Transneptunian Binaries (2018)
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The Geology of the Rocky Bodies Inside Enceladus, Europa, Titan, and Ganymede
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2905.pdf THE GEOLOGY OF THE ROCKY BODIES INSIDE ENCELADUS, EUROPA, TITAN, AND GANYMEDE. Paul K. Byrne1, Paul V. Regensburger1, Christian Klimczak2, DelWayne R. Bohnenstiehl1, Steven A. Hauck, II3, Andrew J. Dombard4, and Douglas J. Hemingway5, 1Planetary Research Group, Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA ([email protected]), 2Department of Geology, University of Georgia, Athens, GA 30602, USA, 3Department of Earth, Environmental, and Planetary Sciences, Case Western Reserve University, Cleveland, OH 44106, USA, 4Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, IL 60607, USA, 5Department of Earth & Planetary Science, University of California Berkeley, Berkeley, CA 94720, USA. Introduction: The icy satellites of Jupiter and horizontal stresses, respectively, Pp is pore fluid Saturn have been the subjects of substantial geological pressure (found from (3)), and μ is the coefficient of study. Much of this work has focused on their outer friction [12]. Finally, because equations (4) and (5) shells [e.g., 1–3], because that is the part most readily assess failure in the brittle domain, we also considered amenable to analysis. Yet many of these satellites ductile deformation with the relation n –E/RT feature known or suspected subsurface oceans [e.g., 4– ε̇ = C1σ exp , (6) 6], likely situated atop rocky interiors [e.g., 7], and where ε̇ is strain rate, C1 is a constant, σ is deviatoric several are of considerable astrobiological significance. stress, n is the stress exponent, E is activation energy, R For example, chemical reactions at the rock–water is the universal gas constant, and T is temperature [13]. -
" Tnos Are Cool": a Survey of the Trans-Neptunian Region VI. Herschel
Astronomy & Astrophysics manuscript no. classicalTNOsManuscript c ESO 2012 April 4, 2012 “TNOs are Cool”: A survey of the trans-Neptunian region VI. Herschel⋆/PACS observations and thermal modeling of 19 classical Kuiper belt objects E. Vilenius1, C. Kiss2, M. Mommert3, T. M¨uller1, P. Santos-Sanz4, A. Pal2, J. Stansberry5, M. Mueller6,7, N. Peixinho8,9 S. Fornasier4,10, E. Lellouch4, A. Delsanti11, A. Thirouin12, J. L. Ortiz12, R. Duffard12, D. Perna13,14, N. Szalai2, S. Protopapa15, F. Henry4, D. Hestroffer16, M. Rengel17, E. Dotto13, and P. Hartogh17 1 Max-Planck-Institut f¨ur extraterrestrische Physik, Postfach 1312, Giessenbachstr., 85741 Garching, Germany e-mail: [email protected] 2 Konkoly Observatory of the Hungarian Academy of Sciences, 1525 Budapest, PO Box 67, Hungary 3 Deutsches Zentrum f¨ur Luft- und Raumfahrt e.V., Institute of Planetary Research, Rutherfordstr. 2, 12489 Berlin, Germany 4 LESIA-Observatoire de Paris, CNRS, UPMC Univ. Paris 06, Univ. Paris-Diderot, France 5 Stewart Observatory, The University of Arizona, Tucson AZ 85721, USA 6 SRON LEA / HIFI ICC, Postbus 800, 9700AV Groningen, Netherlands 7 UNS-CNRS-Observatoire de la Cˆote d’Azur, Laboratoire Cassiope´e, BP 4229, 06304 Nice Cedex 04, France 8 Center for Geophysics of the University of Coimbra, Av. Dr. Dias da Silva, 3000-134 Coimbra, Portugal 9 Astronomical Observatory of the University of Coimbra, Almas de Freire, 3040-04 Coimbra, Portugal 10 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris, France 11 Laboratoire d’Astrophysique de Marseille, CNRS & Universit´ede Provence, 38 rue Fr´ed´eric Joliot-Curie, 13388 Marseille Cedex 13, France 12 Instituto de Astrof´ısica de Andaluc´ıa (CSIC), Camino Bajo de Hu´etor 50, 18008 Granada, Spain 13 INAF – Osservatorio Astronomico di Roma, via di Frascati, 33, 00040 Monte Porzio Catone, Italy 14 INAF - Osservatorio Astronomico di Capodimonte, Salita Moiariello 16, 80131 Napoli, Italy 15 University of Maryland, College Park, MD 20742, USA 16 IMCCE, Observatoire de Paris, 77 av. -
Trans-Neptunian Objects a Brief History, Dynamical Structure, and Characteristics of Its Inhabitants
Trans-Neptunian Objects A Brief history, Dynamical Structure, and Characteristics of its Inhabitants John Stansberry Space Telescope Science Institute IAC Winter School 2016 IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 1 The Solar System beyond Neptune: History • 1930: Pluto discovered – Photographic survey for Planet X • Directed by Percival Lowell (Lowell Observatory, Flagstaff, Arizona) • Efforts from 1905 – 1929 were fruitless • discovered by Clyde Tombaugh, Feb. 1930 (33 cm refractor) – Survey continued into 1943 • Kuiper, or Edgeworth-Kuiper, Belt? – 1950’s: Pluto represented (K.E.), or had scattered (G.K.) a primordial, population of small bodies – thus KBOs or EKBOs – J. Fernandez (1980, MNRAS 192) did pretty clearly predict something similar to the trans-Neptunian belt of objects – Trans-Neptunian Objects (TNOs), trans-Neptunian region best? – See http://www2.ess.ucla.edu/~jewitt/kb/gerard.html IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 2 The Solar System beyond Neptune: History • 1978: Pluto’s moon, Charon, discovered – Photographic astrometry survey • 61” (155 cm) reflector • James Christy (Naval Observatory, Flagstaff) – Technologically, discovery was possible decades earlier • Saturation of Pluto images masked the presence of Charon • 1988: Discovery of Pluto’s atmosphere – Stellar occultation • Kuiper airborne observatory (KAO: 90 cm) + 7 sites • Measured atmospheric refractivity vs. height • Spectroscopy suggested N2 would dominate P(z), T(z) • 1992: Pluto’s orbit explained • Outward migration by Neptune results in capture into 3:2 resonance • Pluto’s inclination implies Neptune migrated outward ~5 AU IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 3 The Solar System beyond Neptune: History • 1992: Discovery of 2nd TNO • 1976 – 92: Multiple dedicated surveys for small (mV > 20) TNOs • Fall 1992: Jewitt and Luu discover 1992 QB1 – Orbit confirmed as ~circular, trans-Neptunian in 1993 • 1993 – 4: 5 more TNOs discovered • c. -
Arxiv:2102.05076V2 [Astro-Ph.EP] 17 Feb 2021 Et Al
Draft version August 30, 2021 Typeset using LATEX twocolumn style in AASTeX63 The Reflectance of Cold Classical Trans-Neptunian Objects in the Nearest Infrared Tom Seccull,1, 2 Wesley C. Fraser,3 and Thomas H. Puzia4 1Gemini Observatory/NSF's NOIRLab, 670 N. A'ohoku Place, Hilo, HI 96720, USA 2Astrophysics Research Centre, Queen's University Belfast, University Road, Belfast, BT7 1NN, UK 3Herzberg Institute of Astrophysics, 5071 West Saanich Road, Victoria, BC V9E 2E7, Canada 4Institute of Astrophysics, Pontificia Universidad Cat´olica de Chile, Av. Vicu~naMacKenna 4860, 7820436, Santiago, Chile (Received 2020 Nov 8; Revised 2021 Jan 22; Accepted 2021 Feb 6) Submitted to PSJ ABSTRACT Recent photometric surveys of Trans-Neptunian Objects (TNOs) have revealed that the cold classical TNOs have distinct z-band color characteristics, and occupy their own distinct surface class. This suggested the presence of an absorption band in the reflectance spectra of cold classicals at λ > 0:8 µm. Here we present reflectance spectra spanning 0:55 − 1:0 µm for six TNOs occupying dynamically cold orbits at a ∼ 44 au. Five of our spectra show a clear and broadly consistent reduction in spectral gradient above 0:8 µm that diverges from their linear red optical continuum and agrees with their reported photometric colour data. Despite predictions, we find no evidence that the spectral flattening is caused by an absorption band centered near 1:0 µm. We predict that the overall consistent shape of these five spectra is related to the presence of similar refractory organics on each of their surfaces, and/or their similar physical surface properties such as porosity or grain size distribution. -
With JWST: Science Justification and Observational Requirements
Observing Outer Planet Satellites (except Titan) with JWST: Science Justification and Observational Requirements Laszlo Keszthelyi1, Will Grundy2, John Stansberry3, Anand Sivaramakrishnan3, Deepashri Thatte3, Murthy Gudipati4, Constantine Tsang5, Alexandra Greenbaum6, Chima McGruder7 1U.S. Geological Survey, Astrogeology Science Center, 2255 N. Gemini Dr., Flagstaff, AZ 86001. ([email protected]) 2Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff, AZ 86001. ([email protected]) 3Space Telescope Science Institute, 3700 San Martin Dr., Baltimore, MD 21218. ([email protected]; [email protected]; [email protected]) 4California Institute of Technology, Jet Propulsion Laboratory, 4800 Oak Grove Dr., Pasadena, CA 91109. ([email protected]) 5Southwest Research Institute, Department of Space Studies, 1050 Walnut St., Suite 300, Boulder, CO 80302. ([email protected]) 6 Department of Physics and Astronomy, 3400 N. Charles Street, Baltimore, MD 21218. ([email protected]) 7Department of Physics & Astronomy, 1408 Circle Drive, Knoxville, TN 37996. ([email protected]) ABSTRACT The James Webb Space Telescope (JWST) will allow observations with a unique combination of spectral, spatial, and temporal resolution for the study of outer planet satellites within our Solar System. We highlight the infrared spectroscopy of icy moons and temporal changes on geologically active satellites as two particularly valuable avenues of scientific inquiry. While some care must be taken to avoid saturation issues, JWST has observation modes that should provide excellent infrared data for such studies. KEYWORDS Solar System Astronomical Techniques 1. Introduction Starting in 2018, the James Webb Space Telescope (JWST) is expected to provide a groundbreaking new tool for astronomical observations, including planetary satellites as close as Phobos and Deimos. -
Markov Chain Monte-Carlo Orbit Computation for Binary Asteroids
SF2A 2013 L. Cambr´esy,F. Martins, E. Nuss and A. Palacios (eds) MARKOV CHAIN MONTE-CARLO ORBIT COMPUTATION FOR BINARY ASTEROIDS Dagmara Oszkiewicz2; 1, Daniel Hestroffer2 and Pedro David2 Abstract. We present a novel method of orbit computation for resolved binary asteroids. The method combines the Thiele, Innes, van den Bos method with a Markov chain Monte Carlo technique (MCMC). The classical Thiele-van den Bos method has been commonly used in multiple applications before, including orbits of binary stars and asteroids; conversely this novel method can be used for the analysis of binary stars, and of other gravitationally bound binaries. The method requires a minimum of three observations (observing times and relative positions - Cartesian or polar) made at the same tangent plane - or close enough for enabling a first approximation. Further, the use of the MCMC technique for statistical inversion yields the whole bundle of possible orbits, including the one that is most probable. In this new method, we make use of the Metropolis-Hastings algorithm to sample the parameters of the Thiele-van den Bos method, that is the orbital period (or equivalently the double areal constant) together with three randomly selected observations from the same tangent plane. The observations are sampled within their observational errors (with an assumed distribution) and the orbital period is the only parameter that has to be tuned during the sampling procedure. We run multiple chains to ensure that the parameter phase space is well sampled and that the solutions have converged. After the sampling is completed we perform convergence diagnostics. The main advantage of the novel approach is that the orbital period does not need to be known in advance and the entire region of possible orbital solutions is sampled resulting in a maximum likelihood solution and the confidence regions. -
CHORUS: Let's Go Meet the Dwarf Planets There Are Five in Our Solar
Meet the Dwarf Planet Lyrics: CHORUS: Let’s go meet the dwarf planets There are five in our solar system Let’s go meet the dwarf planets Now I’ll go ahead and list them I’ll name them again in case you missed one There’s Pluto, Ceres, Eris, Makemake and Haumea They haven’t broken free from all the space debris There’s Pluto, Ceres, Eris, Makemake and Haumea They’re smaller than Earth’s moon and they like to roam free I’m the famous Pluto – as many of you know My orbit’s on a different path in the shape of an oval I used to be planet number 9, But I break the rules; I’m one of a kind I take my time orbiting the sun It’s a long, long trip, but I’m having fun! Five moons keep me company On our epic journey Charon’s the biggest, and then there’s Nix Kerberos, Hydra and the last one’s Styx 248 years we travel out Beyond the other planet’s regular rout We hang out in the Kuiper Belt Where the ice debris will never melt CHORUS My name is Ceres, and I’m closest to the sun They found me in the Asteroid Belt in 1801 I’m the only known dwarf planet between Jupiter and Mars They thought I was an asteroid, but I’m too round and large! I’m Eris the biggest dwarf planet, and the slowest one… It takes me 557 years to travel around the sun I have one moon, Dysnomia, to orbit along with me We go way out past the Kuiper Belt, there’s so much more to see! CHORUS My name is Makemake, and everyone thought I was alone But my tiny moon, MK2, has been with me all along It takes 310 years for us to orbit ‘round the sun But out here in the Kuiper Belt… our adventures just begun Hello my name’s Haumea, I’m not round shaped like my friends I rotate fast, every 4 hours, which stretched out both my ends! Namaka and Hi’iaka are my moons, I have just 2 And we live way out past Neptune in the Kuiper Belt it’s true! CHORUS Now you’ve met the dwarf planets, there are 5 of them it’s true But the Solar System is a great big place, with more exploring left to do Keep watching the skies above us with a telescope you look through Because the next person to discover one… could be me or you… . -
Comparative Planetology Beyond Neptune Enabled by a Near-Term Interstellar Probe
51st Lunar and Planetary Science Conference (2020) 1464.pdf COMPARATIVE PLANETOLOGY BEYOND NEPTUNE ENABLED BY A NEAR-TERM INTERSTELLAR PROBE. K. D. Runyon ([email protected]), K. E. Mandt, P. Brandt, M. Paul, C. Lisse, R. McNutt, Jr. (Johns Hopkins APL, 11101 Johns Hopkins Rd., Laurel, MD, 20723, USA), C.B. Beddingfield (NASA/Ames), S.A. Stern (Southwest Research Institute) Summary: A properly instrumented Interstellar surprising differences despite water having played a Probe could enable flyby geoscience investigations of a substantial role in the surface and subsurface of each Kuiper belt dwarf planet, advancing comparative plan- planet (e.g., Prettyman et al., 2017; Prockter et al., 2005; etology in the trans-Neptunian region. Nimmo and Pappalardo, 2016; Beyer et al., 2019). With Introduction: Comparative planetology among the long time frames and relative difficulty in reaching KBO dwarf planets A) should be a priority for future trans-Neptunian planets, Interstellar Probe could ad- NASA missions; and B) could be partly addressed by a vance the field via in situ exploration of just one more targeted flyby of a dwarf planet by an interstellar probe planet, such as Quaoar, “Gonggong” (officially 2007 leaving the Solar System, such as described by McNutt OR10), or another. et al. (2019). This abstract is based on a near-term white A camera-instrumented Interstellar Probe could tar- paper to be submitted by mid-2020 to the National get high resolution images of a dwarf planet’s surface, Academies Planetary Science Decadal Survey Panel. similar to New Horizons’ flyby images of Pluto, Charon, Please contact the first author to be added to the white and Arrokoth (2014 MU69). -
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Five New and Three Improved Mutual Orbits of Transneptunian Binaries W.M. Grundya, K.S. Nollb, F. Nimmoc, H.G. Roea, M.W. Buied, S.B. Portera, S.D. Benecchie,f, D.C. Stephensg, H.F. Levisond, and J.A. Stansberryh a. Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff AZ 86001. b. Space Telescope Science Institute, 3700 San Martin Dr., Baltimore MD 21218. c. Department of Earth and Planetary Sciences, University of California, Santa Cruz CA 95064. d. Southwest Research Institute, 1050 Walnut St. #300, Boulder CO 80302. e. Planetary Science Institute, 1700 E. Fort Lowell, Suite 106, Tucson AZ 85719. f. Carnegie Institution of Washington, Department of Terrestrial Magnetism, 5241 Broad Branch Rd. NW, Washington DC 20015. g. Dept. of Physics and Astronomy, Brigham Young University, N283 ESC Provo UT 84602. h. Steward Observatory, University of Arizona, 933 N. Cherry Ave., Tucson AZ 85721. — Published in 2011: Icarus 213, 678-692. — doi:10.1016/j.icarus.2011.03.012 ABSTRACT We present three improved and five new mutual orbits of transneptunian binary systems (58534) Logos-Zoe, (66652) Borasisi-Pabu, (88611) Teharonhiawako-Sawiskera, (123509) 2000 WK183, (149780) Altjira, 2001 QY297, 2003 QW111, and 2003 QY90 based on Hubble Space Tele- scope and Keck II laser guide star adaptive optics observations. Combining the five new orbit solutions with 17 previously known orbits yields a sample of 22 mutual orbits for which the period P, semimajor axis a, and eccentricity e have been determined. These orbits have mutual periods ranging from 5 to over 800 days, semimajor axes ranging from 1,600 to 37,000 km, ec- centricities ranging from 0 to 0.8, and system masses ranging from 2 × 1017 to 2 × 1022 kg. -
Mass of the Kuiper Belt · 9Th Planet PACS 95.10.Ce · 96.12.De · 96.12.Fe · 96.20.-N · 96.30.-T
Celestial Mechanics and Dynamical Astronomy manuscript No. (will be inserted by the editor) Mass of the Kuiper Belt E. V. Pitjeva · N. P. Pitjev Received: 13 December 2017 / Accepted: 24 August 2018 The final publication ia available at Springer via http://doi.org/10.1007/s10569-018-9853-5 Abstract The Kuiper belt includes tens of thousands of large bodies and millions of smaller objects. The main part of the belt objects is located in the annular zone between 39.4 au and 47.8 au from the Sun, the boundaries correspond to the average distances for orbital resonances 3:2 and 2:1 with the motion of Neptune. One-dimensional, two-dimensional, and discrete rings to model the total gravitational attraction of numerous belt objects are consid- ered. The discrete rotating model most correctly reflects the real interaction of bodies in the Solar system. The masses of the model rings were determined within EPM2017—the new version of ephemerides of planets and the Moon at IAA RAS—by fitting spacecraft ranging observations. The total mass of the Kuiper belt was calculated as the sum of the masses of the 31 largest trans-neptunian objects directly included in the simultaneous integration and the estimated mass of the model of the discrete ring of TNO. The total mass −2 is (1.97 ± 0.30) · 10 m⊕. The gravitational influence of the Kuiper belt on Jupiter, Saturn, Uranus and Neptune exceeds at times the attraction of the hypothetical 9th planet with a mass of ∼ 10 m⊕ at the distances assumed for it. -
Thermal Measurements
Physical characterization of Kuiper belt objects from stellar occultations and thermal measurements Pablo Santos-Sanz & the SBNAF team [email protected] Stellar occultations Simple method to: -Obtain high precision sizes/shapes (unc. ~km) -Detect/characterize atmospheres/rings… -Obtain albedo, density… -Improve the orbit of the body …this looks like very nice but...the reality is harder (at least for TNOs and Centaurs) EPSC2017, Riga, Latvia, 20 Sep. 2017 Stellar occultations Titan 10 mas Quaoar 0.033 arsec Diameter of 1 Euro (33 mas) Pluto coin at 140 km Eris Charon Makemake Pablo Santos-Sanz EPSC2017, Riga, Latvia, 20 Sep. 2017 Stellar occultations ~25 occultations by 15 TNOs (+ Pluto/Charon + Chariklo + Chiron + 2002 GZ32) Namaka Dysnomia Ixion Hi’iaka Pluto Haumea Eris Chiron 2007 UK126 Chariklo Vanth 2014 MU69 2002 GZ32 2003 VS2 2002 KX14 2002 TX300 2003 AZ84 2005 TV189 Stellar occultations: Eris & Chariklo Eris: 6 November 2010 Chariklo: 3 June 2014 • Size ~ Plutón • It has rings! • Albedo= 96% 3 • Density= 2.5 g/cm Danish 1.54-m telescope (La Silla) • Atmosphere < 1nbar (10-4 x Pluto) Eris’ radius Pluto’s radius 1163±6 km 1188.3±1.6 km (Nimmo et al. 2016) Braga-Ribas et al. 2014 (Nature) Sicardy et al. 2011 (Nature) EPSC2017, Riga, Latvia, 20 Sep. 2017 Stellar occultations: Makemake 23 April 2011 Geometric Albedo = 77% (betwen Pluto and Eris) Possible local atmosphere! Ortiz et al. 2012 (Nature) EPSC2017, Riga, Latvia, 20 Sep. 2017 Stellar occultations: latest “catches” 2007 UK : 15 November 2014 2003 AZ84: 8 Jan. 2011 single, 3 Feb. 126 2012 multi, 2 Dec. -
" Tnos Are Cool": a Survey of the Transneptunian Region IV. Size
Astronomy & Astrophysics manuscript no. SDOs˙Herschel˙Santos-Sanz˙2012 c ESO 2012 February 8, 2012 “TNOs are Cool”: A Survey of the Transneptunian Region IV Size/albedo characterization of 15 scattered disk and detached objects observed with Herschel Space Observatory-PACS? P. Santos-Sanz1, E. Lellouch1, S. Fornasier1;2, C. Kiss3, A. Pal3, T.G. Muller¨ 4, E. Vilenius4, J. Stansberry5, M. Mommert6, A. Delsanti1;7, M. Mueller8;9, N. Peixinho10;11, F. Henry1, J.L. Ortiz12, A. Thirouin12, S. Protopapa13, R. Duffard12, N. Szalai3, T. Lim14, C. Ejeta15, P. Hartogh15, A.W. Harris6, and M. Rengel15 1 LESIA-Observatoire de Paris, CNRS, UPMC Univ. Paris 6, Univ. Paris-Diderot, 5 Place J. Janssen, 92195 Meudon Cedex, France. e-mail: [email protected] 2 Univ. Paris Diderot, Sorbonne Paris Cite,´ 4 rue Elsa Morante, 75205 Paris, France. 3 Konkoly Observatory of the Hungarian Academy of Sciences, Budapest, Hungary. 4 Max–Planck–Institut fur¨ extraterrestrische Physik (MPE), Garching, Germany. 5 University of Arizona, Tucson, USA. 6 Deutsches Zentrum fur¨ Luft- und Raumfahrt (DLR), Institute of Planetary Research, Berlin, Germany. 7 Laboratoire d’Astrophysique de Marseille, CNRS & Universite´ de Provence, Marseille. 8 SRON LEA / HIFI ICC, Postbus 800, 9700AV Groningen, Netherlands. 9 UNS-CNRS-Observatoire de la Coteˆ d0Azur, Laboratoire Cassiopee,´ BP 4229, 06304 Nice Cedex 04, France. 10 Center for Geophysics of the University of Coimbra, Av. Dr. Dias da Silva, 3000-134 Coimbra, Portugal 11 Astronomical Observatory, University of Coimbra, Almas de Freire, 3040-004 Coimbra, Portugal 12 Instituto de Astrof´ısica de Andaluc´ıa (CSIC), Granada, Spain. 13 University of Maryland, USA.