(90377) SEDNA and (90482) ORCUS1 Chadwick A
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(50000) Quaoar, See Quaoar (90377) Sedna, See Sedna 1992 QB1 267
Index (50000) Quaoar, see Quaoar Apollo Mission Science Reports 114 (90377) Sedna, see Sedna Apollo samples 114, 115, 122, 1992 QB1 267, 268 ap-value, 3-hour, conversion from Kp 10 1996 TL66 268 arcade, post-eruptive 24–26 1998 WW31 274 Archimedian spiral 11 2000 CR105 269 Arecibo observatory 63 2000 OO67 277 Ariel, carbon dioxide ice 256–257 2003 EL61 270, 271, 273, 274, 275, 286, astrometric detection, of extrasolar planets – mass 273 190 – satellites 273 Atlas 230, 242, 244 – water ice 273 Bartels, Julius 4, 8 2003 UB313 269, 270, 271–272, 274, 286 – methane 271–272 Becquerel, Antoine Henry 3 – orbital parameters 271 Biermann, Ludwig 5 – satellite 272 biomass, from chemolithoautotrophs, on Earth 169 – spectroscopic studies 271 –, – on Mars 169 2005 FY 269, 270, 272–273, 286 9 bombardment, late heavy 68, 70, 71, 77, 78 – atmosphere 273 Borealis basin 68, 71, 72 – methane 272–273 ‘Brown Dwarf Desert’ 181, 188 – orbital parameters 272 brown dwarfs, deuterium-burning limit 181 51 Pegasi b 179, 185 – formation 181 Alfvén, Hannes 11 Callisto 197, 198, 199, 200, 204, 205, 206, ALH84001 (martian meteorite) 160 207, 211, 213 Amalthea 198, 199, 200, 204–205, 206, 207 – accretion 206, 207 – bright crater 199 – compared with Ganymede 204, 207 – density 205 – composition 204 – discovery by Barnard 205 – geology 213 – discovery of icy nature 200 – ice thickness 204 – evidence for icy composition 205 – internal structure 197, 198, 204 – internal structure 198 – multi-ringed impact basins 205, 211 – orbit 205 – partial differentiation 200, 204, 206, -
Colours of Minor Bodies in the Outer Solar System II - a Statistical Analysis, Revisited
Astronomy & Astrophysics manuscript no. MBOSS2 c ESO 2012 April 26, 2012 Colours of Minor Bodies in the Outer Solar System II - A Statistical Analysis, Revisited O. R. Hainaut1, H. Boehnhardt2, and S. Protopapa3 1 European Southern Observatory (ESO), Karl Schwarzschild Straße, 85 748 Garching bei M¨unchen, Germany e-mail: [email protected] 2 Max-Planck-Institut f¨ur Sonnensystemforschung, Max-Planck Straße 2, 37 191 Katlenburg- Lindau, Germany 3 Department of Astronomy, University of Maryland, College Park, MD 20 742-2421, USA Received —; accepted — ABSTRACT We present an update of the visible and near-infrared colour database of Minor Bodies in the outer Solar System (MBOSSes), now including over 2000 measurement epochs of 555 objects, extracted from 100 articles. The list is fairly complete as of December 2011. The database is now large enough that dataset with a high dispersion can be safely identified and rejected from the analysis. The method used is safe for individual outliers. Most of the rejected papers were from the early days of MBOSS photometry. The individual measurements were combined so not to include possible rotational artefacts. The spectral gradient over the visible range is derived from the colours, as well as the R absolute magnitude M(1, 1). The average colours, absolute magnitude, spectral gradient are listed for each object, as well as their physico-dynamical classes using a classification adapted from Gladman et al., 2008. Colour-colour diagrams, histograms and various other plots are presented to illustrate and in- vestigate class characteristics and trends with other parameters, whose significance are evaluated using standard statistical tests. -
On the Irrelevance of Being a PLUTO! Size Scale of Stars and Planets
On the irrelevance of being a PLUTO! Mayank Vahia DAA, TIFR Irrelevance of being Pluto 1 Size Scale of Stars and Planets Irrelevance of being Pluto 2 1 1 AU 700 Dsun Irrelevance of being Pluto 3 16 Dsun Irrelevance of being Pluto 4 2 Solar System 109 DEarth Irrelevance of being Pluto 5 11 DEarth Venus Irrelevance of being Pluto 6 3 Irrelevance of being Pluto 7 Solar System visible to unaided eye Irrelevance of being Pluto 8 4 Solar System at the beginning of 20 th Century Irrelevance of being Pluto 9 Solar System of my text book (30 years ago) Irrelevance of being Pluto 10 5 Asteroid Belt (Discovered in 1977) Irrelevance of being Pluto 11 The ‘Planet’ Pluto • Pluto is a 14 th magnitude object. • It is NOT visible to naked eye (neither are Uranus and Neptune). • It was discovered by American astronomer Clyde Tombaugh in 1930. Irrelevance of being Pluto 12 6 Prediction of Pluto • Percival Lowell and William H. Pickering are credited with the theoretical work on Pluto’s orbit done in 1909 based on data of Neptune’s orbital changes. • Venkatesh Ketakar had predicted it in May 1911 issue of Bulletin of the Astronomical Society of France. • He modelled his computations after those of Pierre-Simon Laplace who had analysed the motions of the satellites of Jupiter. • His location was within 1 o of its correct location. • He had predicted ts orbital period was 242.28 (248) years and a distance of 38.95 (39.53) A.U. • He had also predicted another planet at 59.573 A.U. -
Tnos Mueller
TNOs are Cool: A Survey of the Transneptunian Region Thomas M¨uller& The TNOs-are-Cool Team MPE Garching (37 members, 19 institutes, 9 countries) 1 Thomas M¨uller TNOs are Cool! • OT KP with 370 hours Overview • PACS and SPIRE photometric point-source observations • characterisation of about 140 Trans-Neptunian Objects (with known orbits) • target with a few mJy up to 400 mJy • Key element: highly reliable photometric ac- curacy in 3 (6) bands • time-critical observations with follow-on constraint (confusion noise) 2 Science Goals in a Nut Shell • Radiometric size and albedo solutions - accurate sizes (! volumes) of TNOs ! primordial (D> 200 km) size distribution - accurate spectroscopic and polarimetric modeling - albedo vs Size vs Colour vs Composition vs Orbit vs Binarity vs ... ! probe formation and evolution processes • Thermophysical properties (from 3 to 6 Pacs/Spire bands) - temperatures & thermal inertia ! ice vs rock surface, surface type - emissivity ! grain size information - beaming parameter ! surface roughness • Binary densities: mass from Ke- • Thermal lightcurves pler's 3rd law, volume from Herschel ! disentangle albedo/shape ! basic geophysical parameter ! spin-axis orientation ! interior structure/composition ! thermal inertia ! binary formation mechanism ! large surface structures 3 Thomas M¨uller TNOs are Cool! Herschel Study of the Kuiperbelt & TNOs: ! a benchmark for understanding the solar system debris disk, and extra-solar ones as well! M¨uller et al. 2009, Earth, Moon & Planet 105, 209-219 4 Thomas M¨uller TNOs -
Transneptunian Object Taxonomy 181
Fulchignoni et al.: Transneptunian Object Taxonomy 181 Transneptunian Object Taxonomy Marcello Fulchignoni LESIA, Observatoire de Paris Irina Belskaya Kharkiv National University Maria Antonietta Barucci LESIA, Observatoire de Paris Maria Cristina De Sanctis IASF-INAF, Rome Alain Doressoundiram LESIA, Observatoire de Paris A taxonomic scheme based on multivariate statistics is proposed to distinguish groups of TNOs having the same behavior concerning their BVRIJ colors. As in the case of asteroids, the broadband spectrophotometry provides a first hint about the bulk compositional properties of the TNOs’ surfaces. Principal components (PC) analysis shows that most of the TNOs’ color variability can be accounted for by a single component (i.e., a linear combination of the col- ors): All the studied objects are distributed along a quasicontinuous trend spanning from “gray” (neutral color with respect to those of the Sun) to very “red” (showing a spectacular increase in the reflectance of the I and J bands). A finer structure is superimposed to this trend and four homogeneous “compositional” classes emerge clearly, and independently from the PC analy- sis, if the TNO sample is analyzed with a grouping technique (the G-mode statistics). The first class (designed as BB) contains the objects that are neutral in color with respect to the Sun, while the RR class contains the very red ones. Two intermediate classes are separated by the G mode: the BR and the IR, which are clearly distinguished by the reflectance relative increases in the R and I bands. Some characteristics of the classes are deduced that extend to all the objects of a given class the properties that are common to those members of the class for which more detailed data are available (observed activity, full spectra, albedo). -
CFAS Astropicture of the Month
1 What object has the furthest known orbit in our Solar System? In terms of how close it will ever get to the Sun, the new answer is 2012 VP113, an object currently over twice the distance of Pluto from the Sun. Pictured above is a series of discovery images taken with the Dark Energy Camera attached to the NOAO's Blanco 4-meter Telescope in Chile in 2012 and released last week. The distant object, seen moving on the lower right, is thought to be a dwarf planet like Pluto. Previously, the furthest known dwarf planet was Sedna, discovered in 2003. Given how little of the sky was searched, it is likely that as many as 1,000 more objects like 2012 VP113 exist in the outer Solar System. 2012 VP113 is currently near its closest approach to the Sun, in about 2,000 years it will be over five times further. Some scientists hypothesize that the reason why objects like Sedna and 2012 VP113 have their present orbits is because they were gravitationally scattered there by a much larger object -- possibly a very distant undiscovered planet. Orbital Data: JDAphelion 449 ± 14 AU (Q) Perihelion 80.5 ± 0.6 AU (q) Semi-major axis 264 ± 8.3 AU (a) Eccentricity 0.696 ± 0.011 Orbital period4313 ± 204 yr 2 Discovery images taken on November 5, 2012. A merger of three discovery images, the red, green and blue dots on the image represent 2012 VP113's location on each of the images, taken two hours apart from each other. 2012 VP113, also written 2012 VP113, is the detached object in the Solar System with the largest known perihelion (closest approach to the Sun) -
Integral-Field Spectroscopy of (90482) Orcus-Vanth
Astronomy & Astrophysics manuscript no. main c ESO 2018 August 1, 2018 Integral-field spectroscopy of (90482) Orcus-Vanth⋆ Benoˆıt Carry1,2,3, Daniel Hestroffer4, Francesca E. DeMeo2,5, Audrey Thirouin6, J´erˆome Berthier4, Pedro Lacerda7, Bruno Sicardy2,8,9, Alain Doressoundiram2, Christophe Dumas10, David Farrelly11, and Thomas G. M¨uller12 1 European Space Astronomy Centre, ESA, P.O. Box 78, 28691 Villanueva de la Ca˜nada, Madrid, Spain e-mail: [email protected] 2 LESIA, Observatoire de Paris, CNRS, 5 place Jules Janssen, 92190 Meudon, France 3 Universit´eParis 7 Denis-Diderot, 5 rue Thomas Mann, 75205 Paris CEDEX, France 4 IMCCE, Observatoire de Paris, UPMC, CNRS, 77 av. Denfert Rochereau 75014 Paris, France 5 Department of Earth, Atmospheric, and Planetary Sciences, MIT, 77 Massachusetts Avenue, Cambridge, MA 02139, USA 6 Instituto de Astrof´ısica de Andaluc´ıa, CSIC, Apt 3004, 18080 Granada, Spain 7 Queen’s University, Belfast, County Antrim BT7 1NN, Ireland 8 Universit´ePierre et Marie Curie, 4, Place Jussieu, 75252 Paris cedex 5, France 9 Institut Universitaire de France, 103, Bld Saint Michel, 75005 Paris, France 10 Alonso de C´ordova 3107, Vitacura, Casilla 19001, Santiago de Chile, Chile 11 Utah State University, 0300 Old Main Hill, Logan, UT 84322, USA 12 Max-Planck-Institut f¨ur extraterrestrische Physik (MPE), Giessenbachstrasse, 85748 Garching, Germany Received ; accepted ABSTRACT Aims. We seek to constrain the surface composition of the Trans-Neptunian Object (90482) Orcus and its small satellite Vanth, as well as their mass and density. Methods. We acquired near-infrared spectra (1.4–2.4 µm) of (90482) Orcus and its companion Vanth using the adaptive-optics-fed integral-field spectrograph SINFONI mounted on Yepun/UT4 at the European Southern Observatory Very Large Telescope. -
Prerequisites for Explosive Cryovolcanism on Dwarf Planet-Class Kuiper Belt Objects ⇑ M
Icarus 246 (2015) 48–64 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Prerequisites for explosive cryovolcanism on dwarf planet-class Kuiper belt objects ⇑ M. Neveu a, , S.J. Desch a, E.L. Shock a,b, C.R. Glein c a School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287-1404, USA b Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ 85287-1404, USA c Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Rd. NW, Washington, DC 20015, USA article info abstract Article history: Explosive extrusion of cold material from the interior of icy bodies, or cryovolcanism, has been observed Received 30 December 2013 on Enceladus and, perhaps, Europa, Triton, and Ceres. It may explain the observed evidence for a young Revised 21 March 2014 surface on Charon (Pluto’s surface is masked by frosts). Here, we evaluate prerequisites for cryovolcanism Accepted 25 March 2014 on dwarf planet-class Kuiper belt objects (KBOs). We first review the likely spatial and temporal extent of Available online 5 April 2014 subsurface liquid, proposed mechanisms to overcome the negative buoyancy of liquid water in ice, and the volatile inventory of KBOs. We then present a new geochemical equilibrium model for volatile exso- Keywords: lution and its ability to drive upward crack propagation. This novel approach bridges geophysics and geo- Charon chemistry, and extends geochemical modeling to the seldom-explored realm of liquid water at subzero Interiors Pluto temperatures. We show that carbon monoxide (CO) is a key volatile for gas-driven fluid ascent; whereas Satellites, formation CO2 and sulfur gases only play a minor role. -
The Kuiper Belt: Launch Opportunities from 2025 to 2040
Return to the Kuiper Belt: launch opportunities from 2025 to 2040 Amanda M. Zangari,* Tiffany J. Finley† and S. Alan Stern‡ Southwest Research Institute 1050 Walnut St, Suite 300, Boulder, CO 80302, USA and Mark B. Tapley§ Southwest Research Institute P.O. Drawer 28510 San Antonio, Texas 78228-0510 Nomenclature AU = astronomical unit, average Earth - Sun distance B = impact parameter C3 = excess launch energy ∆V = change in velocity required to alter a spacecraft's trajectory KBO = Kuiper Belt Object PC = plane crossing rp = planet radius rq = distance from a planet at periapse � = gravitational constant * planet mass �! = arrival velocity of a spacecraft � = angle between incoming and outgoing velocity vectors during a swingby * Research Scientist, Space Science and Engineering, [email protected] † Principal Engineer, Space Science and Engineering, AIAA Member, [email protected] † Principal Engineer, Space Science and Engineering, AIAA Member, [email protected] ‡ Associate Vice President-R&D, Space Science and Engineering, AIAA Member, [email protected] § Institute Engineer, Space Science and Engineering, AIAA Senior Member, [email protected] Preliminary spacecraft trajectories for 45 Kuiper Belt Objects (KBOs) and Pluto suitable for launch between 2025 and 2040 are presented. These 46 objects comprise all objects with H magnitude < 4.0 or which have received a name from the International Astronomical Union as of May 2018. Using a custom Lambert solver, trajectories are modeled after the New Horizons mission to Pluto-Charon, which consisted of a fast launch with a Jupiter gravity assist. In addition to searching for Earth-Jupiter-KBO trajectories, Earth-Saturn-KBO trajectories are examined, with the option to add on a flyby to either Uranus or Neptune. -
The Surface of the Transneptunian Object 90482 Orcus
A&A 437, 1115–1120 (2005) Astronomy DOI: 10.1051/0004-6361:20042533 & c ESO 2005 Astrophysics The surface of the transneptunian object 90482 Orcus C. de Bergh1, A. Delsanti1,2,G.P.Tozzi3,E.Dotto4, A. Doressoundiram1, and M. A. Barucci1, 1 LESIA, Observatoire de Paris, 5 place Jules Janssen, 92195 Meudon, France e-mail: [email protected] 2 Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, Hawaii 96822, USA 3 INAF – Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5, 50125 Firenze, Italy 4 INAF – Osservatorio Astronomico di Roma, via Frascati 33, 00040 Monteporzio Catone (Roma), Italy Received 14 December 2004 / Accepted 11 March 2005 Abstract. In April 2004, we obtained visible and near-infrared spectroscopy and photometry of the Transneptunian Object (TNO) 90482 Orcus (2004 DW) with the European Southern Observatory (ESO) 8-m telescopes of the Very Large Telescope (VLT) in Chile. This object, discovered on February 17, 2004, is one of the largest known TNOs, and it belongs to the dynamical class of Plutinos. The high signal-to-noise ratio visible spectrum recorded on April 11, 2004, is nearly flat, in good agreement with the BVRI photometry we obtained the same night and with photometric measurements from Rabinowitz et al. (2004, IAU Circ., 8295). The near-infrared spectra (J, H,andK bands) were obtained on April 11, 12, and 21, 2004. Relatively strong absorptions attributed to water ice were detected around 1.5 and 2 µm. We compare these data with spectra of Orcus obtained at the 3.56-m Telescopio Nazionale Galileo (TNG) by Fornasier et al. -
Future Surveys of the Kuiper Belt 573
Trujillo: Future Surveys of the Kuiper Belt 573 Future Surveys of the Kuiper Belt Chadwick A. Trujillo Gemini North Observatory The next decade of Kuiper belt object (KBO) science will be completely dominated by the output of two surveys. These two surveys, the Panoramic Survey Telescope and Rapid Response System (Pan-STARRS) and the Large Synoptic Survey Telescope (LSST), will increase the total number of known KBOs by factors of 25 to 150 over the next decade. This discovery rate will not be uniform — it will come as a large flood of information during the first year of operation. If software development allows, additional depth may be gained in successive years if data can be combined across years to find bodies that are too faint to be detected in an individual visit. Not only will the surveys increase the number of objects dramatically, but they will also be sensitive to heliocentric distances far beyond 100 AU due to their multiyear survey methodology. In this work, we outline a basic timeline of operation of these two powerful surveys and the science that will be enabled by their data output, as well as other significant advances in KBO surveys expected in the next decade. 1. INTRODUCTION de Bergh et al., 2005; Cruikshank et al., 2005; Stern, 2005; Trujillo et al., 2005; Gaudi et al., 2005; Brown et al., 2005; The coming decade should see a dramatic increase in our Matese et al., 2005; Doressoundiram et al., 2005; Licandro knowledge of the Kuiper belt object (KBO) population due et al., 2006; Rabinowitz et al., 2006; Barkume et al., 2006; entirely to new telescopic survey experiments. -
Sedna: Confirmation and Compositional Constraints
A&A 466, 395–398 (2007) Astronomy DOI: 10.1051/0004-6361:20067021 & c ESO 2007 Astrophysics Ices on (90377) Sedna: confirmation and compositional constraints J. P. Emery1,2,C.M.DalleOre1,2,D.P.Cruikshank1, Y. R. Fernández3, D. E. Trilling4, and J. A. Stansberry4 1 NASA Ames Research Center, Mail Stop 245-6, Moffett Field, CA 94035, USA e-mail: [jemery;cdalleore]@mail.arc.nasa.gov, [email protected] 2 Carl Sagan Center, SETI Institute, 515 N Whisman Rd, Mountain View, CA 94043, USA 3 University of Central Florida, Department of Physics, 4000 Central Florida Blvd, M.A.P. Bulding, Orlando, FL 32816-2385, USA e-mail: [email protected] 4 University of Arizona, Steward Observatory, 933 N Cherry Ave., Tucson, AZ 85721, USA e-mail: [trilling; stansber]@as.arizona.edu Received 23 December 2006 / Accepted 25 January 2007 ABSTRACT We report measurements of reflectances of 90377 Sedna at λ>2.5 µm using the Infrared Array Camera (IRAC) on the Spitzer Space Telescope. Sedna orbits well beyond even the Kuiper Belt, with a perihelion distance of 76 AU, and is therefore very faint as viewed from Earth, despite its relatively large size. Previously published near-infrared spectra show possible signatures of CH4 and N2 at ∼2.3 and ∼2.15 µm, respectively. These and other ices also exhibit much stronger absorptions at λ>2.5 µm, providing the motivation for the present work. We detected flux from Sedna at 3.6 and 4.5 µm, but not at 5.8 or 8.0 µm.