ASTRONOMICAL SOCIETY of the PACIFIC 233 V. COMET OTERMA 1943 A: a MINOR PLANET?
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CAPTURE of TRANS-NEPTUNIAN PLANETESIMALS in the MAIN ASTEROID BELT David Vokrouhlický1, William F
The Astronomical Journal, 152:39 (20pp), 2016 August doi:10.3847/0004-6256/152/2/39 © 2016. The American Astronomical Society. All rights reserved. CAPTURE OF TRANS-NEPTUNIAN PLANETESIMALS IN THE MAIN ASTEROID BELT David Vokrouhlický1, William F. Bottke2, and David Nesvorný2 1 Institute of Astronomy, Charles University, V Holešovičkách 2, CZ–18000 Prague 8, Czech Republic; [email protected] 2 Department of Space Studies, Southwest Research Institute, 1050 Walnut Street, Suite 300, Boulder, CO 80302; [email protected], [email protected] Received 2016 February 9; accepted 2016 April 21; published 2016 July 26 ABSTRACT The orbital evolution of the giant planets after nebular gas was eliminated from the Solar System but before the planets reached their final configuration was driven by interactions with a vast sea of leftover planetesimals. Several variants of planetary migration with this kind of system architecture have been proposed. Here, we focus on a highly successful case, which assumes that there were once five planets in the outer Solar System in a stable configuration: Jupiter, Saturn, Uranus, Neptune, and a Neptune-like body. Beyond these planets existed a primordial disk containing thousands of Pluto-sized bodies, ∼50 million D > 100 km bodies, and a multitude of smaller bodies. This system eventually went through a dynamical instability that scattered the planetesimals and allowed the planets to encounter one another. The extra Neptune-like body was ejected via a Jupiter encounter, but not before it helped to populate stable niches with disk planetesimals across the Solar System. Here, we investigate how interactions between the fifth giant planet, Jupiter, and disk planetesimals helped to capture disk planetesimals into both the asteroid belt and first-order mean-motion resonances with Jupiter. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 36, NUMBER 3, A.D. 2009 JULY-SEPTEMBER 77. PHOTOMETRIC MEASUREMENTS OF 343 OSTARA Our data can be obtained from http://www.uwec.edu/physics/ AND OTHER ASTEROIDS AT HOBBS OBSERVATORY asteroid/. Lyle Ford, George Stecher, Kayla Lorenzen, and Cole Cook Acknowledgements Department of Physics and Astronomy University of Wisconsin-Eau Claire We thank the Theodore Dunham Fund for Astrophysics, the Eau Claire, WI 54702-4004 National Science Foundation (award number 0519006), the [email protected] University of Wisconsin-Eau Claire Office of Research and Sponsored Programs, and the University of Wisconsin-Eau Claire (Received: 2009 Feb 11) Blugold Fellow and McNair programs for financial support. References We observed 343 Ostara on 2008 October 4 and obtained R and V standard magnitudes. The period was Binzel, R.P. (1987). “A Photoelectric Survey of 130 Asteroids”, found to be significantly greater than the previously Icarus 72, 135-208. reported value of 6.42 hours. Measurements of 2660 Wasserman and (17010) 1999 CQ72 made on 2008 Stecher, G.J., Ford, L.A., and Elbert, J.D. (1999). “Equipping a March 25 are also reported. 0.6 Meter Alt-Azimuth Telescope for Photometry”, IAPPP Comm, 76, 68-74. We made R band and V band photometric measurements of 343 Warner, B.D. (2006). A Practical Guide to Lightcurve Photometry Ostara on 2008 October 4 using the 0.6 m “Air Force” Telescope and Analysis. Springer, New York, NY. located at Hobbs Observatory (MPC code 750) near Fall Creek, Wisconsin. -
Assa Handbook-1993
ASTRONOMICAL HANDBOOK FOR SOUTHERN AFRICA 1 published by the Astronomical Society of Southern Africa 5 A MUSEUM QUEEN VICTORIA STREET (3 61 CAPE TOWN 8000 (021)243330 o PUBLIC SHOWS o MONTHLY SKY UPDATES 0 ASTRONOMY COURSES O MUSIC CONCERTS o ASTRONOMY WEEK 0 SCHOOL SHOWS ° CLUB BOOKINGS ° CORPORATE LAUNCH VENUE FOR MORE INFO PHONE 243330 ASTRONOMICAL HANDBOOK FOR SOUTHERN AFRICA 1993 This booklet is intended both as an introduction to observational astronomy for the interested layman - even if hie interest is only a passing one - and as a handbook for the established amateur or professional astronomer. Front cover The telescope of Ds G. de Beer (right) of the Ladismith Astronomical Society. He, Dr M. Schreuder (left) and the late Mr Ron Dale of the Natal Midlands Centre, are viewing Siriu3 in the daytime with the aid of setting circles. Photograph Mr J. Watson ® t h e Astronomical Society of Southern Africa, Cape Town. 1992 ISSN 0571-7191 CONTENTS ASTRONOMY IN SOUTHERN AFRICA...................... 1 DIARY................................................................. 6 THE SUN............................................................... 8 THE MOON............................................................. 11 THE PLANETS.......................................................... 17 THE MOONS OF JUPITER ................................................ 24 THE MOONS OF SATURN....................................... 28 COMETS AND METEORS............................ 29 THE STARS........................................................... -
Observations from Orbiting Platforms 219
Dotto et al.: Observations from Orbiting Platforms 219 Observations from Orbiting Platforms E. Dotto Istituto Nazionale di Astrofisica Osservatorio Astronomico di Torino M. A. Barucci Observatoire de Paris T. G. Müller Max-Planck-Institut für Extraterrestrische Physik and ISO Data Centre A. D. Storrs Towson University P. Tanga Istituto Nazionale di Astrofisica Osservatorio Astronomico di Torino and Observatoire de Nice Orbiting platforms provide the opportunity to observe asteroids without limitation by Earth’s atmosphere. Several Earth-orbiting observatories have been successfully operated in the last decade, obtaining unique results on asteroid physical properties. These include the high-resolu- tion mapping of the surface of 4 Vesta and the first spectra of asteroids in the far-infrared wave- length range. In the near future other space platforms and orbiting observatories are planned. Some of them are particularly promising for asteroid science and should considerably improve our knowledge of the dynamical and physical properties of asteroids. 1. INTRODUCTION 1800 asteroids. The results have been widely presented and discussed in the IRAS Minor Planet Survey (Tedesco et al., In the last few decades the use of space platforms has 1992) and the Supplemental IRAS Minor Planet Survey opened up new frontiers in the study of physical properties (Tedesco et al., 2002). This survey has been very important of asteroids by overcoming the limits imposed by Earth’s in the new assessment of the asteroid population: The aster- atmosphere and taking advantage of the use of new tech- oid taxonomy by Barucci et al. (1987), its recent extension nologies. (Fulchignoni et al., 2000), and an extended study of the size Earth-orbiting satellites have the advantage of observing distribution of main-belt asteroids (Cellino et al., 1991) are out of the terrestrial atmosphere; this allows them to be in just a few examples of the impact factor of this survey. -
Ice& Stone 2020
Ice & Stone 2020 WEEK 51: DECEMBER 13-19 Presented by The Earthrise Institute # 51 Authored by Alan Hale COMET OF THE WEEK: The Great Comet of 1680 Perihelion: 1680 December 18.49, q = 0.006 AU The Great Comet of 1680 over Rotterdam in The Netherlands, during late December 1680 as painted by the Dutch artist Lieve Verschuier. This particular comet was undoubtedly one of the brightest comets of the 17th Century, but it is also one of the most important comets in history from a scientific perspective, and perhaps even from the perspective of overall human history. While there were certainly plenty of superstitions attached to the comet’s appearance, the scientific investigations made of it were among the beginnings of the era in European history we now call The Enlightenment, and indeed, in a sense the Great Comet of 1680 can perhaps be considered as one of the sparks of that era. The significance began with the comet’s discovery, which was made on the morning of November 14, 1680, by a German astronomer residing in Coburg, Gottfried Kirch – the first comet ever to be discovered by means of a telescope. It was already around 4th magnitude at that time, and located near the star Regulus in the constellation Leo; from that point it traveled eastward and brightened rapidly, being closest to Earth (0.42 AU) on November 30. By that time it was a conspicuous naked-eye object with a tail 20 to 30 degrees long, and it remained visible for another week before disappearing into morning twilight. -
The Minor Planet Bulletin 44 (2017) 142
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 44, NUMBER 2, A.D. 2017 APRIL-JUNE 87. 319 LEONA AND 341 CALIFORNIA – Lightcurves from all sessions are then composited with no TWO VERY SLOWLY ROTATING ASTEROIDS adjustment of instrumental magnitudes. A search should be made for possible tumbling behavior. This is revealed whenever Frederick Pilcher successive rotational cycles show significant variation, and Organ Mesa Observatory (G50) quantified with simultaneous 2 period software. In addition, it is 4438 Organ Mesa Loop useful to obtain a small number of all-night sessions for each Las Cruces, NM 88011 USA object near opposition to look for possible small amplitude short [email protected] period variations. Lorenzo Franco Observations to obtain the data used in this paper were made at the Balzaretto Observatory (A81) Organ Mesa Observatory with a 0.35-meter Meade LX200 GPS Rome, ITALY Schmidt-Cassegrain (SCT) and SBIG STL-1001E CCD. Exposures were 60 seconds, unguided, with a clear filter. All Petr Pravec measurements were calibrated from CMC15 r’ values to Cousins Astronomical Institute R magnitudes for solar colored field stars. Photometric Academy of Sciences of the Czech Republic measurement is with MPO Canopus software. To reduce the Fricova 1, CZ-25165 number of points on the lightcurves and make them easier to read, Ondrejov, CZECH REPUBLIC data points on all lightcurves constructed with MPO Canopus software have been binned in sets of 3 with a maximum time (Received: 2016 Dec 20) difference of 5 minutes between points in each bin. -
Asteroid Regolith Weathering: a Large-Scale Observational Investigation
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2019 Asteroid Regolith Weathering: A Large-Scale Observational Investigation Eric Michael MacLennan University of Tennessee, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Recommended Citation MacLennan, Eric Michael, "Asteroid Regolith Weathering: A Large-Scale Observational Investigation. " PhD diss., University of Tennessee, 2019. https://trace.tennessee.edu/utk_graddiss/5467 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Eric Michael MacLennan entitled "Asteroid Regolith Weathering: A Large-Scale Observational Investigation." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Geology. Joshua P. Emery, Major Professor We have read this dissertation and recommend its acceptance: Jeffrey E. Moersch, Harry Y. McSween Jr., Liem T. Tran Accepted for the Council: Dixie L. Thompson Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) Asteroid Regolith Weathering: A Large-Scale Observational Investigation A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville Eric Michael MacLennan May 2019 © by Eric Michael MacLennan, 2019 All Rights Reserved. -
The Search for Water Ice on Comets and Asteroids
UNIVERSIDAD COMPLUTENSE DE MADRID FACULTAD DE CIENCIAS FÍSICAS TESIS DOCTORAL The Search for water ice on Comets and Asteroids La búsqueda de hielo de agua en Cometas y Asteroides MEMORIA PARA OPTAR AL GRADO DE DOCTOR PRESENTADA POR Laurence O’Rourke DIRECTOR Michael Küppers Madrid © Laurence O’Rourke, 2021 UNIVERSIDAD COMPLUTENSE DE MADRID FACULTAD DE CIENCIAS FÍSICAS TESIS DOCTORAL La búsqueda de hielo de agua en Cometas y Asteroides MEMORIA PARA OPTAR AL GRADO DE DOCTOR PRESENTADA POR Laurence O’Rourke DIRECTOR Dr. Michael Küppers The Search for water ice on Comets and Asteroids La búsqueda de hielo de agua en Cometas y Asteroides TESIS DOCTORAL LAURENCE O’ROURKE Departamento de Física de la Tierra y Astrofísica Facultad de Ciencias Físicas Universidad Complutense de Madrid A thesis submitted for the degree of Doctor en Astrofisica September 2020 Director: Dr. Michael Küppers Tutor: Prof. David Montes Gutiérrez Dedication I would like to dedicate this thesis to my wife Cristina & our children David and Paulina, and to my parents, Laurence and Rita (neé Curley) O’Rourke, who have both passed away but who would no doubt have been very proud of me for this achievement. Acknowledgements This work has been possible thanks to the great support and help provided by my PhD director Michael Küppers and by my UCM tutor, David Montes Gutiérrez. The published papers presented, provide an excellent overview of the significant collaborations I have had across the planetary science community with nearly 50 different co-authors represented in the papers. Their professionalism, expertise and friendship were vital to ensure that the papers I wrote were at the highest level. -
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. -
Astronomy 405 Solar System and ISM
Astronomy 405 Solar System and ISM Lecture 15 Asteroids February 18, 2013 Asteroids (minor planets) 1 Ceres - discovered in 1801 334 Chicago - 154 km, 7.7 yr Several 105 asteroids known. Total number may be 107, but the total mass is only 5x10-4 M⊕. Dactyl 2 243 Ida 1.6x1.2 km 55 km long Diemos Phobos 237,000 objects plotted in the figure E J Distribution of 1796 Asteroids in the Asteroid Belt The distribution of asteroids is not uniform. Kirkwood gaps - orbital resonance with Jupiter 2:1 resonance at 3.3 AU; 3:1 resonance at 2.5 AU Not empty in gaps; similar to gaps in Saturn’s rings. Tidal interaction => elliptical orbits => move out of gap 3:1 2:1 Distribution of Asteroids Trojan Asteroids Asteroid Belt Trojan Asteroids Lagrangian points - no force on 1:1 resonance with Jupiter. the test mass. Gravitational wells that L4, L5 (each) form equilateral provide unusual stability. triangles with M1 and M2 Mars and Neptune also have their own 1:1 resonant asteroids Asteroids with Orbits Crossing the Terrestrial Planets Amors - between Mars and Earth Apollos - cross Earth orbit approaching perihelion Atens - orbital semimajor axis < 1 AU Earth-crossing asteroids Earth-crossing asteroids were in the main belt at one time, but were perturbed by Jupiter and reoriented their orbits. M Some might be extinct V cometary nuclei. E M Collisions with Earth are Possible!!! Collisions among asteroids can shatter a large asteroid into an “asteroid family” that occupy near identical orbits. Kiyotsugu Hirayama first pointed this out in 1918. -
The Minor Planet Bulletin 37 (2010) 45 Classification for 244 Sita
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 37, NUMBER 2, A.D. 2010 APRIL-JUNE 41. LIGHTCURVE AND PHASE CURVE OF 1130 SKULD Robinson (2009) from his data taken in 2002. There is no evidence of any change of (V-R) color with asteroid rotation. Robert K. Buchheim Altimira Observatory As a result of the relatively short period of this lightcurve, every 18 Altimira, Coto de Caza, CA 92679 (USA) night provided at least one minimum and maximum of the [email protected] lightcurve. The phase curve was determined by polling both the maximum and minimum points of each night’s lightcurve. Since (Received: 29 December) The lightcurve period of asteroid 1130 Skuld is confirmed to be P = 4.807 ± 0.002 h. Its phase curve is well-matched by a slope parameter G = 0.25 ±0.01 The 2009 October-November apparition of asteroid 1130 Skuld presented an excellent opportunity to measure its phase curve to very small solar phase angles. I devoted 13 nights over a two- month period to gathering photometric data on the object, over which time the solar phase angle ranged from α = 0.3 deg to α = 17.6 deg. All observations used Altimira Observatory’s 0.28-m Schmidt-Cassegrain telescope (SCT) working at f/6.3, SBIG ST- 8XE NABG CCD camera, and photometric V- and R-band filters. Exposure durations were 3 or 4 minutes with the SNR > 100 in all images, which were reduced with flat and dark frames. -
Strange and Terrible Wonders: Climate Change In
STRANGE AND TERRIBLE WONDERS: CLIMATE CHANGE IN THE EARLY MODERN WORLD A Dissertation by CHRISTOPHER RYAN GILSON Submitted to the Office of Graduate and Professional Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Chair of Committee, Chester S. L. Dunning Committee Members, R. J. Q. Adams Joseph G. Dawson III Peter J. Hugill Head of Department, David Vaught August 2015 Major Subject: History Copyright 2015 Christopher R. Gilson ABSTRACT The study of climate and climatic change began during the Little Ice Age of the early modern world. Beginning in the sixteenth century, European clerics, scientists, and natural philosophers penned detailed observations of the era’s unusually cool and stormy weather. Scouring the historical record for evidence of similar phenomena in the past, early modern scholars concluded that the climate could change. By the eighteenth century, natural philosophers had identified at least five theories of climatic change, and many had adopted some variation of an anthropogenic explanation. The early modern observations described in this dissertation support the conclusion that cool temperatures and violent storms defined the Little Ice Age. This dissertation also demonstrates that modern notions of climate change are based upon 400 years of rich scholarship and spirited debate. This dissertation opens with a discussion of the origins of “climate” and meteorology in ancient Greek and Roman literature, particularly Aristotle’s Meteorologica. Although ancient scholars explored notions of environmental change, climate change—defined as such—was thought impossible. The translation and publication of ancient texts during the Renaissance contributed to the reexamination of nature and natural variability.