Models of Distorted and Evolving Dark Matter Halos
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Aqueous Alteration on Main Belt Primitive Asteroids: Results from Visible Spectroscopy1
Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 1 LESIA, Observatoire de Paris, CNRS, UPMC Univ Paris 06, Univ. Paris Diderot, 5 Place J. Janssen, 92195 Meudon Pricipal Cedex, France 2 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris Cedex 13 3 Department of Physics and Astronomy of the University of Padova, Via Marzolo 8 35131 Padova, Italy Submitted to Icarus: November 2013, accepted on 28 January 2014 e-mail: [email protected]; fax: +33145077144; phone: +33145077746 Manuscript pages: 38; Figures: 13 ; Tables: 5 Running head: Aqueous alteration on primitive asteroids Send correspondence to: Sonia Fornasier LESIA-Observatoire de Paris arXiv:1402.0175v1 [astro-ph.EP] 2 Feb 2014 Batiment 17 5, Place Jules Janssen 92195 Meudon Cedex France e-mail: [email protected] 1Based on observations carried out at the European Southern Observatory (ESO), La Silla, Chile, ESO proposals 062.S-0173 and 064.S-0205 (PI M. Lazzarin) Preprint submitted to Elsevier September 27, 2018 fax: +33145077144 phone: +33145077746 2 Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 Abstract This work focuses on the study of the aqueous alteration process which acted in the main belt and produced hydrated minerals on the altered asteroids. Hydrated minerals have been found mainly on Mars surface, on main belt primitive asteroids and possibly also on few TNOs. These materials have been produced by hydration of pristine anhydrous silicates during the aqueous alteration process, that, to be active, needed the presence of liquid water under low temperature conditions (below 320 K) to chemically alter the minerals. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 41, NUMBER 4, A.D. 2014 OCTOBER-DECEMBER 203. LIGHTCURVE ANALYSIS FOR 4167 RIEMANN Amy Zhao, Ashok Aggarwal, and Caroline Odden Phillips Academy Observatory (I12) 180 Main Street Andover, MA 01810 USA [email protected] (Received: 10 June) Photometric observations of 4167 Riemann were made over six nights in 2014 April. A synodic period of P = 4.060 ± 0.001 hours was derived from the data. 4167 Riemann is a main-belt asteroid discovered in 1978 by L. V. Period analysis was carried out by the authors using MPO Canopus Zhuraveya. Observations of the asteroid were conducted at the and its Fourier analysis feature developed by Harris (Harris et al., Phillips Academy Observatory, which is equipped with a 0.4-m f/8 1989). The resulting lightcurve consists of 288 data points. The reflecting telescope by DFM Engineering. Images were taken with period spectrum strongly favors the bimodal solution. The an SBIG 1301-E CCD camera that has a 1280x1024 array of 16- resulting lightcurve has synodic period P = 4.060 ± 0.001 hours micron pixels. The resulting image scale was 1.0 arcsecond per and amplitude 0.17 mag. Dips in the period spectrum were also pixel. Exposures were 300 seconds and taken primarily at –35°C. noted at 8.1200 hours (2P) and at 6.0984 hours (3/2P). A search of All images were guided, unbinned, and unfiltered. Images were the Asteroid Lightcurve Database (Warner et al., 2009) and other dark and flat-field corrected with Maxim DL. -
The Planetary and Lunar Ephemeris DE 421
IPN Progress Report 42-178 • August 15, 2009 The Planetary and Lunar Ephemeris DE 421 William M. Folkner,* James G. Williams,† and Dale H. Boggs† The planetary and lunar ephemeris DE 421 represents updated estimates of the orbits of the Moon and planets. The lunar orbit is known to submeter accuracy through fitting lunar laser ranging data. The orbits of Venus, Earth, and Mars are known to subkilometer accu- racy. Because of perturbations of the orbit of Mars by asteroids, frequent updates are needed to maintain the current accuracy into the future decade. Mercury’s orbit is determined to an accuracy of several kilometers by radar ranging. The orbits of Jupiter and Saturn are determined to accuracies of tens of kilometers as a result of spacecraft tracking and modern ground-based astrometry. The orbits of Uranus, Neptune, and Pluto are not as well deter- mined. Reprocessing of historical observations is expected to lead to improvements in their orbits in the next several years. I. Introduction The planetary and lunar ephemeris DE 421 is a significant advance over earlier ephemeri- des. Compared with DE 418, released in July 2007,1 the DE 421 ephemeris includes addi- tional data, especially range and very long baseline interferometry (VLBI) measurements of Mars spacecraft; range measurements to the European Space Agency’s Venus Express space- craft; and use of current best estimates of planetary masses in the integration process. The lunar orbit is more robust due to an expanded set of lunar geophysical solution parameters, seven additional months of laser ranging data, and complete convergence. -
The British Astronomical Association Handbook 2014
THE HANDBOOK OF THE BRITISH ASTRONOMICAL ASSOCIATION 2015 2014 October ISSN 0068–130–X CONTENTS CALENDAR 2015 . 2 PREFACE . 3 HIGHLIGHTS FOR 2015 . 4 SKY DIARY . .. 5 VISIBILITY OF PLANETS . 6 RISING AND SETTING OF THE PLANETS IN LATITUDES 52°N AND 35°S . 7-8 ECLIPSES . 9-14 TIME . 15-16 EARTH AND SUN . 17-19 LUNAR LIBRATION . 20 MOON . 21 MOONRISE AND MOONSET . 21-25 SUN’S SELENOGRAPHIC COLONGITUDE . 26 LUNAR OCCULTATIONS . 27-33 GRAZING LUNAR OCCULTATIONS . 34-35 APPEARANCE OF PLANETS . 36 MERCURY . 37-38 VENUS . 39 MARS . 40-41 ASTEROIDS . 42 ASTEROID EPHEMERIDES . 43-47 ASTEROID OCCULTATIONS .. 48-50 NEO CLOSE APPROACHES TO EARTH . 51 ASTEROIDS: FAVOURABLE OBSERVING OPPORTUNITIES . 52-54 JUPITER . 55-59 SATELLITES OF JUPITER . 59-63 JUPITER ECLIPSES, OCCULTATIONS AND TRANSITS . 64-73 SATURN . 74-77 SATELLITES OF SATURN . 78-81 URANUS . 82 NEPTUNE . 83 TRANS–NEPTUNIAN & SCATTERED DISK OBJECTS . 84 DWARF PLANETS . 85-88 COMETS . 89-96 METEOR DIARY . 97-99 VARIABLE STARS (RZ Cassiopeiae; Algol; λ Tauri) . 100-101 MIRA STARS . 102 VARIABLE STAR OF THE YEAR (V Bootis) . 103-105 EPHEMERIDES OF DOUBLE STARS . 106-107 BRIGHT STARS . 108 ACTIVE GALAXIES . 109 PLANETS – EXPLANATION OF TABLES . 110 ELEMENTS OF PLANETARY ORBITS . 111 ASTRONOMICAL AND PHYSICAL CONSTANTS . 111-112 INTERNET RESOURCES . 113-114 GREEK ALPHABET . 115 ACKNOWLEDGEMENTS . 116 ERRATA . 116 Front Cover: The Moon at perigee and apogee – highlighting the clear size difference when the Moon is closest and farthest away from the Earth. Perigee on 2009/11/08 at 23:24UT, distance -
This Work Is Licensed Under the Creative Commons Attribution-Noncommercial-Share Alike 3.0 United States License
This work is licensed under the Creative Commons Attribution-Noncommercial-Share Alike 3.0 United States License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/us/ or send a letter to Creative Commons, 171 Second Street, Suite 300, San Francisco, California, 94105, USA. THE PREDACEOUS WATER BEETLES (COLEOPTERA: DYTISCIDAE) OF ALBERTA: SYSTEMATICS, NATURAL HISTORY AND DISTRIBUTION DA VID J. LARSON Department of Biology University of Calgary Quaestiones Entomologicae Calgary, Alberta 11: 245 - 498 1975 One hundred and forty five species belonging to 17 genera of the family Dytiscidae are recorded from Alberta. Adults of each species are described and keys for identification are presented. Six species are described as new: Hydroporus criniticoxis, Hydroporus carri, Hydroporus hockingi, Hydroporus rubyi, Agabus margareti and Acilius athabascae. The species Hygrotus picatus (Kirby) is recognized as valid, and the name Dytiscus alaskanus J. Balfour- Browne is revalidated. The following new synonymy is proposed: Hydroporus coloradensis Fall = H. griseostriatus (DeGeer); Hydroporus hortense Hatch = H. laevis Kirby; Hydroporus productotruncatus Hatch = H. alaskanus Fall; Rhantus aequalis Hatch = R. binotatus (Harris); Dytiscus ooligbukii Kirby = D. circumcinctus Ahrens; and Dytiscus vexatus Sharp = D. dauricus Gebler. For each species, the following information is presented: synonymy, selected literature ref erences, description, taxonomic notes, natural history notes, and distribution, which includes a brief outline of the species range and a map showing Alberta collection localities. Illustrations of taxonomically important characters are presented. The post-glacial distribution of the Alberta species is discussed and related to post-glacial vegetational movements and climatic change. The sources of most elements of the Alberta dytiscid fauna cannot be determined definitely but it is shown that the fauna is of diverse origin. -
The Planetary and Lunar Ephemerides DE430 and DE431
IPN Progress Report 42-196 • February 15, 2014 The Planetary and Lunar Ephemerides DE430 and DE431 William M. Folkner,* James G. Williams,† Dale H. Boggs,† Ryan S. Park,* and Petr Kuchynka* ABSTRACT. — The planetary and lunar ephemerides DE430 and DE431 are generated by fitting numerically integrated orbits of the Moon and planets to observations. The present-day lunar orbit is known to submeter accuracy through fitting lunar laser ranging data with an updated lunar gravity field from the Gravity Recovery and Interior Laboratory (GRAIL) mission. The orbits of the inner planets are known to subkilometer accuracy through fitting radio tracking measurements of spacecraft in orbit about them. Very long baseline interfer- ometry measurements of spacecraft at Mars allow the orientation of the ephemeris to be tied to the International Celestial Reference Frame with an accuracy of 0′′.0002. This orien- tation is the limiting error source for the orbits of the terrestrial planets, and corresponds to orbit uncertainties of a few hundred meters. The orbits of Jupiter and Saturn are determined to accuracies of tens of kilometers as a result of fitting spacecraft tracking data. The orbits of Uranus, Neptune, and Pluto are determined primarily from astrometric observations, for which measurement uncertainties due to the Earth’s atmosphere, combined with star catalog uncertainties, limit position accuracies to several thousand kilometers. DE430 and DE431 differ in their integrated time span and lunar dynamical modeling. The dynamical model for DE430 included a damping term between the Moon’s liquid core and solid man- tle that gives the best fit to lunar laser ranging data but that is not suitable for backward integration of more than a few centuries. -
Symposium on Telescope Science
Proceedings for the 23rd Annual Conference of the Society for Astronomical Sciences (Formerly the IAPPP-Western Wing) Symposium on Telescope Science Editors: Dale Mais David A. Kenyon Brian D. Warner May 26/27, 2004 Northwoods Resort, Big Bear Lake, CA 1 ©2004 Society for Astronomical Sciences, Inc. All Rights Reserved Published by the Society for Astronomical Sciences, Inc. First printed: May 2004 ISBN: 0-9714693-3-4 2 Table of Contents TABLE OF CONTENTS 3 PREFACE 5 CONFERENCE SPONSORS 6 SAS PARTNERS 7 Submitted Papers THE A.L.P.O. NEAR EARTH OBJECT PHOTOMETRY AND SHAPE MODELING PROGRAM 11 Richard A. Kowalski SURVEYS ARE YOUR FRIENDS 15 Arne A. Henden UNCOOL SCIENCE: PHOTOMETRY AND ASTROMETRY WITH MODIFIED WEB CAMERAS AND UNCOOLED IMAGERS 23 John E. Hoot DISPATCH SCHEDULING OF AUTOMATED TELESCOPES 35 Robert B. Denny THE STRATOSPHERIC OBSERVATORY FOR INFRARED ASTRONOMY (SOFIA) 51 Jürgen Wolf WWW.TRANSITSEARCH.ORG: A STATUS REPORT 63 Tim Castellano RADIAL VELOCITY DETECTION OF EXTRASOLAR PLANETS 65 Thomas G. Kaye MIRA VARIABLE STARS: SPECTROSCOPIC AND PHOTOMETRIC MONITORING OF THIS BROAD CLASS OF LONG TERM VARIABLE AND HIGHLY EVOLVED STARS-II 71 Dale E. Mais, Robert E. Stencel, and David Richards NASA’S HIGH ENERGY VISION: CHANDRA AND THE X-RAY UNIVERSE 81 Donna L. Young 3 MODERN ASTEROID OCCULTATION OBSERVING METHODS 85 Gene A. Lucas ASTEROIDAL OCCULTATION RESULTS 101 David W. Dunham, David Herald, Rohith Adavikolanu, and Steve Preston BLURRING THE LINE: NON-PROFESSIONALS AS OBSERVERS & DATA ANALYSTS 105 Aaron Price PRO-AM COLLABORATIONS: THE GLOBAL (NÉE GLAST) TELESCOPE NETWORK 109 Philip Plait, Gordon Spear, Tim Graves, and Lynn Cominsky DATA ACQUISITION AND REDUCTION METHODS FOR SLITLESS SPECTROSCOPY 113 John E. -
© in This Web Service Cambridge University Press
Cambridge University Press 978-0-521-89935-2 - Patrick Moore’s Data Book of Astronomy Edited by Patrick Moore and Robin Rees Index More information Index 3C-273 in Virgo 360 Anderson, J. D. and W. B. Hubbard model Aristarchus 526 47 Tucani cluster 349 of Jupiter 183 Aristotle, 127, 288 Planet X and movements of Uranus and Armstrong, Neil 34 Abbott, Charles 13 Neptune 251 Arp 148 362 Abell 370 cluster of galaxies 361 Anderson, L. 248 Arp, Halton 366 Absolute magnitude, conversion to luminosity Andromeda 373 Arrhenius, Svante 122, 272 (table) 304 M31 361 and meteor crater 285 Achondrites 281 spiral 3, 338 Ashen light 109 Acidalia 137 spiral 338 explanations: Gruithuisen, Herschel 109 Active Galactic Nulcei (AGN) 358 spiral galaxy, distance 357 modern theory 109–110 Active galaxies 358 Andromedid meteor shower 273 Asher, D. 277 Adams, J. C. 224 Anglo-Australian Observatory 512 Assyrians data collector 526 calculations of the outer planets 235 Anglo-Australian telescope 306 Asterisms 370 Adams, W. S. 110, 132, 319 Angstrom, A. 9 Summer Triangle 372 Adel, A. 226 Angstrom, Anders 291 Asteroid 1036 Ganymed 171 Adhara, epsilon Canis Major, brightest EUV source 521 Angstrom unit 10 Asteroid 1200 Phaethon 163 Adrastea 189 Annular eclipses, British, list of 22 Asteroid 1566 Icarus 169 Aegospotamos, Greece 416BC 280 Ant nebula 351 Asteroid 1620 Geographos 171 Aerogel 268 Antarctica 364 Asteroid 2001QE24 157 Aerolites 280 meteorites in 280 Asteroid 2008 TC3, collision with 169 Ahnighito meteorite 281 Antares 319 Asteroid 2060 Chiron 177 Airglow 291 Antennae galaxies 358 Asteroid 21 Lutetia 167 Airy, G. -
Download This Article in PDF Format
A&A 514, A96 (2010) Astronomy DOI: 10.1051/0004-6361/200913346 & c ESO 2010 Astrophysics A ring as a model of the main belt in planetary ephemerides P. Kuchynka1, J. Laskar1,A.Fienga1,2, and H. Manche1 1 Astronomie et Systèmes Dynamiques, IMCCE-CNRS UMR8028, Observatoire de Paris, UPMC, 77 avenue Denfert-Rochereau, 75014 Paris, France e-mail: [email protected] 2 Observatoire de Besançon-CNRS UMR6213, 41 bis avenue de l’Observatoire, 25000 Besançon, France Received 24 September 2009 / Accepted 4 February 2010 ABSTRACT Aims. We assess the ability of a solid ring to model a global perturbation induced by several thousands of main-belt asteroids. Methods. The ring is first studied in an analytical framework that provides an estimate of all the ring’s parameters excepting mass. In the second part, numerically estimated perturbations on the Earth-Mars, Earth-Venus, and Earth-Mercury distances induced by various subsets of the main-belt population are compared with perturbations induced by a ring. To account for large uncertainties in the asteroid masses, we obtain results from Monte Carlo experiments based on asteroid masses randomly generated according to available data and the statistical asteroid model. Results. The radius of the ring is analytically estimated at 2.8 AU. A systematic comparison of the ring with subsets of the main belt shows that, after removing the 300 most perturbing asteroids, the total main-belt perturbation of the Earth-Mars distance reaches on average 246 m on the 1969−2010 time interval. A ring with appropriate mass is able to reduce this effect to 38 m. -
Density of Asteroids
Density of asteroids B. Carry European Space Astronomy Centre, ESA, P.O. Box 78, 28691 Villanueva de la Ca˜nada,Madrid, Spain Abstract The small bodies of our solar system are the remnants of the early stages of planetary formation. A considerable amount of infor- mation regarding the processes that occurred during the accretion of the early planetesimals is still present among this population. A review of our current knowledge of the density of small bodies is presented here. Density is indeed a fundamental property for the understanding of their composition and internal structure. Intrinsic physical properties of small bodies are sought by searching for relationships between the dynamical and taxonomic classes, size, and density. Mass and volume estimates for 287 small bodies (asteroids, comets, and transneptunian objects) are collected from the literature. The accuracy and biases affecting the methods used to estimate these quantities are discussed and best-estimates are strictly selected. Bulk densities are subsequently computed and compared with meteorite density, allowing to estimate the macroporosity (i.e., amount of voids) within these bodies. Dwarf-planets apparently have no macroporosity, while smaller bodies (<400 km) can have large voids. This trend is apparently correlated with size: C and S-complex asteroids tends to have larger density with increasing diameter. The average density of each Bus-DeMeo taxonomic classes is computed (DeMeo et al., 2009, Icarus 202). S-complex asteroids are more dense on average than those in the C-complex that in turn have a larger macroporosity, although both complexes partly overlap. Within the C-complex asteroids, B-types stand out in albedo, reflectance spectra, and density, indicating a unique composition and structure. -
Patrick Moore's Data Book of Astronomy
Cambridge University Press 978-0-521-89935-2 - Patrick Moore’s Data Book of Astronomy Edited by Patrick Moore and Robin Rees Frontmatter More information Patrick Moore’s Data Book of Astronomy Packed with up-to-date astronomical data about the Solar System, our Galaxy and the wider universe, this is a one-stop reference for astronomers of all levels. It gives the names, positions, sizes and other key facts of all the planets and their satellites; discusses the Sun in depth, from sunspots to solar eclipses; lists the dates for cometary returns, close-approach asteroids, and significant meteor showers; and includes 88 star charts, with the names, positions, magnitudes and spectra of the stars, along with key data on nebulæ and clusters. Full of facts and figures, this is the only book you need to look up data about astronomy. It is destined to become the standard reference for everyone interested in astronomy. Patrick Moore CBE, FRS, is an astronomer and author. He has received numerous awards and prizes in recognition of his work, including the CBE in 1988 and knighthood in 2001 ‘for services to popularisation of science and to broadcasting’. A former Presi- dent of the British Astronomical Association, he is now honorary Life Vice President, and is the only amateur ever to have held an official post at the International Astronomical Union. Robin Rees, FRAS, is Director of Canopus Publishing and has produced a number of best-selling astronomy books, and under the Canopus Academic Publishing imprint he publishes academic physics titles. -
1 Jet Propulsion Laboratory Memorandum IOM 343R-08-003
Jet Propulsion Laboratory Memorandum IOM 343R-08-003 California Institute of Technology 31-March 2008 The Planetary and Lunar Ephemeris DE 421 W. M. Folkner, J. G. Williams, D. H. Boggs Abstract The planetary and lunar ephemeris DE 421 represents the ‘current best estimates’ of the orbits of the Moon and planets. The lunar orbit is currently known to sub-meter accuracy though fitting lunar laser ranging data. The orbits of Venus, Earth, and Mars areknown to sub-kilometer accuracy. Because of perturbation of the orbit of Mars by asteroids, frequent updates are needed to maintain the current accuracy into the future decade. Mercury’s orbit is determined to an accuracy of several kilometers by radar ranging. The orbits of Jupiter and Saturn are determined to accuracies of tens of kilometers as a result of spacecraft tracking and modern ground-based astrometry. The orbits of Uranus, Neptune, and Pluto are not as well determined. Reprocessing of historical observations is expected to lead to improvements in their orbits in the next several years. 1. Introduction The planetary and lunar ephemeris DE 421 is a significant advance over earlier ephemerides. Compared with DE 418, released in July 2007 (Folkner et al. 2007), the current ephemeris includes additional data, especially range and VLBI measurements of Mars spacecraft; range measurements to the ESA Venus Express spacecraft; and use of current best estimates of planetary masses in the integration process. The lunar orbit is more robust due to an expanded set of lunar geophysical solution parameters, seven additional months of laser ranging data, and complete convergence.