Log-Normal Distribution and Planetary–Solar Resonance
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Lurking in the Shadows: Wide-Separation Gas Giants As Tracers of Planet Formation
Lurking in the Shadows: Wide-Separation Gas Giants as Tracers of Planet Formation Thesis by Marta Levesque Bryan In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California 2018 Defended May 1, 2018 ii © 2018 Marta Levesque Bryan ORCID: [0000-0002-6076-5967] All rights reserved iii ACKNOWLEDGEMENTS First and foremost I would like to thank Heather Knutson, who I had the great privilege of working with as my thesis advisor. Her encouragement, guidance, and perspective helped me navigate many a challenging problem, and my conversations with her were a consistent source of positivity and learning throughout my time at Caltech. I leave graduate school a better scientist and person for having her as a role model. Heather fostered a wonderfully positive and supportive environment for her students, giving us the space to explore and grow - I could not have asked for a better advisor or research experience. I would also like to thank Konstantin Batygin for enthusiastic and illuminating discussions that always left me more excited to explore the result at hand. Thank you as well to Dimitri Mawet for providing both expertise and contagious optimism for some of my latest direct imaging endeavors. Thank you to the rest of my thesis committee, namely Geoff Blake, Evan Kirby, and Chuck Steidel for their support, helpful conversations, and insightful questions. I am grateful to have had the opportunity to collaborate with Brendan Bowler. His talk at Caltech my second year of graduate school introduced me to an unexpected population of massive wide-separation planetary-mass companions, and lead to a long-running collaboration from which several of my thesis projects were born. -
Long-Term Orbital and Rotational Motions of Ceres and Vesta T
A&A 622, A95 (2019) Astronomy https://doi.org/10.1051/0004-6361/201833342 & © ESO 2019 Astrophysics Long-term orbital and rotational motions of Ceres and Vesta T. Vaillant, J. Laskar, N. Rambaux, and M. Gastineau ASD/IMCCE, Observatoire de Paris, PSL Université, Sorbonne Université, 77 avenue Denfert-Rochereau, 75014 Paris, France e-mail: [email protected] Received 2 May 2018 / Accepted 24 July 2018 ABSTRACT Context. The dwarf planet Ceres and the asteroid Vesta have been studied by the Dawn space mission. They are the two heaviest bodies of the main asteroid belt and have different characteristics. Notably, Vesta appears to be dry and inactive with two large basins at its south pole. Ceres is an ice-rich body with signs of cryovolcanic activity. Aims. The aim of this paper is to determine the obliquity variations of Ceres and Vesta and to study their rotational stability. Methods. The orbital and rotational motions have been integrated by symplectic integration. The rotational stability has been studied by integrating secular equations and by computing the diffusion of the precession frequency. Results. The obliquity variations of Ceres over [ 20 : 0] Myr are between 2◦ and 20◦ and the obliquity variations of Vesta are between − 21◦ and 45◦. The two giant impacts suffered by Vesta modified the precession constant and could have put Vesta closer to the resonance with the orbital frequency 2s s . Given the uncertainty on the polar moment of inertia, the present Vesta could be in this resonance 6 − V where the obliquity variations can vary between 17◦ and 48◦. -
Ghost Imaging of Space Objects
Ghost Imaging of Space Objects Dmitry V. Strekalov, Baris I. Erkmen, Igor Kulikov, and Nan Yu Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, California 91109-8099 USA NIAC Final Report September 2014 Contents I. The proposed research 1 A. Origins and motivation of this research 1 B. Proposed approach in a nutshell 3 C. Proposed approach in the context of modern astronomy 7 D. Perceived benefits and perspectives 12 II. Phase I goals and accomplishments 18 A. Introducing the theoretical model 19 B. A Gaussian absorber 28 C. Unbalanced arms configuration 32 D. Phase I summary 34 III. Phase II goals and accomplishments 37 A. Advanced theoretical analysis 38 B. On observability of a shadow gradient 47 C. Signal-to-noise ratio 49 D. From detection to imaging 59 E. Experimental demonstration 72 F. On observation of phase objects 86 IV. Dissemination and outreach 90 V. Conclusion 92 References 95 1 I. THE PROPOSED RESEARCH The NIAC Ghost Imaging of Space Objects research program has been carried out at the Jet Propulsion Laboratory, Caltech. The program consisted of Phase I (October 2011 to September 2012) and Phase II (October 2012 to September 2014). The research team consisted of Drs. Dmitry Strekalov (PI), Baris Erkmen, Igor Kulikov and Nan Yu. The team members acknowledge stimulating discussions with Drs. Leonidas Moustakas, Andrew Shapiro-Scharlotta, Victor Vilnrotter, Michael Werner and Paul Goldsmith of JPL; Maria Chekhova and Timur Iskhakov of Max Plank Institute for Physics of Light, Erlangen; Paul Nu˜nez of Coll`ege de France & Observatoire de la Cˆote d’Azur; and technical support from Victor White and Pierre Echternach of JPL. -
Two Jovian Planets Around the Giant Star HD 202696: a Growing Population of Packed Massive Planetary Pairs Around Massive Stars?
The Astronomical Journal, 157:93 (13pp), 2019 March https://doi.org/10.3847/1538-3881/aafa11 © 2019. The American Astronomical Society. All rights reserved. Two Jovian Planets around the Giant Star HD 202696: A Growing Population of Packed Massive Planetary Pairs around Massive Stars? Trifon Trifonov1 , Stephan Stock2 , Thomas Henning1 , Sabine Reffert2 , Martin Kürster1 , Man Hoi Lee3,4 , Bertram Bitsch1 , R. Paul Butler5 , and Steven S. Vogt6 1 Max-Planck-Institut für Astronomie, Königstuhl 17, D-69117 Heidelberg, Germany; [email protected] 2 Landessternwarte, Zentrum für Astronomie der Universität Heidelberg, Königstuhl 12, D-69117 Heidelberg, Germany 3 Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong 4 Department of Physics, The University of Hong Kong, Pokfulam Road, Hong Kong 5 Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC 20015, USA 6 UCO/Lick Observatory, Department of Astronomy and Astrophysics, University of California at Santa Cruz, Santa Cruz, CA 95064, USA Received 2018 September 24; revised 2018 December 18; accepted 2018 December 18; published 2019 February 4 Abstract We present evidence for a new two-planet system around the giant star HD 202696 (=HIP 105056, BD +26 4118). The discovery is based on public HIRES radial velocity (RV) measurements taken at Keck Observatory between +0.09 2007 July and 2014 September. We estimate a stellar mass of 1.91-0.14 M for HD 202696, which is located close to the base of the red giant branch. A two-planet self-consistent dynamical modeling MCMC scheme of the RV = +8.9 = +20.7 data followed by a long-term stability test suggests planetary orbital periods of Pb 517.8-3.9 and Pc 946.6-20.9 = +0.078 = +0.065 = +0.22 days, eccentricities of eb 0.011-0.011 and ec 0.028-0.012, and minimum dynamical masses of mb 2.00-0.10 = +0.18 fi and mc 1.86-0.23 MJup, respectively. -
15:1 Resonance Effects on the Orbital Motion of Artificial Satellites
doi: 10.5028/jatm.2011.03032011 Jorge Kennety S. Formiga* FATEC - College of Technology 15:1 Resonance effects on the São José dos Campos/SP – Brazil [email protected] orbital motion of artificial satellites Rodolpho Vilhena de Moraes Abstract: The motion of an artificial satellite is studied considering Federal University of São Paulo geopotential perturbations and resonances between the frequencies of the São José dos Campos/SP – Brazil mean orbital motion and the Earth rotational motion. The behavior of the [email protected] satellite motion is analyzed in the neighborhood of the resonances 15:1. A suitable sequence of canonical transformations reduces the system of differential equations describing the orbital motion to an integrable kernel. *author for correspondence The phase space of the resulting system is studied taking into account that one resonant angle is fixed. Simulations are presented showing the variations of the semi-major axis of artificial satellites due to the resonance effects. Keywords: Resonance, Artificial satellites, Celestial mechanics. INTRODUCTION some resonance’s region. In our study, it satellites in the neighbourhood of the 15:1 resonance (Fig. 1), or satellites The problem of resonance effects on orbital motion with an orbital period of about 1.6 hours will be considered. of satellites falls under a more categorical problem In our choice, the characteristic of the 356 satellites under in astrodynamics, which is known as the one of zero this condition can be seen in Table 1 (Formiga, 2005). divisors. The influence of resonances on the orbital and translational motion of artificial satellites has been extensively discussed in the literature under several aspects. -
Pdfs) for Each Orbital Parameter Used in and (3) in Cumming Et Al
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Caltech Authors The Astrophysical Journal, 709:396–410, 2010 January 20 doi:10.1088/0004-637X/709/1/396 C 2010. The American Astronomical Society. All rights reserved. Printed in the U.S.A. RETIRED A STARS AND THEIR COMPANIONS. III. COMPARING THE MASS–PERIOD DISTRIBUTIONS OF PLANETS AROUND A-TYPE STARS AND SUN-LIKE STARS∗ Brendan P. Bowler1, John Asher Johnson1,7, Geoffrey W. Marcy2, Gregory W. Henry3, Kathryn M. G. Peek2, Debra A. Fischer4, Kelsey I. Clubb4, Michael C. Liu1, Sabine Reffert5, Christian Schwab5, and Thomas B. Lowe6 1 Institute for Astronomy, University of Hawai‘i, 2680 Woodlawn Drive, Honolulu, HI 96822, USA; [email protected] 2 Department of Astronomy, University of California, MS 3411, Berkeley, CA 94720-3411, USA 3 Center of Excellence in Information Systems, Tennessee State University, 3500 John A. Merritt Blvd., Box 9501, Nashville, TN 37209, USA 4 Department of Physics and Astronomy, San Francisco State University, San Francisco, CA 94132, USA 5 ZAH-Landessternwarte, Konigstuhl¨ 12, 69117 Heidelberg, Germany 6 UCO/Lick Observatory, Santa Cruz, CA 95064, USA Received 2009 June 10; accepted 2009 December 3; published 2009 December 31 ABSTRACT We present an analysis of ∼5 years of Lick Observatory radial velocity measurements targeting a uniform sample of 31 intermediate-mass (IM) subgiants (1.5 M∗/M 2.0) with the goal of measuring the occurrence rate of Jovian planets around (evolved) A-type stars and comparing the distributions of their orbital and physical characteristics to those of planets around Sun-like stars. -
Orbital Resonances and Chaos in the Solar System
Solar system Formation and Evolution ASP Conference Series, Vol. 149, 1998 D. Lazzaro et al., eds. ORBITAL RESONANCES AND CHAOS IN THE SOLAR SYSTEM Renu Malhotra Lunar and Planetary Institute 3600 Bay Area Blvd, Houston, TX 77058, USA E-mail: [email protected] Abstract. Long term solar system dynamics is a tale of orbital resonance phe- nomena. Orbital resonances can be the source of both instability and long term stability. This lecture provides an overview, with simple models that elucidate our understanding of orbital resonance phenomena. 1. INTRODUCTION The phenomenon of resonance is a familiar one to everybody from childhood. A very young child is delighted in a playground swing when an older companion drives the swing at its natural frequency and rapidly increases the swing amplitude; the older child accomplishes the same on her own without outside assistance by driving the swing at a frequency twice that of its natural frequency. Resonance phenomena in the Solar system are essentially similar – the driving of a dynamical system by a periodic force at a frequency which is a rational multiple of the natural frequency. In fact, there are many mathematical similarities with the playground analogy, including the fact of nonlinearity of the oscillations, which plays a fundamental role in the long term evolution of orbits in the planetary system. But there is also an important difference: in the playground, the child adjusts her driving frequency to remain in tune – hence in resonance – with the natural frequency which changes with the amplitude of the swing. Such self-tuning is sometimes realized in the Solar system; but it is more often and more generally the case that resonances come-and-go. -
AMD-Stability and the Classification of Planetary Systems
A&A 605, A72 (2017) DOI: 10.1051/0004-6361/201630022 Astronomy c ESO 2017 Astrophysics& AMD-stability and the classification of planetary systems? J. Laskar and A. C. Petit ASD/IMCCE, CNRS-UMR 8028, Observatoire de Paris, PSL, UPMC, 77 Avenue Denfert-Rochereau, 75014 Paris, France e-mail: [email protected] Received 7 November 2016 / Accepted 23 January 2017 ABSTRACT We present here in full detail the evolution of the angular momentum deficit (AMD) during collisions as it was described in Laskar (2000, Phys. Rev. Lett., 84, 3240). Since then, the AMD has been revealed to be a key parameter for the understanding of the outcome of planetary formation models. We define here the AMD-stability criterion that can be easily verified on a newly discovered planetary system. We show how AMD-stability can be used to establish a classification of the multiplanet systems in order to exhibit the planetary systems that are long-term stable because they are AMD-stable, and those that are AMD-unstable which then require some additional dynamical studies to conclude on their stability. The AMD-stability classification is applied to the 131 multiplanet systems from The Extrasolar Planet Encyclopaedia database for which the orbital elements are sufficiently well known. Key words. chaos – celestial mechanics – planets and satellites: dynamical evolution and stability – planets and satellites: formation – planets and satellites: general 1. Introduction motion resonances (MMR, Wisdom 1980; Deck et al. 2013; Ramos et al. 2015) could justify the Hill-type criteria, but the The increasing number of planetary systems has made it nec- results on the overlap of the MMR island are valid only for close essary to search for a possible classification of these planetary orbits and for short-term stability. -
Arxiv:1603.07071V1
Dynamical Evidence for a Late Formation of Saturn’s Moons Matija Cuk´ Carl Sagan Center, SETI Institute, 189 North Bernardo Avenue, Mountain View, CA 94043 [email protected] Luke Dones Southwest Research Institute, Boulder, CO 80302 and David Nesvorn´y Southwest Research Institute, Boulder, CO 80302 Received ; accepted Revised and submitted to The Astrophysical Journal arXiv:1603.07071v1 [astro-ph.EP] 23 Mar 2016 –2– ABSTRACT We explore the past evolution of Saturn’s moons using direct numerical in- tegrations. We find that the past Tethys-Dione 3:2 orbital resonance predicted in standard models likely did not occur, implying that the system is less evolved than previously thought. On the other hand, the orbital inclinations of Tethys, Dione and Rhea suggest that the system did cross the Dione-Rhea 5:3 resonance, which is closely followed by a Tethys-Dione secular resonance. A clear implica- tion is that either the moons are significantly younger than the planet, or that their tidal evolution must be extremely slow (Q > 80, 000). As an extremely slow-evolving system is incompatible with intense tidal heating of Enceladus, we conclude that the moons interior to Titan are not primordial, and we present a plausible scenario for the system’s recent formation. We propose that the mid-sized moons re-accreted from a disk about 100 Myr ago, during which time Titan acquired its significant orbital eccentricity. We speculate that this disk has formed through orbital instability and massive collisions involving the previous generation of Saturn’s mid-sized moons. We identify the solar evection resonance perturbing a pair of mid-sized moons as the most likely trigger of such an insta- bility. -
Orbital Resonance and Solar Cycles by P.A.Semi
Orbital resonance and Solar cycles by P.A.Semi Abstract We show resonance cycles between most planets in Solar System, of differing quality. The most precise resonance - between Earth and Venus, which not only stabilizes orbits of both planets, locks planet Venus rotation in tidal locking, but also affects the Sun: This resonance group (E+V) also influences Sunspot cycles - the position of syzygy between Earth and Venus, when the barycenter of the resonance group most closely approaches the Sun and stops for some time, relative to Jupiter planet, well matches the Sunspot cycle of 11 years, not only for the last 400 years of measured Sunspot cycles, but also in 1000 years of historical record of "severe winters". We show, how cycles in angular momentum of Earth and Venus planets match with the Sunspot cycle and how the main cycle in angular momentum of the whole Solar system (854-year cycle of Jupiter/Saturn) matches with climatologic data, assumed to show connection with Solar output power and insolation. We show the possible connections between E+V events and Solar global p-Mode frequency changes. We futher show angular momentum tables and charts for individual planets, as encoded in DE405 and DE406 ephemerides. We show, that inner planets orbit on heliocentric trajectories whereas outer planets orbit on barycentric trajectories. We further TRY to show, how planet positions influence individual Sunspot groups, in SOHO and GONG data... [This work is pending...] Orbital resonance Earth and Venus The most precise orbital resonance is between Earth and Venus planets. These planets meet 5 times during 8 Earth years and during 13 Venus years. -
Martian Moon's Orbit Hints at an Ancient Ring of Mars
Martian Moon’s Orbit Hints at an Ancient Ring of Mars PRESS RELEASE DATE June 2, 2020 CONTACT Rebecca McDonald Director of Communications SETI Institute [email protected] +1 650-960-4526 Photo credit: https://solarsystem.nasa.gov/moons/mars-moons/deimos/in-depth/ June 2, 2020, Mountain View, CA – Scientists from the SETI Institute and Purdue University have found that the only way to produce Deimos’s unusually tilted orbit is for Mars to have had a ring billions of years ago. While some of the more massive planets in our solar system have giant rings and numerous big moons, Mars only has two small, misshapen moons, Phobos and Deimos. Although these moons are small, their peculiar orbits hide important secrets about their past. For a long time, scientists believed that Mars’s two moons, discovered in 1877, were captured asteroids. However, since their orbits are almost in the same plane as Mars’s equator, that the moons must have formed at the same time as Mars. But the orbit of the smaller, more distant moon Deimos is tilted by two degrees. “The fact that Deimos’s orbit is not exactly in plane with Mars’s equator was considered unimportant, and nobody cared to try to explain it,” says lead author Matija Ćuk, a research scientist at the SETI Institute. “But once we had a big new idea and we looked at it with new eyes, Deimos’s orbital tilt revealed its big secret.” This significant new idea was put forward in 2017 byĆ uk’s co-author David Minton, professor at Purdue University and his then-graduate student Andrew Hesselbrock. -
Destination Dwarf Planets: a Panel Discussion
Destination Dwarf Planets: A Panel Discussion OPAG, August 2019 Convened: Orkan Umurhan (SETI/NASA-ARC) Co-Panelists: Walt Harris (LPL, UA) Kathleen Mandt (JHUAPL) Alan Stern (SWRI) Dwarf Planets/KBO: a rogues gallery Triton Unifying Story for these bodies awaits Perihelio n/ Diamet Aphelion DocumentGoals 09.2018) from OPAG (Taken Name Surface characteristics Other observations/ hypotheses Moons er (km) /Current Distance (AU) Eris ~2326 P=38 Appears almost white, albedo of 0.96, higher Largest KBO by mass second Dysnomia A=98 than any other large Solar System body except by size. Models of internal C=96 Enceledus. Methane ice appears to be quite radioactive decay indicate evenly spread over the surface that a subsurface water ocean may be stable Haumea ~1600 P=35 Displays a white surface with an albedo of 0.6- Is a triaxial ellipsoid, with its Hi’iaka and A=51 0.8 , and a large, dark red area . Surface shows major axis twice as long as Namaka C=51 the presence of crystalline water ice (66%-80%) , the minor. Rapid rotation (~4 but no methane, and may have undergone hrs), high density, and high resurfacing in the last 10 Myr. Hydrogen cyanide, albedo may be the result of a phyllosilicate clays, and inorganic cyanide salts giant collision. Has the only may be present , but organics are no more than ring system known for a TNO. 8% 2007 OR10 ~1535 P=33 Amongst the reddest objects known, perhaps due May retain a thin methane S/(225088) A=101 to the abundant presence of methane frosts atmosphere 1 C=87 (tholins?) across the surface.Surface also show the presence of water ice.