averaged values,
observed by WISE; and it is now at the near-Earth end of the tadpole.                             as in a. The grey band is the period of the present libration. c, Semimajor axis
In the present epoch, the longitude remains in the sector of L4, trapped                          daily values. Initial conditions (best orbital solution) are given in Table 1.
1
 Athabasca University, 1 University Drive, Athabasca, Alberta T9S 3A3, Canada. 2Department of Earth and Space Sciences, UCLA, Los Angeles, California 90095, USA. 3Department of Physics and
Astronomy, The University of Western Ontario, London, Ontario N6A 3K7, Canada. 4Canada–France–Hawaii Telescope, Kamuela, Hawaii 96743, USA.


                                                                                                                                   2 8 J U LY 2 0 1 1 | V O L 4 7 5 | N AT U R E | 4 8 1
                                                         ©2011 Macmillan Publishers Limited. All rights reserved
RESEARCH LETTER

computed diverged sufficiently that we must say that the asteroid’s                   Table 1 | Heliocentric orbital elements of 2010 TK7
precise behaviour cannot be predicted with certainty outside that                     Epoch                                                               JD 2455600.5
,7,000-yr span. The range of behaviour shown by the clones and, thus,                 Semimajor axis, a                                                   1.0004078 AU
                                                                                      Eccentricity, e                                                     0.1908177
possible for the real object includes making transitions to horseshoe
                                                                                      Inclination, i                                                      20.87984u
modes and ‘jumping’ between Lagrange points. Short-term unstable                      Argument of perihelion                                              45.86009u
libration about L3, the Lagrange point on the other side of the Sun from              Longitude of ascending node                                         96.54190u
Earth, can occur as a result of the asteroid’s large inclination. Such orbits         Mean anomaly                                                        20.30069u
were theorized as early as 192017, but no real object had until now been              Results in the figures were obtained using these initial conditions in the Mercury integrator24 (verified in
                                                                                      the near-present using the JPL Horizons system25). The RADAU26 option was used with 1-d spacing for
suspected to enter them.                                                              the eight planets, Pluto and the Earth–Moon barycentre. Clone studies included the eight planets and
   Jumping from one Lagrange point to the other is a behaviour prev-                  the Moon27, with variations7 among the orbital elements of the order of the last significant digit shown.
iously attributed to the Jupiter Trojan 1868 Thersites19, and was found               The Julian date (JD) shown corresponds to 0:00 UT on 8 February 2011.

in about half of the clone orbits. Here, the large eccentricity leads to                 Chaotic effects have a large role in the behaviour of this asteroid. Its
longitudinal excursions (Kepler’s second law), including when near L3.                sensitivity to small influences when in the vicinity of L3 allows the
In Fig. 2, these are shown to have allowed (in about AD 500) a rapid                  range of outcomes seen among the clones. The overall Trojan beha-
transition of 2010 TK7 from L5 to the present L4 libration. The libration             viour is dictated by 1:1 orbital resonance with Earth, but non-resonant
now remains only in the sector of L4 and is relatively stable, in a                   effects of Jupiter are 80 times stronger than those of Earth when Jupiter
classic16 Trojan pattern, although of large amplitude.                                is at the same celestial longitude as L3. Such influences, demonstrated
                                                                                      by the ‘banding’ seen in Fig. 2, alter the asteroid’s chaotic behaviour.
                                                                                      Many clone orbits make repeated transitions between the Lagrange
a                                                                                     points, such that the chaos can be stable20, with L4 and L5 each defining
         1.003
                                                                                      permitted regions of phase space. Knowledge of the orbit will improve
                                                                                      as it is observed over the years, but its chaotic nature dictates that
         1.002
                                                                                      dynamics-based discussions of the origin and fate of 2010 TK7, and
                                                                                      its relationship to other bodies, will necessarily remain statistical in
         1.001                                                                        nature.
                           L4                                     L5
                                                                                         Earth Trojan asteroids have been proposed as natural candidates for
a (AU)




         1.000                                                                        spacecraft rendezvous missions21. However, the large inclination of
                                                                                      2010 TK7 results in a Dv of 9.4 km s21 being required, whereas other
         0.999                                                                        near-Earth asteroids have values of Dv less than 4 km s21. The reported
                                                                                      absolute magnitude, 20.7 mag, puts the diameter of 2010 TK7 at 300 m
                                                                                      with an assumed albedo of 0.1 (ref. 22), which makes it relatively large
         0.998
                                                                                      among the near-Earth asteroid population. No spectral or colour
                                                                                      information is as yet available to determine whether the asteroid is
         0.997                                                                        in any other way unusual.
b                0    60         120        180          240           300     360
         1.003
                                                                                      Received 11 April; accepted 27 May 2011.

         1.002                                                                        1.    Wilson, C. in Planetary Astronomy from the Renaissance to the Rise of Astrophysics.
                                                                                            Part B: The Eighteenth and Nineteenth Centuries (eds Taton, R. & Wilson, C.)
                                                                                            108–130 (Cambridge, 1995).
         1.001                                                                        2.    Stacey, R. G. & Connors, M. A centenary survey of orbits of co-orbitals of Jupiter.
                                                                                            Planet. Space Sci. 56, 358–367 (2008).
                           L4                   L3                                    3.    Connors, M. et al. A survey of orbits of co-orbitals of Mars. Planet. Space Sci. 53,
a (AU)




         1.000                                                                              617–624 (2005).
                                                                                      4.    Almeida, A. J. C., Peixinho, N. & Correia, A. C. M. Neptune Trojans and Plutinos:
                                                                                            colors, sizes, dynamics, and their possible collisions. Astron. Astrophys. 508,
         0.999                                                                              1021–1030 (2009).
                                                                                      5.    Wiegert, P., Innanen, K. A. & Mikkola, S. Earth Trojan asteroids: a study in support of
                                                                                            observational searches. Icarus 145, 33–43 (2000).
         0.998                                                                        6.    Wiegert, P., Innanen, K. A. & Mikkola, S. An asteroidal companion to the Earth.
                                                                                            Nature 387, 685–686 (1997).
                                                                                      7.    Brasser, R. et al. Transient co-orbital asteroids. Icarus 171, 102–109 (2004).
         0.997                                                                        8.    Connors, M. et al. Discovery of an asteroid and quasi-satellite in an Earth-like
                 0    60         120        180          240           300     360          horseshoe orbit. Meteor. Planet. Sci. 37, 1435–1441 (2002).
                                          θ – θE (°)                                  9.    Mikkola, S. & Innanen, K. A. Studies in solar system dynamics. II. The stability of
                                                                                            Earth’s Trojans. Astron. J. 100, 290–293 (1990).
Figure 2 | Semimajor axis versus relative longitude for 2010 TK7.                     10.   Whitely, R. J. & Tholen, D. J. A. CCD search for Lagrangian asteroids of the Earth-
                                                                                            Sun system. Icarus 136, 154–167 (1998).
a, Libration during the period AD 1–800, featuring a ‘jump’ from libration            11.   Connors, M. et al. Initial results of a survey of Earth’s L4 point for possible Earth
initially about L5 (right) to the present libration around L4. As in Fig. 1, black          Trojan asteroids. Bull. Am. Astron. Soc. 32, 1019 (2000).
lines indicate daily values and red lines indicate the annual averages. When the      12.   Wright, E. L. et al. The Wide-field Infrared Survey Explorer (WISE): mission
asteroid is near a relative longitude, h 2 hE, of about 180u, the annual excursions         description and initial on-orbit performance. Astron. J. 140, 1868–1881 (2010).
in relative longitude can cause it to cross L3. This crossing can trigger a rapid     13.   Mainzer, A. et al. Preliminary results from NEOWISE: an enhancement to the Wide-
                                                                                            Field Infrared Survey Explorer for solar system science. Astrophys. J. 731, 53
transition or ‘jump’ between librational modes. Clone studies show that the
                                                                                            (2011).
chaotic behaviour of the asteroid is due mainly to a great sensitivity to non-        14.   Christou, A. A. & Asher, D. J. A long-lived horseshoe companion to the Earth. Mon.
resonant perturbations when near L3. Libration about L5 results in an average               Not. R. Astron. Soc. advance online publication, doi:10.1111/j.1365-
longitude 120u different from that for libration about L4. Such a large change              2966.2011.18595.x (12 April 2011).
resulting from small perturbations (when near L3) is characteristic of chaos.         15.   Boulade, O. et al. Development of MegaCam, the next-generation wide-field
b, Present (AD 2010–2405) libration about L4. The location of L3 is shown for               imaging camera for the 3.6-m Canada-France-Hawaii Telescope. Proc. SPIE 2008,
                                                                                            657–668 (2000).
reference but the relative longitude in the era after AD 800 does not cross it,       16.   Murray, C. D. & Dermott, S. F. Solar System Dynamics 63–110 (Cambridge Univ.
resulting in the current stability of the orbit. The apparent banding in both               Press, 1999).
panels is due to changes in semimajor axis and has a predominant period of            17.   Moulton, F. R. Periodic Orbits 299–324, 151–198 (Carnegie Institute, 1920).
roughly 12 yr; therefore, it is probably mainly caused by Jupiter perturbations.      18.   Whipple, A. L. Lyapunov times of the inner asteroids. Icarus 115, 347–353 (1995).

4 8 2 | N AT U R E | VO L 4 7 5 | 2 8 J U LY 2 0 1 1
                                                       ©2011 Macmillan Publishers Limited. All rights reserved
LETTER RESEARCH

19. Tsiganis, K., Dvorak, R. & Pilat-Lohinger, E. Thersites: a ‘jumping’ Trojan? Astron.       Supplementary Information is linked to the online version of the paper at
    Astrophys. 354, 1091–1100 (2000).                                                          www.nature.com/nature.
20. Milani, A. & Nobili, A. M. An example of stable chaos in the Solar System. Nature
    357, 569–571 (1992).                                                                       Acknowledgements We thank the WISE team and JPL and NEODyS (University of Pisa)
21. Stacey, R. G. & Connors, M. Delta-v requirements for earth co-orbital rendezvous           data services. Support came from Canada’s Natural Sciences and Engineering
    missions. Planet. Space Sci. 57, 822–829 (2009).                                           Research Council and Research Chairs. Problems with some 2010 TK7 positions
22. Bowell, E. et al. in Asteroids II (eds Binzel, R., Gehrels, T. & Matthews, M.) 524–556     reported in ref. 23 were pointed out by T. Spahr and D. Tholen. We are grateful to them
    (Univ. Arizona Press, 1989).                                                               for data reductions provided, and to D. Tholen, M. Micheli and G. T. Elliot for
23. MPEC 2011-G37: Daily Orbit Update (2011 Apr. 5 UT). IAU Minor Planet Center                observations made in support of this study.
    Æhttp://www.minorplanetcenter.org/mpec/K11/K11G37.htmlæ (2011).                            Author Contributions The authors contributed equally to this work. M.C. and P.W.
24. Chambers, J. E. A hybrid symplectic integrator that permits close encounters               concentrated on dynamical calculations, and C.V. concentrated on observations and
    between massive bodies. Mon. Not. R. Astron. Soc. 304, 793–799 (1999).                     associated data reduction.
25. Giogini, J. D. et al. JPL’s online solar system data service. Bull. Am. Astron. Soc. 28,
    1158 (1996).                                                                               Author Information Reprints and permissions information is available at
26. Everhart, E. in Dynamics of Comets: Their Origin and Evolution (eds Carusi, A. &           www.nature.com/reprints. The authors declare no competing financial interests.
    Valsecchi, G. B.) 185–202 (Kluwer, 1985).                                                  Readers are welcome to comment on the online version of this article at
27. Standish, E. M. Planetary and Lunar Ephemerides DE406/LE406. Tech. Report IOM              www.nature.com/nature. Correspondence and requests for materials should be
    312.F-98–048 (NASA Jet Propulsion Laboratory, 1998).                                       addressed to M.C. (martinc@athabascau.ca).




                                                                                                                            2 8 J U LY 2 0 1 1 | V O L 4 7 5 | N AT U R E | 4 8 3
                                                        ©2011 Macmillan Publishers Limited. All rights reserved

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Asteroide troiano

  • 1. LETTER doi:10.1038/nature10233 Earth’s Trojan asteroid Martin Connors1,2, Paul Wiegert3 & Christian Veillet4 It was realized in 1772 that small bodies can stably share the same between Earth and L3. Interaction with Earth at the near-Earth end of orbit as a planet if they remain near ‘triangular points’ 606 ahead of the tadpole results in a rapid decrease in the object’s semimajor axis, a, or behind it in the orbit1. Such ‘Trojan asteroids’ have been found co- making it increase its angular speed (Kepler’s third law) and outpace orbiting with Jupiter2, Mars3 and Neptune4. They have not hitherto Earth. This is currently taking place. Slow resonant interaction at the been found associated with Earth, where the viewing geometry poses other parts of the tadpole increases a, making the object slow gradually difficulties for their detection5, although other kinds of co-orbital such that it again approaches Earth. In the current cycle, this will take asteroid (horseshoe orbiters6 and quasi-satellites7) have been place in the years AD 2050–2350, approximately. Repetition of this cycle observed8. Here we report an archival search of infrared data for leads to a sawtooth pattern in a as a function of time (Fig. 1c). possible Earth Trojans, producing the candidate 2010 TK7. We sub- The present motion of 2010 TK7 is well established, but there are sequently made optical observations which established that 2010 inherent limits on our ability to compute orbits into the past or future. TK7 is a Trojan companion of Earth, librating around the leading Chaos limits the accuracy of computations of this asteroid’s position Lagrange triangular point, L4. Its orbit is stable over at least ten over timescales18 greater than about 250 yr. However, we can still thousand years. discuss the basic nature of its orbit with confidence by computing The existence of Trojan asteroids of other planets raises the question the motion of many ‘dynamical clones’ whose orbital parameters vary7 of whether such companions could exist for Earth. Despite studies within the limits set by observations. Approximately 1,800 yr in the showing that such bodies could be relatively stable9 and may wander past, and more than 5,000 yr in the future, the 100 clone orbits we relatively far from the Lagrange points5, they would dwell mostly in the daylight sky as seen from Earth, making detection difficult. Indeed, a (AU) they hitherto have not been observed10,11. The launch of the Wide-field 1.0 Infrared Survey Explorer (WISE) by NASA in 200912 provided L4 improved viewing circumstances that made possible new detections of over 500 near-Earth objects13. WISE searched large areas of sky always 90u from the Sun, with high efficiency for asteroidal bodies 0.5 and good astrometric accuracy. Examining WISE discoveries in the expectation that Earth co-orbital objects, possibly including a Trojan, could be found, resulted in two promising candidates, 2010 SO16 and 2010 TK7. Both are larger than most co-orbital objects, being several L3 Sun Earth 0.0 hundred metres in diameter, and 2010 SO16 is a horseshoe orbiter14. We identified 2010 TK7 as probably being an Earth Trojan, on the basis −1.0 −0.5 0.0 0.5 1.0 (AU) of positions measured over a six-day arc in late 2010. Observations b 360 made at the University of Hawaii (D. Tholen, personal communica- L5 300 θ – θE (°) tion) and the Canada–France–Hawaii Telescope15 in April 2011, after 240 L3 180 the object had for months been in an unfavourable position as seen 120 L4 60 from Earth, so greatly improved the knowledge of its orbit that we can 0 c 1.003 state with certainty that 2010 TK7 is an Earth Trojan. 1.002 The ‘tadpole’ motion of 2010 TK7, which is characteristic of Trojan 1.001 a (AU) 1.000 asteroids, is shown in Fig. 1 in the frame co-rotating with Earth (see 0.999 Supplementary Information for three-dimensional depictions of the 0.998 0.997 motion). The 1-yr-averaged curve shows the centre of motion librating –400 0 400 800 1200 1600 2000 2400 2800 3200 3600 4000 about L4, the Lagrange point 60u ahead of Earth. The period of this Year motion is at present 395 yr. Superposed on this is an annual motion or Figure 1 | Orbital parameters of asteroid 2010 TK7. a, Path over one Trojan epicycle2,16,17 (not shown for clarity). This mode of display emphasizes libration from AD 2010 to 2405 in the co-rotating reference frame. In this frame, the longitudinal motion despite the enhanced radial scale: the asteroid’s Earth is stationary and the average position of the asteroid librates about L4 in a mean position drifts along the red line, from the ‘head’ of the tadpole, ‘tadpole’ orbit. Both Earth and the asteroid revolve about the Sun with periods near Earth, to the far ‘tail’, where it is nearly on the opposite side of the close to 1 yr, and slow changes in their relative positions are best seen in the co- Sun from the Earth. The relatively large eccentricity, of e 5 0.191, results rotating frame. The difference between the asteroid’s semimajor axis, a, and a in an annual heliocentric radial motion between roughly 0.81 and circle of radius 1 AU (an astronomical unit (AU) is the Earth–Sun distance) is multiplied by a factor of 20 for clarity, and Earth and the Sun are not shown to 1.19 AU. The inclination of 2010 TK7 is about i 5 20.9u, so there is scale. Black lines indicate a and longitude relative to Earth daily; the red curve significant motion perpendicular to Earth’s orbital plane. The asteroid’s shows the annual average. b, Longitude relative to Earth, h 2 hE, over the period eccentricity and inclination produce a large epicycle, which is respons- 420 BC to AD 4200. A ‘jump’ from L5 libration to the present L4 libration took ible for the visibility of the object at the solar elongation of 90u, as place in around AD 400. Black and red lines indicate daily and averaged values, observed by WISE; and it is now at the near-Earth end of the tadpole. as in a. The grey band is the period of the present libration. c, Semimajor axis In the present epoch, the longitude remains in the sector of L4, trapped daily values. Initial conditions (best orbital solution) are given in Table 1. 1 Athabasca University, 1 University Drive, Athabasca, Alberta T9S 3A3, Canada. 2Department of Earth and Space Sciences, UCLA, Los Angeles, California 90095, USA. 3Department of Physics and Astronomy, The University of Western Ontario, London, Ontario N6A 3K7, Canada. 4Canada–France–Hawaii Telescope, Kamuela, Hawaii 96743, USA. 2 8 J U LY 2 0 1 1 | V O L 4 7 5 | N AT U R E | 4 8 1 ©2011 Macmillan Publishers Limited. All rights reserved
  • 2. RESEARCH LETTER computed diverged sufficiently that we must say that the asteroid’s Table 1 | Heliocentric orbital elements of 2010 TK7 precise behaviour cannot be predicted with certainty outside that Epoch JD 2455600.5 ,7,000-yr span. The range of behaviour shown by the clones and, thus, Semimajor axis, a 1.0004078 AU Eccentricity, e 0.1908177 possible for the real object includes making transitions to horseshoe Inclination, i 20.87984u modes and ‘jumping’ between Lagrange points. Short-term unstable Argument of perihelion 45.86009u libration about L3, the Lagrange point on the other side of the Sun from Longitude of ascending node 96.54190u Earth, can occur as a result of the asteroid’s large inclination. Such orbits Mean anomaly 20.30069u were theorized as early as 192017, but no real object had until now been Results in the figures were obtained using these initial conditions in the Mercury integrator24 (verified in the near-present using the JPL Horizons system25). The RADAU26 option was used with 1-d spacing for suspected to enter them. the eight planets, Pluto and the Earth–Moon barycentre. Clone studies included the eight planets and Jumping from one Lagrange point to the other is a behaviour prev- the Moon27, with variations7 among the orbital elements of the order of the last significant digit shown. iously attributed to the Jupiter Trojan 1868 Thersites19, and was found The Julian date (JD) shown corresponds to 0:00 UT on 8 February 2011. in about half of the clone orbits. Here, the large eccentricity leads to Chaotic effects have a large role in the behaviour of this asteroid. Its longitudinal excursions (Kepler’s second law), including when near L3. sensitivity to small influences when in the vicinity of L3 allows the In Fig. 2, these are shown to have allowed (in about AD 500) a rapid range of outcomes seen among the clones. The overall Trojan beha- transition of 2010 TK7 from L5 to the present L4 libration. The libration viour is dictated by 1:1 orbital resonance with Earth, but non-resonant now remains only in the sector of L4 and is relatively stable, in a effects of Jupiter are 80 times stronger than those of Earth when Jupiter classic16 Trojan pattern, although of large amplitude. is at the same celestial longitude as L3. Such influences, demonstrated by the ‘banding’ seen in Fig. 2, alter the asteroid’s chaotic behaviour. Many clone orbits make repeated transitions between the Lagrange a points, such that the chaos can be stable20, with L4 and L5 each defining 1.003 permitted regions of phase space. Knowledge of the orbit will improve as it is observed over the years, but its chaotic nature dictates that 1.002 dynamics-based discussions of the origin and fate of 2010 TK7, and its relationship to other bodies, will necessarily remain statistical in 1.001 nature. L4 L5 Earth Trojan asteroids have been proposed as natural candidates for a (AU) 1.000 spacecraft rendezvous missions21. However, the large inclination of 2010 TK7 results in a Dv of 9.4 km s21 being required, whereas other 0.999 near-Earth asteroids have values of Dv less than 4 km s21. The reported absolute magnitude, 20.7 mag, puts the diameter of 2010 TK7 at 300 m with an assumed albedo of 0.1 (ref. 22), which makes it relatively large 0.998 among the near-Earth asteroid population. No spectral or colour information is as yet available to determine whether the asteroid is 0.997 in any other way unusual. b 0 60 120 180 240 300 360 1.003 Received 11 April; accepted 27 May 2011. 1.002 1. Wilson, C. in Planetary Astronomy from the Renaissance to the Rise of Astrophysics. Part B: The Eighteenth and Nineteenth Centuries (eds Taton, R. & Wilson, C.) 108–130 (Cambridge, 1995). 1.001 2. Stacey, R. G. & Connors, M. A centenary survey of orbits of co-orbitals of Jupiter. Planet. Space Sci. 56, 358–367 (2008). L4 L3 3. Connors, M. et al. A survey of orbits of co-orbitals of Mars. Planet. Space Sci. 53, a (AU) 1.000 617–624 (2005). 4. Almeida, A. J. C., Peixinho, N. & Correia, A. C. M. Neptune Trojans and Plutinos: colors, sizes, dynamics, and their possible collisions. Astron. Astrophys. 508, 0.999 1021–1030 (2009). 5. Wiegert, P., Innanen, K. A. & Mikkola, S. Earth Trojan asteroids: a study in support of observational searches. Icarus 145, 33–43 (2000). 0.998 6. Wiegert, P., Innanen, K. A. & Mikkola, S. An asteroidal companion to the Earth. Nature 387, 685–686 (1997). 7. Brasser, R. et al. Transient co-orbital asteroids. Icarus 171, 102–109 (2004). 0.997 8. Connors, M. et al. Discovery of an asteroid and quasi-satellite in an Earth-like 0 60 120 180 240 300 360 horseshoe orbit. Meteor. Planet. Sci. 37, 1435–1441 (2002). θ – θE (°) 9. Mikkola, S. & Innanen, K. A. Studies in solar system dynamics. II. The stability of Earth’s Trojans. Astron. J. 100, 290–293 (1990). Figure 2 | Semimajor axis versus relative longitude for 2010 TK7. 10. Whitely, R. J. & Tholen, D. J. A. CCD search for Lagrangian asteroids of the Earth- Sun system. Icarus 136, 154–167 (1998). a, Libration during the period AD 1–800, featuring a ‘jump’ from libration 11. Connors, M. et al. Initial results of a survey of Earth’s L4 point for possible Earth initially about L5 (right) to the present libration around L4. As in Fig. 1, black Trojan asteroids. Bull. Am. Astron. Soc. 32, 1019 (2000). lines indicate daily values and red lines indicate the annual averages. When the 12. Wright, E. L. et al. The Wide-field Infrared Survey Explorer (WISE): mission asteroid is near a relative longitude, h 2 hE, of about 180u, the annual excursions description and initial on-orbit performance. Astron. J. 140, 1868–1881 (2010). in relative longitude can cause it to cross L3. This crossing can trigger a rapid 13. Mainzer, A. et al. Preliminary results from NEOWISE: an enhancement to the Wide- Field Infrared Survey Explorer for solar system science. Astrophys. J. 731, 53 transition or ‘jump’ between librational modes. Clone studies show that the (2011). chaotic behaviour of the asteroid is due mainly to a great sensitivity to non- 14. Christou, A. A. & Asher, D. J. A long-lived horseshoe companion to the Earth. Mon. resonant perturbations when near L3. Libration about L5 results in an average Not. R. Astron. Soc. advance online publication, doi:10.1111/j.1365- longitude 120u different from that for libration about L4. Such a large change 2966.2011.18595.x (12 April 2011). resulting from small perturbations (when near L3) is characteristic of chaos. 15. Boulade, O. et al. Development of MegaCam, the next-generation wide-field b, Present (AD 2010–2405) libration about L4. The location of L3 is shown for imaging camera for the 3.6-m Canada-France-Hawaii Telescope. Proc. SPIE 2008, 657–668 (2000). reference but the relative longitude in the era after AD 800 does not cross it, 16. Murray, C. D. & Dermott, S. F. Solar System Dynamics 63–110 (Cambridge Univ. resulting in the current stability of the orbit. The apparent banding in both Press, 1999). panels is due to changes in semimajor axis and has a predominant period of 17. Moulton, F. R. Periodic Orbits 299–324, 151–198 (Carnegie Institute, 1920). roughly 12 yr; therefore, it is probably mainly caused by Jupiter perturbations. 18. Whipple, A. L. Lyapunov times of the inner asteroids. Icarus 115, 347–353 (1995). 4 8 2 | N AT U R E | VO L 4 7 5 | 2 8 J U LY 2 0 1 1 ©2011 Macmillan Publishers Limited. All rights reserved
  • 3. LETTER RESEARCH 19. Tsiganis, K., Dvorak, R. & Pilat-Lohinger, E. Thersites: a ‘jumping’ Trojan? Astron. Supplementary Information is linked to the online version of the paper at Astrophys. 354, 1091–1100 (2000). www.nature.com/nature. 20. Milani, A. & Nobili, A. M. An example of stable chaos in the Solar System. Nature 357, 569–571 (1992). Acknowledgements We thank the WISE team and JPL and NEODyS (University of Pisa) 21. Stacey, R. G. & Connors, M. Delta-v requirements for earth co-orbital rendezvous data services. Support came from Canada’s Natural Sciences and Engineering missions. Planet. Space Sci. 57, 822–829 (2009). Research Council and Research Chairs. Problems with some 2010 TK7 positions 22. Bowell, E. et al. in Asteroids II (eds Binzel, R., Gehrels, T. & Matthews, M.) 524–556 reported in ref. 23 were pointed out by T. Spahr and D. Tholen. We are grateful to them (Univ. Arizona Press, 1989). for data reductions provided, and to D. Tholen, M. Micheli and G. T. Elliot for 23. MPEC 2011-G37: Daily Orbit Update (2011 Apr. 5 UT). IAU Minor Planet Center observations made in support of this study. Æhttp://www.minorplanetcenter.org/mpec/K11/K11G37.htmlæ (2011). Author Contributions The authors contributed equally to this work. M.C. and P.W. 24. Chambers, J. E. A hybrid symplectic integrator that permits close encounters concentrated on dynamical calculations, and C.V. concentrated on observations and between massive bodies. Mon. Not. R. Astron. Soc. 304, 793–799 (1999). associated data reduction. 25. Giogini, J. D. et al. JPL’s online solar system data service. Bull. Am. Astron. Soc. 28, 1158 (1996). Author Information Reprints and permissions information is available at 26. Everhart, E. in Dynamics of Comets: Their Origin and Evolution (eds Carusi, A. & www.nature.com/reprints. The authors declare no competing financial interests. Valsecchi, G. B.) 185–202 (Kluwer, 1985). Readers are welcome to comment on the online version of this article at 27. Standish, E. M. Planetary and Lunar Ephemerides DE406/LE406. Tech. Report IOM www.nature.com/nature. Correspondence and requests for materials should be 312.F-98–048 (NASA Jet Propulsion Laboratory, 1998). addressed to M.C. (martinc@athabascau.ca). 2 8 J U LY 2 0 1 1 | V O L 4 7 5 | N AT U R E | 4 8 3 ©2011 Macmillan Publishers Limited. All rights reserved