Spectrogoniometry and Modeling of Martian and Lunar Analog Samples and Apollo Soils ⇑ Jeffrey R
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(101955) Bennu from OSIRIS-Rex Imaging and Thermal Analysis
ARTICLES https://doi.org/10.1038/s41550-019-0731-1 Properties of rubble-pile asteroid (101955) Bennu from OSIRIS-REx imaging and thermal analysis D. N. DellaGiustina 1,26*, J. P. Emery 2,26*, D. R. Golish1, B. Rozitis3, C. A. Bennett1, K. N. Burke 1, R.-L. Ballouz 1, K. J. Becker 1, P. R. Christensen4, C. Y. Drouet d’Aubigny1, V. E. Hamilton 5, D. C. Reuter6, B. Rizk 1, A. A. Simon6, E. Asphaug1, J. L. Bandfield 7, O. S. Barnouin 8, M. A. Barucci 9, E. B. Bierhaus10, R. P. Binzel11, W. F. Bottke5, N. E. Bowles12, H. Campins13, B. C. Clark7, B. E. Clark14, H. C. Connolly Jr. 15, M. G. Daly 16, J. de Leon 17, M. Delbo’18, J. D. P. Deshapriya9, C. M. Elder19, S. Fornasier9, C. W. Hergenrother1, E. S. Howell1, E. R. Jawin20, H. H. Kaplan5, T. R. Kareta 1, L. Le Corre 21, J.-Y. Li21, J. Licandro17, L. F. Lim6, P. Michel 18, J. Molaro21, M. C. Nolan 1, M. Pajola 22, M. Popescu 17, J. L. Rizos Garcia 17, A. Ryan18, S. R. Schwartz 1, N. Shultz1, M. A. Siegler21, P. H. Smith1, E. Tatsumi23, C. A. Thomas24, K. J. Walsh 5, C. W. V. Wolner1, X.-D. Zou21, D. S. Lauretta 1 and The OSIRIS-REx Team25 Establishing the abundance and physical properties of regolith and boulders on asteroids is crucial for understanding the for- mation and degradation mechanisms at work on their surfaces. Using images and thermal data from NASA’s Origins, Spectral Interpretation, Resource Identification, and Security-Regolith Explorer (OSIRIS-REx) spacecraft, we show that asteroid (101955) Bennu’s surface is globally rough, dense with boulders, and low in albedo. -
(155140) 2005 UD and (3200) Phaethon*
The Planetary Science Journal, 1:15 (15pp), 2020 June https://doi.org/10.3847/PSJ/ab8e45 © 2020. The Author(s). Published by the American Astronomical Society. New Evidence for a Physical Link between Asteroids (155140) 2005 UD and (3200) Phaethon* Maxime Devogèle1 , Eric MacLennan2, Annika Gustafsson3 , Nicholas Moskovitz1 , Joey Chatelain4, Galin Borisov5,6, Shinsuke Abe7, Tomoko Arai8, Grigori Fedorets2,9, Marin Ferrais10,11,12, Mikael Granvik2,13 , Emmanuel Jehin10, Lauri Siltala2,14, Mikko Pöntinen2, Michael Mommert1 , David Polishook15, Brian Skiff1, Paolo Tanga16, and Fumi Yoshida8 1 Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff, AZ 86001, USA; [email protected] 2 Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland 3 Department of Astronomy & Planetary Science, Northern Arizona University, P.O. Box 6010, Flagstaff, AZ 86011, USA 4 Las Cumbres Observatory, CA, USA 5 Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK 6 Institute of Astronomy and National Astronomical Observatory, Bulgarian Academy of Sciences, 72, Tsarigradsko Chaussèe Blvd., Sofia BG-1784, Bulgaria 7 Aerospace Engineering, Nihon University, 7-24-1 Narashinodai, Funabashi, Chiba 2748501, Japan 8 Planetary Exploration Research Center, Chiba Institute of Technology, Narashino, Japan 9 Astrophysics Research Centre, School of Mathematics and Physics, Queen’s University Belfast, Belfast BT7 1NN, UK 10 Space sciences, Technologies & Astrophysics Research (STAR) Institute University of Liège Allée du 6 Août 19, B-4000 Liège, Belgium 11 Aix Marseille Université, CNRS, LAM (Laboratoire d’Astrophysique de Marseille) UMR 7326, F-13388, Marseille, France 12 Space sciences, Technologies, France 13 Division of Space Technology, LuleåUniversity of Technology, Box 848, SE-98128 Kiruna, Sweden 14 Nordic Optical Telescope, Apartado 474, E-38700 S/C de La Palma, Santa Cruz de Tenerife, Spain 15 Faculty of Physics, Weizmann Institute of Science, 234 Herzl St. -
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. -
Extended Mission Orbit #2 (XMO2, ~1500 Km Altitude)
Carol A. Raymond Deputy Principal Investigator SBAG 17 Jet Propulsion Laboratory, Caltech 13 Jun 2017 • Spacecraft and instruments are healthy and data return has been excellent to date • Primary mission ended on June 30 2016. All mission objectives and Level-1 requirements were met. • Extended mission at Ceres ends June 30 2017. All mission objectives and Level-1 requirements were met. • Primary mission data archive complete pending ongoing review; extended mission archive is up to date • NASA is considering options for continued operations beyond June 2017 2 • Loss of third reaction wheel on April 23rd limits Dawn’s lifetime – but otherwise does not affect the mission – dependent on hydrazine jets for attitude control – Lifetime decreases with orbit altitude • Dawn is currently in a ~20000x50000 km eccentric orbit • Recently performed opposition observation • Four special journal issues in work: – Icarus: Geological Mapping (in revision) – Icarus: Mineralogical Mapping (submitted) – MAPS: Composition/Crosscutting (in submission) – Icarus: Occator Crater (in progress) – Interest in a special issue on ground ice: contact Britney Schmidt if you would like to participate 3 Ceres Extended Mission Timeline Start of End of End of Extended Mission Extended Mission Project Operations Operations XM1 Science Plan Extended Mission Orbit #1 (XMO1, ~385 km altitude) • Obtain IR spectra of high-priority targets (VIR) ✓ • Expand high-resolution color imaging (FC) ✓ • Improve elemental mapping (GRaND) ✓ • Expand high-resolution surface coverage for topography -
Mars Exploration Rovers: 4 Years on Mars
https://ntrs.nasa.gov/search.jsp?R=20080047431 2019-10-28T16:17:34+00:00Z Mars Exploration Rovers: 4 Years on Mars Geoffrey A. Landis This January, the Mars Exploration Rovers "Spirit" and "Opportunity" are starting their fifth year of exploring the surface of Mars, well over ten times their nominal 90-day design lifetime. This lecture discusses the Mars Exploration Rovers, presents the current mission status for the extended mission, some of the most results from the mission and how it is affecting our current view of Mars, and briefly presents the plans for the coming NASA missions to the surface of Mars and concepts for exploration with robots and humans into the next decade, and beyond. Four Years on Mars: the Mars Exploration Rovers Geoffrey A. Landis NASA John Glenn Research Center http://www.sff.net/people/geoffrey.landis Presentation at MIT Department of Aeronautics and Astronautics, January 18, 2008 Exploration - Landis Mars viewed from the Hubble Space Telescope Exploration - Landis Views of Mars in the early 20th century Lowell 1908 Sciaparelli 1888 Burroughs 1912 (cover painting by Frazetta) Tales of Outer Space ed. Donald A. Wollheim, Ace D-73, 1954 (From Winchell Chung's web page projectrho.com) Exploration - Landis Past Missions to Mars: first close up images of Mars from Mariner 4 Mariner 4 discovered Mars was a barren, moon-like desert Exploration - Landis Viking 1976 Signs of past water on Mars? orbiter Photo from orbit by the 1976 Viking orbiter Exploration - Landis Pathfinder and Sojourner Rover: a solar-powered mission -
A Tale of Two Sides: Pluto's Opposition Surge in 2018 and 2019
EPSC Abstracts Vol. 14, EPSC2020-546, 2020, updated on 27 Sep 2021 https://doi.org/10.5194/epsc2020-546 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. A Tale of Two Sides: Pluto's Opposition Surge in 2018 and 2019 Anne Verbiscer1, Paul Helfenstein2, Mark Showalter3, and Marc Buie4 1University of Virginia, Charlottesville, VA, USA ([email protected]) 2Cornell University, Ithaca, NY, USA ([email protected]) 3SETI Institute, Mountain View, CA, USA ([email protected]) 4Southwest Research Institute, Boulder, CO, USA ([email protected]) Near-opposition photometry employs remote sensing observations to reveal the microphysical properties of regolith-covered surfaces over a wide range of solar system bodies. When aligned directly opposite the Sun, objects exhibit an opposition effect, or surge, a dramatic, non-linear increase in reflectance seen with decreasing solar phase angle (the Sun-target-observer angle). This phenomenon is a consequence of both interparticle shadow hiding and a constructive interference phenomenon known as coherent backscatter [1-3]. While the size of the Earth’s orbit restricts observations of Pluto and its moons to solar phase angles no larger than α = 1.9°, the opposition surge, which occurs largely at α < 1°, can discriminate surface properties [4-6]. The smallest solar phase angles are attainable at node crossings when the Earth transits the solar disk as viewed from the object. In this configuration, a solar system body is at “true” opposition. When combined with observations acquired at larger phase angles, the resulting reflectance measurement can be related to the optical, structural, and thermal properties of the regolith and its inferred collisional history. -
Near-Infrared Photometry of Mercury Richard W
Georgia Journal of Science Volume 76 No.2 Scholarly Contributions from the Article 4 Membership and Others 2018 Near-Infrared Photometry of Mercury Richard W. Schmude Jr. Gordon State College, [email protected] Follow this and additional works at: https://digitalcommons.gaacademy.org/gjs Recommended Citation Schmude, Richard W. Jr. (2018) "Near-Infrared Photometry of Mercury," Georgia Journal of Science, Vol. 76, No. 2, Article 4. Available at: https://digitalcommons.gaacademy.org/gjs/vol76/iss2/4 This Research Articles is brought to you for free and open access by Digital Commons @ the Georgia Academy of Science. It has been accepted for inclusion in Georgia Journal of Science by an authorized editor of Digital Commons @ the Georgia Academy of Science. Near-Infrared Photometry of Mercury Acknowledgements I am grateful to Gordon State College for a Faculty Development Grand which was awarded in 2014 and enabled me to purchase the SSP-4 photometer. This research articles is available in Georgia Journal of Science: https://digitalcommons.gaacademy.org/gjs/vol76/iss2/4 Schmude: Near-Infrared Photometry of Mercury NEAR-INFRARED PHOTOMETRY OF MERCURY Richard W. Schmude, Jr. Gordon State College ABSTRACT This report summarizes 100 brightness measurements of Mercury made between May 2014 and September 2017 in the J and H near-infrared filters. Brightness models are reported for the J (solar phase angles between 52.3° and 124.5°) and H (solar phase angles between 38.6° and 133.0°) filters. Additional conclusions are as follows: Mercury’s brightness is within 0.1 magnitudes, at a given phase angle, for waxing and waning phases, and the geometric albedos at a solar phase angle of 0° are estimated to be 0.16 ± 0.03 and 0.24 ± 0.05 for the J and H filters, respectively. -
Scientific Observations with the Insight Solar Arrays: Dust, Clouds
Scientific Observations With the InSight Solar Arrays: Dust, Clouds, and Eclipses on Mars Ralph Lorenz, Mark Lemmon, Justin Maki, Donald Banfield, Aymeric Spiga, Constantinos Charalambous, Elizabeth Barrett, Jennifer Herman, Brett White, Samuel Pasco, et al. To cite this version: Ralph Lorenz, Mark Lemmon, Justin Maki, Donald Banfield, Aymeric Spiga, et al.. Scientific Obser- vations With the InSight Solar Arrays: Dust, Clouds, and Eclipses on Mars. Earth and Space Science, American Geophysical Union/Wiley, 2020, 7 (5), 10.1029/2019EA000992. hal-02872154 HAL Id: hal-02872154 https://hal.sorbonne-universite.fr/hal-02872154 Submitted on 17 Jun 2020 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. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License RESEARCH ARTICLE Scientific Observations With the InSight Solar Arrays: 10.1029/2019EA000992 Dust, Clouds, and Eclipses on Mars Special Section: Ralph D. Lorenz1 , Mark T. Lemmon2 , Justin Maki3 , Donald Banfield4 , InSight at Mars 5,6 7 3 3 Aymeric Spiga -
Brightness of Saturn's Rings with Decreasing Solar Elevation
Planetary and Space Science 58 (2010) 1758–1765 Contents lists available at ScienceDirect Planetary and Space Science journal homepage: www.elsevier.com/locate/pss Brightness of Saturn’s rings with decreasing solar elevation Alberto Flandes a,Ã, Linda Spilker a, Ryuji Morishima a, Stuart Pilorz b,Ce´dric Leyrat c, Nicolas Altobelli d, Shawn Brooks a, Scott G. Edgington a a Jet Propulsion Laboratory/California Institute of Technology, Pasadena, USA b SETI Institute, Mountain View, USA c Observatoire de Paris-LESIA, France d European Space and Astronomy Center, European Space Agency (ESAC/ESA), Madrid, Spain article info abstract Article history: Early ground-based and spacecraft observations suggested that the temperature of Saturn’s main rings Received 5 January 2010 (A, B and C) varied with the solar elevation angle, B0. Data from the composite infrared spectrometer Received in revised form (CIRS) on board Cassini, which has been in orbit around Saturn for more than five years, confirm this 31 March 2010 variation and have been used to derive the temperature of the main rings from a wide variety of Accepted 6 April 2010 geometries while B0 varied from near À243 to 03 (Saturn’s equinox). Available online 18 April 2010 Still, an unresolved issue in fully explaining this variation relates to how the ring particles are Keywords: organized and whether even a simple mono-layer or multi-layer approximation describes this best. We Planetary rings present a set of temperature data of the main rings of Saturn that cover the 233Frange of B0 angles Rings of Saturn 3 3 obtained with CIRS at low (a 30 ) and high (aZ120 ) phase angles. -
Opposition Effect on Comet 67P/Churyumov-Gerasimenko Using Rosetta-OSIRIS Images
Opposition effect on comet 67P/Churyumov-Gerasimenko using Rosetta-OSIRIS images Nafiseh Masoumzadeh, Nilda Oklay, Ludmilla Kolokolova, Holger Sierks, Sonia Fornasier, Maria A. Barucci, Jean-Baptiste Vincent, Cécilia Tubiana, Carsten Güttler, Frank Preusker, et al. To cite this version: Nafiseh Masoumzadeh, Nilda Oklay, Ludmilla Kolokolova, Holger Sierks, Sonia Fornasier, etal..Op- position effect on comet 67P/Churyumov-Gerasimenko using Rosetta-OSIRIS images. Astronomy and Astrophysics - A&A, EDP Sciences, 2017, 599, A11 (8 p.). 10.1051/0004-6361/201629734. insu-01473386 HAL Id: insu-01473386 https://hal-insu.archives-ouvertes.fr/insu-01473386 Submitted on 16 Sep 2020 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. A&A 599, A11 (2017) Astronomy DOI: 10.1051/0004-6361/201629734 & © ESO 2017 Astrophysics Opposition effect on comet 67P/Churyumov-Gerasimenko using Rosetta-OSIRIS images N. Masoumzadeh1;? , N. Oklay1, L. Kolokolova11, H. Sierks1, S. Fornasier13, M. A. Barucci13, J.-B. Vincent1, C. Tubiana1, C. Güttler1, F. Preusker22, F. Scholten22, S. Mottola22, P. H. Hasselmann13, C. Feller13, C. Barbieri4, P. L. Lamy5, R. Rodrigo6; 7, D. Koschny8, H. Rickman9; 10, M. F. A’Hearn11; 12; 1, J.-L. Bertaux14, I. -
Astronomy & Astrophysics Detailed Phase
A&A 376, 672–685 (2001) Astronomy DOI: 10.1051/0004-6361:20011028 & c ESO 2001 Astrophysics Detailed phase function of comet 28P/Neujmin 1? C. E. Delahodde1,2,K.J.Meech3,O.R.Hainaut1, and E. Dotto4 1 European Southern Observatory, Casilla 19001, Santiago, Chile 2 Institut d’Astrophysique de Marseille, Traverse du Siphon, 13376 Marseille Cedex 12, France 3 Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA 4 Osservatorio Astronomico di Torino, Strada Osservatorio 20, 100025 Pino Torinese (TO), Italy Received 11 April 2001 / Accepted 10 July 2001 Abstract. In 2000, comet 28P/Neujmin 1 was an ideal candidate for a phase function study: during its April opposition it reached a phase angle of α =0.8◦, and previous observations at similar heliocentric distances (r ≥ 4 AU) indicated that the comet was likely to be inactive. We observed this comet using ESO’s NTT and 2.2m telescopes at La Silla, on 6 epochs from April to August 2000, covering α = 0.8–8◦. These data were combined with a large set of data from 1985 to 1997. In order to disentangle the rotation effects from the phase effects, we obtained complete rotation coverage at opposition, providing us with a lightcurve template. We have obtained an improved rotation period of 12.75 0.03 hrs, with a full amplitude of ∆m =0.45 0.05 mag, which yields an axis ratio lower limit of 1.51 0.07. For each subsequent epochs, we have obtained enough rotation coverage to re-synchronize the lightcurve fragments with the template, and determine the magnitude change caused by the phase function. -
Mars Rover Churns up Questions with Sulfur-Rich Soil 14 March 2007
Mars Rover Churns Up Questions With Sulfur-Rich Soil 14 March 2007 The bright white and yellow material was hidden under a layer of normal-looking soil until Spirit's wheels churned it up while the rover was struggling to cross a patch of unexpectedly soft soil nearly a year ago. The right front wheel had stopped working a week earlier. Controllers at NASA's Jet Propulsion Laboratory, Pasadena, Calif., were trying to maneuver the rover backwards, dragging that wheel, to the north slope of a hill in order to spend the southern-hemisphere winter with solar panels tilted toward the sun. While driving eastward toward the northwestern flank of "McCool Hill," the wheels of NASA´s Mars Due to the difficulty crossing that patch, informally Exploration Rover Spirit churned up the largest amount named "Tyrone," the team chose to drive Spirit to a of bright soil discovered so far in the mission. This smaller but more accessible slope for the winter. image, taken on the rover´s 788th Martian day, or Spirit stayed put in its winter haven for nearly seven sol, of exploration (March 22, 2006), shows the strikingly months. Tyrone was one of several targets Spirit bright tone and large extent of the materials uncovered. Image credit: NASA/JPL-Caltech/Cornell examined from a distance during that period, using an infrared spectrometer to check their composition. The instrument detected small amounts of water bound to minerals in the soil. Some bright Martian soil containing lots of sulfur and a trace of water intrigues researchers who are The rover resumed driving in late 2006 when the studying information provided by NASA's Spirit Martian season brought sufficient daily sunshine to rover.