The Observer March 2016
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THE PLANETARY REPORT FAREWELL, SEPTEMBER EQUINOX 2017 VOLUME 37, NUMBER 3 CASSINI Planetary.Org CELEBRATING a LEGACY of DISCOVERIES
THE PLANETARY REPORT FAREWELL, SEPTEMBER EQUINOX 2017 VOLUME 37, NUMBER 3 CASSINI planetary.org CELEBRATING A LEGACY OF DISCOVERIES ATMOSPHERIC CHANGES C DYNAMIC RINGS C COMPLICATED TITAN C ACTIVE ENCELADUS ABOUT THIS ISSUE LINDA J. SPILKER is Cassini project scientist at the Jet Propulsion Laboratory. IN 2004, Cassini, the most distant planetary seafloor. As a bonus, it has revealed jets of orbiter ever launched by humanity, arrived at water vapor and ice particles shooting out of Saturn. For 13 years, through its primary and fractures at the moon’s south pole. two extended missions, this spacecraft has These discoveries have fundamentally been making astonishing discoveries, reshap- altered many of our concepts of where life ing and changing our understanding of this may be found in our solar system. Cassini’s unique planetary system within our larger observations at Enceladus and Titan have made system of unique worlds. A few months ater exploring these ocean worlds a major focus for arrival, Cassini released Huygens, European planetary science. New insights from these dis- Space Agency’s parachuted probe built to coveries also have implications for potentially study the atmosphere and surface of Titan habitable worlds beyond our solar system. and image its surface for the very first time. In this special issue of The Planetary Report, a handful of Cassini scientists share some results from their studies of Saturn and its moons. Because there’s no way to fit every- thing into this slim volume, they’ve focused on a few highlights. Meanwhile, Cassini continues performing its Grand Finale orbits between the rings and the top of Saturn’s atmosphere, circling the planet once every 6.5 days. -
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. -
The Dynamics of Plutinos
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by CERN Document Server The dynamics of Plutinos Qingjuan Yu and Scott Tremaine Princeton University Observatory, Peyton Hall, Princeton, NJ 08544-1001, USA ABSTRACT Plutinos are Kuiper-belt objects that share the 3:2 Neptune resonance with Pluto. The long-term stability of Plutino orbits depends on their eccentric- ity. Plutinos with eccentricities close to Pluto (fractional eccentricity difference < ∆e=ep = e ep =ep 0:1) can be stable because the longitude difference librates, | − | ∼ in a manner similar to the tadpole and horseshoe libration in coorbital satellites. > Plutinos with ∆e=ep 0:3 can also be stable; the longitude difference circulates ∼ and close encounters are possible, but the effects of Pluto are weak because the encounter velocity is high. Orbits with intermediate eccentricity differences are likely to be unstable over the age of the solar system, in the sense that encoun- ters with Pluto drive them out of the 3:2 Neptune resonance and thus into close encounters with Neptune. This mechanism may be a source of Jupiter-family comets. Subject headings: planets and satellites: Pluto — Kuiper Belt, Oort cloud — celestial mechanics, stellar dynamics 1. Introduction The orbit of Pluto has a number of unusual features. It has the highest eccentricity (ep =0:253) and inclination (ip =17:1◦) of any planet in the solar system. It crosses Neptune’s orbit and hence is susceptible to strong perturbations during close encounters with that planet. However, close encounters do not occur because Pluto is locked into a 3:2 orbital resonance with Neptune, which ensures that conjunctions occur near Pluto’s aphelion (Cohen & Hubbard 1965). -
Spacecraft Imaging for Amateurs an International Community of Space
Planetary Close-ups emily lakdawalla Spacecraft Imaging for Amateurs An international community of space This is Mars’s Big Sky Country, a windswept, nearly featureless plain. Tiny ripples in the rust-colored sand march farther than the eye can see, to a horizon so fl at one might be able to see the curvature of the planet. As far as anyone knows, those ripples have not budged in eons. But all is not still; gaze upward, and you might be surprised by the rapid motion overhead, where feathery cirrus clouds, frosty with bright crystals of water ice, fl oat on high Martian winds. The scene is from Meridiani Planum, composed from eight images captured by the Mars Exploration Rover Opportunity just before she reached a deep crater named Victoria, on the 950th Martian day of her mission. But the beautiful image was not created by anyone on the Mars Exploration Rover team; no scientist would likely have Earthbound produced it, because it owes its beauty as much to art as it observers never does to science. see Mars as a The image is the collaborative creation of a whole crescent, but amateur-imagesmith community; six people, each from spacecraft do. a diff erent country, had a hand in it. Twelve hours after The author cre- Opportunity took the photos, the data had been received on ated this view Earth and posted to the internet. Within another 17 hours, from six images rover fans had found the photos, assembled the mosaic, taken by Viking and shaded the sand and sky based on color photos Oppor- Orbiter 2 in tunity had taken of a similar landscape the day before. -
Alactic Observer
alactic Observer G John J. McCarthy Observatory Volume 14, No. 2 February 2021 International Space Station transit of the Moon Composite image: Marc Polansky February Astronomy Calendar and Space Exploration Almanac Bel'kovich (Long 90° E) Hercules (L) and Atlas (R) Posidonius Taurus-Littrow Six-Day-Old Moon mosaic Apollo 17 captured with an antique telescope built by John Benjamin Dancer. Dancer is credited with being the first to photograph the Moon in Tranquility Base England in February 1852 Apollo 11 Apollo 11 and 17 landing sites are visible in the images, as well as Mare Nectaris, one of the older impact basins on Mare Nectaris the Moon Altai Scarp Photos: Bill Cloutier 1 John J. McCarthy Observatory In This Issue Page Out the Window on Your Left ........................................................................3 Valentine Dome ..............................................................................................4 Rocket Trivia ..................................................................................................5 Mars Time (Landing of Perseverance) ...........................................................7 Destination: Jezero Crater ...............................................................................9 Revisiting an Exoplanet Discovery ...............................................................11 Moon Rock in the White House....................................................................13 Solar Beaming Project ..................................................................................14 -
Distant Ekos: 2012 BX85 and 4 New Centaur/SDO Discoveries: 2000 GQ148, 2012 BR61, 2012 CE17, 2012 CG
Issue No. 79 February 2012 r ✤✜ s ✓✏ DISTANT EKO ❞✐ ✒✑ The Kuiper Belt Electronic Newsletter ✣✢ Edited by: Joel Wm. Parker [email protected] www.boulder.swri.edu/ekonews CONTENTS News & Announcements ................................. 2 Abstracts of 8 Accepted Papers ......................... 3 Newsletter Information .............................. .....9 1 NEWS & ANNOUNCEMENTS There was 1 new TNO discovery announced since the previous issue of Distant EKOs: 2012 BX85 and 4 new Centaur/SDO discoveries: 2000 GQ148, 2012 BR61, 2012 CE17, 2012 CG Objects recently assigned numbers: 2010 EP65 = (312645) 2008 QD4 = (315898) 2010 EN65 = (316179) 2008 AP129 = (315530) Objects recently assigned names: 1997 CS29 = Sila-Nunam Current number of TNOs: 1249 (including Pluto) Current number of Centaurs/SDOs: 337 Current number of Neptune Trojans: 8 Out of a total of 1594 objects: 644 have measurements from only one opposition 624 of those have had no measurements for more than a year 316 of those have arcs shorter than 10 days (for more details, see: http://www.boulder.swri.edu/ekonews/objects/recov_stats.jpg) 2 PAPERS ACCEPTED TO JOURNALS The Dynamical Evolution of Dwarf Planet (136108) Haumea’s Collisional Family: General Properties and Implications for the Trans-Neptunian Belt Patryk Sofia Lykawka1, Jonathan Horner2, Tadashi Mukai3 and Akiko M. Nakamura3 1 Astronomy Group, Faculty of Social and Natural Sciences, Kinki University, Japan 2 Department of Astrophysics, School of Physics, University of New South Wales, Australia 3 Department of Earth and Planetary Sciences, Kobe University, Japan Recently, the first collisional family was identified in the trans-Neptunian belt (otherwise known as the Edgeworth-Kuiper belt), providing direct evidence of the importance of collisions between trans-Neptunian objects (TNOs). -
1 Resonant Kuiper Belt Objects
Resonant Kuiper Belt Objects - a Review Renu Malhotra Lunar and Planetary Laboratory, The University of Arizona, Tucson, AZ, USA Email: [email protected] Abstract Our understanding of the history of the solar system has undergone a revolution in recent years, owing to new theoretical insights into the origin of Pluto and the discovery of the Kuiper belt and its rich dynamical structure. The emerging picture of dramatic orbital migration of the planets driven by interaction with the primordial Kuiper belt is thought to have produced the final solar system architecture that we live in today. This paper gives a brief summary of this new view of our solar system's history, and reviews the astronomical evidence in the resonant populations of the Kuiper belt. Introduction Lying at the edge of the visible solar system, observational confirmation of the existence of the Kuiper belt came approximately a quarter-century ago with the discovery of the distant minor planet (15760) Albion (formerly 1992 QB1, Jewitt & Luu 1993). With the clarity of hindsight, we now recognize that Pluto was the first discovered member of the Kuiper belt. The current census of the Kuiper belt includes more than 2000 minor planets at heliocentric distances between ~30 au and ~50 au. Their orbital distribution reveals a rich dynamical structure shaped by the gravitational perturbations of the giant planets, particularly Neptune. Theoretical analysis of these structures has revealed a remarkable dynamic history of the solar system. The story is as follows (see Fernandez & Ip 1984, Malhotra 1993, Malhotra 1995, Fernandez & Ip 1996, and many subsequent works). -
THE PLANETARY REPORT JUNE SOLSTICE 2016 VOLUME 36, NUMBER 2 Planetary.Org
THE PLANETARY REPORT JUNE SOLSTICE 2016 VOLUME 36, NUMBER 2 planetary.org ILLUMINATING CERES DAWN SHEDS NEW LIGHT ON AN ENIGMATIC WORLD BREAKTHROUGH STARSHOT C LIGHTSAIL 2 TEST C MEMBERSHIP UPGRADES SNAPSHOTS FROM SPACE EMILY STEWART LAKDAWALLA blogs at planetary.org/blog. Black Sands of Mars ON SOL 1192 (December 13, 2015), Curiosity approached the side of Namib, a Faccin and Marco Bonora Image: NASA/JPL/MSSS/Elisabetta massive barchan sand dune. Namib belongs to a field of currently active dark basaltic sand dunes that form a long barrier between the rover and the tantalizing rocks of Mount Sharp. This view, processed by Elisabetta Bonora and Marco Faccin, features wind-carved yardangs (crests or ridges ) of Mount Sharp in the background. After taking this set of photos, Curiosity went on to sample sand from the dune, and it is now working its way through a gap in the dune field on the way to the mountain. —Emily Stewart Lakdawalla SEE MORE AMATEUR-PROCESSED SPACE IMAGES planetary.org/amateur SEE MORE EVERY DAY! planetary.org/blogs 2 THE PLANETARY REPORT C JUNE SOLSTICE 2016 CONTENTS JUNE SOLSTICE 2016 COVER STORY Unveiling Ceres 6 Simone Marchi on why Ceres is a scientific treasure chest for Dawn. Pathway to the Stars Looking back at years of Society-led solar sail 10 development as Breakthrough Starshot is announced. Life, the Universe, and Everything 13 Planetary Radio in Death Valley. ADVOCATING FOR SPACE Partisan Peril 18 Casey Dreier looks at the U.S. President’s impact on space policy and legislation. DEVELOPMENTS IN SPACE SCIENCE Update on LightSail 2 20 Bruce Betts details the progress we’ve made in the year since LightSail 1 launched. -
1950 Da, 205, 269 1979 Va, 230 1991 Ry16, 183 1992 Kd, 61 1992
Cambridge University Press 978-1-107-09684-4 — Asteroids Thomas H. Burbine Index More Information 356 Index 1950 DA, 205, 269 single scattering, 142, 143, 144, 145 1979 VA, 230 visual Bond, 7 1991 RY16, 183 visual geometric, 7, 27, 28, 163, 185, 189, 190, 1992 KD, 61 191, 192, 192, 253 1992 QB1, 233, 234 Alexandra, 59 1993 FW, 234 altitude, 49 1994 JR1, 239, 275 Alvarez, Luis, 258 1999 JU3, 61 Alvarez, Walter, 258 1999 RL95, 183 amino acid, 81 1999 RQ36, 61 ammonia, 223, 301 2000 DP107, 274, 304 amoeboid olivine aggregate, 83 2000 GD65, 205 Amor, 251 2001 QR322, 232 Amor group, 251 2003 EH1, 107 Anacostia, 179 2007 PA8, 207 Anand, Viswanathan, 62 2008 TC3, 264, 265 Angelina, 175 2010 JL88, 205 angrite, 87, 101, 110, 126, 168 2010 TK7, 231 Annefrank, 274, 275, 289 2011 QF99, 232 Antarctic Search for Meteorites (ANSMET), 71 2012 DA14, 108 Antarctica, 69–71 2012 VP113, 233, 244 aphelion, 30, 251 2013 TX68, 64 APL, 275, 292 2014 AA, 264, 265 Apohele group, 251 2014 RC, 205 Apollo, 179, 180, 251 Apollo group, 230, 251 absorption band, 135–6, 137–40, 145–50, Apollo mission, 129, 262, 299 163, 184 Apophis, 20, 269, 270 acapulcoite/ lodranite, 87, 90, 103, 110, 168, 285 Aquitania, 179 Achilles, 232 Arecibo Observatory, 206 achondrite, 84, 86, 116, 187 Aristarchus, 29 primitive, 84, 86, 103–4, 287 Asporina, 177 Adamcarolla, 62 asteroid chronology function, 262 Adeona family, 198 Asteroid Zoo, 54 Aeternitas, 177 Astraea, 53 Agnia family, 170, 198 Astronautica, 61 AKARI satellite, 192 Aten, 251 alabandite, 76, 101 Aten group, 251 Alauda family, 198 Atira, 251 albedo, 7, 21, 27, 185–6 Atira group, 251 Bond, 7, 8, 9, 28, 189 atmosphere, 1, 3, 8, 43, 66, 68, 265 geometric, 7 A- type, 163, 165, 167, 169, 170, 177–8, 192 356 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-1-107-09684-4 — Asteroids Thomas H. -
PAC March 9 10 2020 Report
NASA ADVISORY COUNCIL PLANETARY SCIENCE ADVISORY COMMITTEE March 9-10, 2020 NASA Headquarters Washington, DC MEETING REPORT _____________________________________________________________ Anne Verbiscer, Chair ____________________________________________________________ Stephen Rinehart, Executive Secretary Table of Contents Opening and Announcements, Introductions 3 PSD Update and Status 3 PSD R&A Status 5 Planetary Protection 7 Discussion 8 Mars Exploration Program 8 Lunar Exploration Program 9 PDCO 11 Planetary Data System 12 PDS at Headquarters 13 Findings and Discussion 13 General Comments 13 Exoplanets in Our Backyard 14 AP Assets for Solar System Observations 15 Solar System Science with JWST 16 Mercury Group 17 VEXAG 17 SBAG 18 OPAG 19 MEPAG 19 MAPSIT 20 LEAG 21 CAPTEM 21 Discussion 22 Findings and Recommendations Discussion 23 Appendix A- Attendees Appendix B- Membership roster Appendix C- Agenda Appendix D- Presentations Prepared by Joan M. Zimmermann Zantech, Inc. 2 Opening, Announcements, Around the Table Identification Executive Secretary of the Planetary Science Advisory Committee (PAC), Dr. Stephen Rinehart, opened the meeting and made administrative announcements. PAC Chair, Dr. Anne Verbiscer, welcomed everyone to the virtual meeting. Announcements were made around the table and on Webex. PSD Status Report Dr. Lori Glaze, Director of the Planetary Science Division, gave a status report. First addressing the President’s Budget Request (PBR) for Fiscal Year 2021 (FY21) for the Science Mission Directorate (SMD), Dr. Glaze noted that it was one of the strongest science budgets in NASA history, representing a 12% increase over the enacted FY20 budget. The total PBR keeps NASA on track to land on the Moon by 2024; and to help prepare for human exploration at Mars. -
Atmospheres and Surfaces of Small Bodies and Dwarf Planets in the Kuiper Belt
EPJ Web of Conferences 9, 267–276 (2010) DOI: 10.1051/epjconf/201009021 c Owned by the authors, published by EDP Sciences, 2010 Atmospheres and surfaces of small bodies and dwarf planets in the Kuiper Belt E.L. Schallera Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA Abstract. Kuiper Belt Objects (KBOs) are icy relics orbiting the sun beyond Neptune left over from the planetary accretion disk. These bodies act as unique tracers of the chemical, thermal, and dynamical history of our solar system. Over 1000 Kuiper Belt Objects (KBOs) and centaurs (objects with perihelia between the giant planets) have been discovered over the past two decades. While the vast majority of these objects are small (< 500 km in diameter), there are now many objects known that are massive enough to attain hydrostatic equilibrium (and are therefore considered dwarf planets) including Pluto, Eris, MakeMake, and Haumea. The discoveries of these large objects, along with the advent of large (> 6-meter) telescopes, have allowed for the first detailed studies of their surfaces and atmospheres. Visible and near-infrared spectroscopy of KBOs and centaurs has revealed a great diversity of surface compositions. Only the largest and coldest objects are capable of retaining volatile ices and atmospheres. Knowledge of the dynamics, physical properties, and collisional history of objects in the Kuiper belt is important for understanding solar system formation and evolution. 1 Introduction The existence of a belt of debris beyond Neptune left over from planetary accretion was proposed by Kuiper in 1951 [1]. Though Pluto was discovered in 1930, it took over sixty years for other Kuiper belt objects (KBOs) to be detected [2] and for Pluto to be recognized as the first known member of a larger population now known to consist of over 1000 objects (Fig. -
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.