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Surface Characteristics of Transneptunian Objects and Centaurs from Photometry and Spectroscopy
Barucci et al.: Surface Characteristics of TNOs and Centaurs 647 Surface Characteristics of Transneptunian Objects and Centaurs from Photometry and Spectroscopy M. A. Barucci and A. Doressoundiram Observatoire de Paris D. P. Cruikshank NASA Ames Research Center The external region of the solar system contains a vast population of small icy bodies, be- lieved to be remnants from the accretion of the planets. The transneptunian objects (TNOs) and Centaurs (located between Jupiter and Neptune) are probably made of the most primitive and thermally unprocessed materials of the known solar system. Although the study of these objects has rapidly evolved in the past few years, especially from dynamical and theoretical points of view, studies of the physical and chemical properties of the TNO population are still limited by the faintness of these objects. The basic properties of these objects, including infor- mation on their dimensions and rotation periods, are presented, with emphasis on their diver- sity and the possible characteristics of their surfaces. 1. INTRODUCTION cally with even the largest telescopes. The physical char- acteristics of Centaurs and TNOs are still in a rather early Transneptunian objects (TNOs), also known as Kuiper stage of investigation. Advances in instrumentation on tele- belt objects (KBOs) and Edgeworth-Kuiper belt objects scopes of 6- to 10-m aperture have enabled spectroscopic (EKBOs), are presumed to be remnants of the solar nebula studies of an increasing number of these objects, and signifi- that have survived over the age of the solar system. The cant progress is slowly being made. connection of the short-period comets (P < 200 yr) of low We describe here photometric and spectroscopic studies orbital inclination and the transneptunian population of pri- of TNOs and the emerging results. -
Planet Positions: 1 Planet Positions
Planet Positions: 1 Planet Positions As the planets orbit the Sun, they move around the celestial sphere, staying close to the plane of the ecliptic. As seen from the Earth, the angle between the Sun and a planet -- called the elongation -- constantly changes. We can identify a few special configurations of the planets -- those positions where the elongation is particularly noteworthy. The inferior planets -- those which orbit closer INFERIOR PLANETS to the Sun than Earth does -- have configurations as shown: SC At both superior conjunction (SC) and inferior conjunction (IC), the planet is in line with the Earth and Sun and has an elongation of 0°. At greatest elongation, the planet reaches its IC maximum separation from the Sun, a value GEE GWE dependent on the size of the planet's orbit. At greatest eastern elongation (GEE), the planet lies east of the Sun and trails it across the sky, while at greatest western elongation (GWE), the planet lies west of the Sun, leading it across the sky. Best viewing for inferior planets is generally at greatest elongation, when the planet is as far from SUPERIOR PLANETS the Sun as it can get and thus in the darkest sky possible. C The superior planets -- those orbiting outside of Earth's orbit -- have configurations as shown: A planet at conjunction (C) is lined up with the Sun and has an elongation of 0°, while a planet at opposition (O) lies in the opposite direction from the Sun, at an elongation of 180°. EQ WQ Planets at quadrature have elongations of 90°. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
The Opposition and Tilt Effects of Saturn's Rings from HST Observations
The opposition and tilt effects of Saturn’s rings from HST observations Heikki Salo, Richard G. French To cite this version: Heikki Salo, Richard G. French. The opposition and tilt effects of Saturn’s rings from HST observa- tions. Icarus, Elsevier, 2010, 210 (2), pp.785. 10.1016/j.icarus.2010.07.002. hal-00693815 HAL Id: hal-00693815 https://hal.archives-ouvertes.fr/hal-00693815 Submitted on 3 May 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript The opposition and tilt effects of Saturn’s rings from HST observations Heikki Salo, Richard G. French PII: S0019-1035(10)00274-5 DOI: 10.1016/j.icarus.2010.07.002 Reference: YICAR 9498 To appear in: Icarus Received Date: 30 March 2009 Revised Date: 2 July 2010 Accepted Date: 2 July 2010 Please cite this article as: Salo, H., French, R.G., The opposition and tilt effects of Saturn’s rings from HST observations, Icarus (2010), doi: 10.1016/j.icarus.2010.07.002 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. -
Summer ASTRONOMICAL CALENDAR
2020 Buhl Planetarium & Observatory ASTRONOMICAL CALENDAR Summer JUNE 2020 1 Mon M13 globular cluster well-placed for observation (Use telescope in Hercules) 3 Wed Mercury at highest point in evening sky (Look west-northwest at sunset) 5 Fri Full Moon (Strawberry Moon) 9 Tues Moon within 3 degrees of both Jupiter and Saturn (Look south before dawn) 13 Sat Moon within 3 degrees of Mars (Look southeast before dawn) Moon at last quarter phase 20 Sat Summer solstice 21 Sun New Moon 27 Sat Bootid meteor shower peak (Best displays soon after dusk) 28 Sun Moon at first quarter phase JULY 2020 5 Sun Full Moon (Buck Moon) Penumbral lunar eclipse (Look south midnight into Monday) Moon within 2 degrees of Jupiter (Look south midnight into Monday) 6 Mon Moon within 3 degrees of Saturn (Look southwest before dawn) 8 Wed Venus at greatest brightness (Look east at dawn) 11 Sat Moon within 2 degrees of Mars (Look south before dawn) 12 Sun Moon at last quarter phase 14 Tues Jupiter at opposition (Look south midnight into Wednesday) 17 Fri Moon just over 3 degrees from Venus (Look east before dawn) 20 Mon New Moon; Saturn at opposition (Look south midnight into Tuesday) 27 Mon Moon at first quarter phase 28 Tues Piscis Austrinid meteor shower peak (Best displays before dawn) 29 Wed Southern Delta Aquariid and Alpha Capricornid meteor showers peak AUGUST 2020 1 Sat Moon within 2 degrees of Jupiter (Look southeast after dusk) 2 Sun Moon within 3 degrees of Saturn (Look southeast after dusk) 3 Mon Full Moon (Sturgeon Moon) 9 Sun Conjunction of the Moon and -
Historical Events Around US Neptune Cycles US Neptune: 22°25’ Virgo Greg Knell
Historical Events around US Neptune Cycles US Neptune: 22°25’ Virgo Greg Knell As we are in the midst of the United States’ Second Neptune Opposition, I initiated this research to consider the historical threads of this nation’s Neptunian narrative throughout its past 245 years. That this Neptune Opposition arrived to usher in the US’ First Pluto Return and its Fifth Chiron Return emphasized its prominence. Upon delving into this work, however, I came of the opinion that to isolate Neptune and its cycle would not do justice to what I sense is its place and purpose in the greater scheme of all relevant planetary cycles. Given that one Uranus cycle is roughly half of a Neptune cycle, Uranus Oppositions and Returns coincide with Neptune Squares, Oppositions, and Returns. Since its inception, the United States has had six Neptunian Timeline events: one return, two oppositions, and three squares. Among these, Pluto’s Timeline events have coincided four times. Given Pluto’s erratic orbit, this was by no means guaranteed. Pluto’s opposition occurred almost two-thirds through its entire orbit – in 1935, not even 100 years ago – instead of at the half way point of slightly before the turn of the Twentieth Century. This timing provides a clue as to the purpose, the plan, and the mission of these planetary cycles at this particular point in history. While it would be possible to isolate Neptune, perhaps, or any of the other cycles, I choose not to do so, as I do not believe that inquiry is worthy of individual pursuit for my purposes here. -
The Pancam Instrument for the Exomars Rover
ASTROBIOLOGY ExoMars Rover Mission Volume 17, Numbers 6 and 7, 2017 Mary Ann Liebert, Inc. DOI: 10.1089/ast.2016.1548 The PanCam Instrument for the ExoMars Rover A.J. Coates,1,2 R. Jaumann,3 A.D. Griffiths,1,2 C.E. Leff,1,2 N. Schmitz,3 J.-L. Josset,4 G. Paar,5 M. Gunn,6 E. Hauber,3 C.R. Cousins,7 R.E. Cross,6 P. Grindrod,2,8 J.C. Bridges,9 M. Balme,10 S. Gupta,11 I.A. Crawford,2,8 P. Irwin,12 R. Stabbins,1,2 D. Tirsch,3 J.L. Vago,13 T. Theodorou,1,2 M. Caballo-Perucha,5 G.R. Osinski,14 and the PanCam Team Abstract The scientific objectives of the ExoMars rover are designed to answer several key questions in the search for life on Mars. In particular, the unique subsurface drill will address some of these, such as the possible existence and stability of subsurface organics. PanCam will establish the surface geological and morphological context for the mission, working in collaboration with other context instruments. Here, we describe the PanCam scientific objectives in geology, atmospheric science, and 3-D vision. We discuss the design of PanCam, which includes a stereo pair of Wide Angle Cameras (WACs), each of which has an 11-position filter wheel and a High Resolution Camera (HRC) for high-resolution investigations of rock texture at a distance. The cameras and electronics are housed in an optical bench that provides the mechanical interface to the rover mast and a planetary protection barrier. -
Contents JUPITER Transits
1 Contents JUPITER Transits..........................................................................................................5 JUPITER Conjunct Sun..............................................................................................6 JUPITER Opposite Sun............................................................................................10 JUPITER Sextile Sun...............................................................................................14 JUPITER Square Sun...............................................................................................17 JUPITER Trine Sun..................................................................................................20 JUPITER Conjunct Moon.........................................................................................23 JUPITER Opposite Moon.........................................................................................28 JUPITER Sextile Moon.............................................................................................32 JUPITER Square Moon............................................................................................36 JUPITER Trine Moon................................................................................................40 JUPITER Conjunct Mercury.....................................................................................45 JUPITER Opposite Mercury.....................................................................................48 JUPITER Sextile Mercury........................................................................................51 -
Mars Surface Context Cameras Past, Present, and Future 10.1002/2016EA000166 M
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Aberystwyth Research Portal Aberystwyth University Mars surface context cameras past, present and future Gunn, Matthew; Cousins, Claire Published in: Earth and Space Science DOI: 10.1002/2016EA000166 Publication date: 2016 Citation for published version (APA): Gunn, M., & Cousins, C. (2016). Mars surface context cameras past, present and future. Earth and Space Science, 3(4), 144-162. https://doi.org/10.1002/2016EA000166 Document License CC BY-NC-ND General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. tel: +44 1970 62 2400 email: [email protected] Download date: 09. Jul. 2020 PUBLICATIONS Earth and Space Science REVIEW Mars surface context cameras past, present, and future 10.1002/2016EA000166 M. D. Gunn1 and C. R. Cousins2 Key Points: 1Institute of Maths, Physics and Computer Science, Aberystwyth University, Aberystwyth, UK, 2Department of Earth and • Camera systems have been a core component of all instrument payloads Environmental Sciences, Irvine Building, University of St Andrews, St. -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
Exomars Presentation
EE XX OO MM AA RR SS Mission Objectives & Science Strategy J. L. Vago and the ExoMars project team Solar System Working Group – SSWG 8 September 2005, ESA HQ (F) The Aurora Programme ESA’s new programme to prepare for the human exploration of the Solar system. Characteristics: Defines a long-term space exploration strategy for Europe; Focuses on exploration infrastructure and technology development; Robotic missions in preparation of future human ones; Synergy between scientific and technological objectives; Provides a framework for cooperation with other space agencies. 2 What is ExoMars? • Is the first mission of ESA’s Aurora Exploration Programme. • ExoMars will deploy two science elements on the Martian surface: a Rover carrying the Pasteur payload, and a fixed station —the Geophysics/Environment Package (GEP). Scientific Objectives: Pasteur Rover: ¾ To search for traces of past and present life on Mars; ¾ To characterise, in the shallow subsurface, vertical distribution profiles for water and geochemical composition. GEP: ¾ To measure planetary geophysics parameters important to understand Mars’s evolution and habitability; ¾ To study the surface environment and identify hazards to human missions. Technology Objectives: To develop a European capability to land large payloads on Mars; To demonstrate high surface mobility and access to the subsurface; 3 To prepare technologies necessary for a Mars Sample Return mission. Why life on Mars? • Early in the history of Mars, liquid water was present on its surface; • Some of the processes considered important for the origin of life on Earth may have also been present on early Mars; • Asteroid and comet impacts may have been less severe on Mars, favouring the survival of life; • Establishing if there ever was life on Mars is fundamental for planning future human missions. -
Neptune Closest to Earth for 2020 - a September 2020 Sky Event from the Astronomy Club of Asheville
Neptune Closest to Earth for 2020 - a September 2020 Sky Event from the Astronomy Club of Asheville Earth reaches “opposition” with the solar Not to Scale system’s most distant planet on September 11th. At opposition, speedier Earth, moving counterclockwise on its inside lane, laps the outer planet, positioning the Sun directly opposite the Earth from Neptune. This puts Neptune closest to Earth for the year and in great observing position for those using a telescope. Rising at dusk and setting at dawn, the planet Neptune is visible all night during the month of September. Located in the constellation Aquarius, Neptune is positioned some 2.7 billion miles (or 4 light-hours) away from Earth at “opposition” this month. _________________________________ At magnitude 7.8, Neptune will appear as a small blue disk in most amateur telescopes. You will find Neptune along the ecliptic in the constellation Aquarius this year. In September, it will be located about 2° southeast of the 4.2 magnitude star Phi (φ) Aquarii. Like Uranus, Neptune has an upper atmosphere with significant methane gas (CH4). Methane strongly absorbs red light; thus, the blue end of the light spectrum, from the reflected sunlight, is what primarily passes through to our eyes, when observing this distant planet. Neptune’s Discovery Neptune was the 2nd solar system planet to be discovered! Uranus’ discovery preceded it, when William Herschel observed its blue disk, quite by accident, in 1781. But Uranus’ orbit had an unexplained problem – a deviation that astronomers called a “perturbation”. Johannes Kepler’s laws of planetary motion and Isaac Newton’s laws of motion and gravity could not adequately explain this perturbation in Uranus’ orbit.