Simultaneous HARPS and HARPS-N Observations of the Earth Transit of 2014 As Seen from Jupiter: Detection of an Inverse Rossiter–Mclaughlin Effect
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Modelling and the Transit of Venus
Modelling and the transit of Venus Dave Quinn University of Queensland <[email protected]> Ron Berry University of Queensland <[email protected]> Introduction enior secondary mathematics students could justifiably question the rele- Svance of subject matter they are being required to understand. One response to this is to place the learning experience within a context that clearly demonstrates a non-trivial application of the material, and which thereby provides a definite purpose for the mathematical tools under consid- eration. This neatly complements a requirement of mathematics syllabi (for example, Queensland Board of Senior Secondary School Studies, 2001), which are placing increasing emphasis on the ability of students to apply mathematical thinking to the task of modelling real situations. Success in this endeavour requires that a process for developing a mathematical model be taught explicitly (Galbraith & Clatworthy, 1991), and that sufficient opportu- nities are provided to students to engage them in that process so that when they are confronted by an apparently complex situation they have the think- ing and operational skills, as well as the disposition, to enable them to proceed. The modelling process can be seen as an iterative sequence of stages (not ) necessarily distinctly delineated) that convert a physical situation into a math- 1 ( ematical formulation that allows relationships to be defined, variables to be 0 2 l manipulated, and results to be obtained, which can then be interpreted and a n r verified as to their accuracy (Galbraith & Clatworthy, 1991; Mason & Davis, u o J 1991). The process is iterative because often, at this point, limitations, inac- s c i t curacies and/or invalid assumptions are identified which necessitate a m refinement of the model, or perhaps even a reassessment of the question for e h t which we are seeking an answer. -
(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. -
Predictable Patterns in Planetary Transit Timing Variations and Transit Duration Variations Due to Exomoons
Astronomy & Astrophysics manuscript no. ms c ESO 2016 June 21, 2016 Predictable patterns in planetary transit timing variations and transit duration variations due to exomoons René Heller1, Michael Hippke2, Ben Placek3, Daniel Angerhausen4, 5, and Eric Agol6, 7 1 Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077 Göttingen, Germany; [email protected] 2 Luiter Straße 21b, 47506 Neukirchen-Vluyn, Germany; [email protected] 3 Center for Science and Technology, Schenectady County Community College, Schenectady, NY 12305, USA; [email protected] 4 NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA; [email protected] 5 USRA NASA Postdoctoral Program Fellow, NASA Goddard Space Flight Center, 8800 Greenbelt Road, Greenbelt, MD 20771, USA 6 Astronomy Department, University of Washington, Seattle, WA 98195, USA; [email protected] 7 NASA Astrobiology Institute’s Virtual Planetary Laboratory, Seattle, WA 98195, USA Received 22 March 2016; Accepted 12 April 2016 ABSTRACT We present new ways to identify single and multiple moons around extrasolar planets using planetary transit timing variations (TTVs) and transit duration variations (TDVs). For planets with one moon, measurements from successive transits exhibit a hitherto unde- scribed pattern in the TTV-TDV diagram, originating from the stroboscopic sampling of the planet’s orbit around the planet–moon barycenter. This pattern is fully determined and analytically predictable after three consecutive transits. The more measurements become available, the more the TTV-TDV diagram approaches an ellipse. For planets with multi-moons in orbital mean motion reso- nance (MMR), like the Galilean moon system, the pattern is much more complex and addressed numerically in this report. -
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 -
A Disintegrating Minor Planet Transiting a White Dwarf!
A Disintegrating Minor Planet Transiting a White Dwarf! Andrew Vanderburg1, John Asher Johnson1, Saul Rappaport2, Allyson Bieryla1, Jonathan Irwin1, John Arban Lewis1, David Kipping1,3, Warren R. Brown1, Patrick Dufour4, David R. Ciardi5, Ruth Angus1,6, Laura Schaefer1, David W. Latham1, David Charbonneau1, Charles Beichman5, Jason Eastman1, Nate McCrady7, Robert A. Wittenmyer8, & Jason T. Wright9,10. ! White dwarfs are the end state of most stars, including We initiated follow-up ground-based photometry to the Sun, after they exhaust their nuclear fuel. Between better time-resolve the transits seen in the K2 data (Figure 1/4 and 1/2 of white dwarfs have elements heavier than S1). We observed WD 1145+017 frequently over the course helium in their atmospheres1,2, even though these of about a month with the 1.2-meter telescope at the Fred L. elements should rapidly settle into the stellar interiors Whipple Observatory (FLWO) on Mt. Hopkins, Arizona; unless they are occasionally replenished3–5. The one of the 0.7-meter MINERVA telescopes, also at FLWO; abundance ratios of heavy elements in white dwarf and four of the eight 0.4-meter telescopes that compose the atmospheres are similar to rocky bodies in the Solar MEarth-South Array at Cerro Tololo Inter-American system6,7. This and the existence of warm dusty debris Observatory in Chile. Most of these data showed no disks8–13 around about 4% of white dwarfs14–16 suggest interesting or significant signals, but on two nights we that rocky debris from white dwarf progenitors’ observed deep (up to 40%), short-duration (5 minutes), planetary systems occasionally pollute the stars’ asymmetric transits separated by the dominant 4.5 hour atmospheres17. -
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 -
A Warm Terrestrial Planet with Half the Mass of Venus Transiting a Nearby Star∗
Astronomy & Astrophysics manuscript no. toi175 c ESO 2021 July 13, 2021 A warm terrestrial planet with half the mass of Venus transiting a nearby star∗ y Olivier D. S. Demangeon1; 2 , M. R. Zapatero Osorio10, Y. Alibert6, S. C. C. Barros1; 2, V. Adibekyan1; 2, H. M. Tabernero10; 1, A. Antoniadis-Karnavas1; 2, J. D. Camacho1; 2, A. Suárez Mascareño7; 8, M. Oshagh7; 8, G. Micela15, S. G. Sousa1, C. Lovis5, F. A. Pepe5, R. Rebolo7; 8; 9, S. Cristiani11, N. C. Santos1; 2, R. Allart19; 5, C. Allende Prieto7; 8, D. Bossini1, F. Bouchy5, A. Cabral3; 4, M. Damasso12, P. Di Marcantonio11, V. D’Odorico11; 16, D. Ehrenreich5, J. Faria1; 2, P. Figueira17; 1, R. Génova Santos7; 8, J. Haldemann6, N. Hara5, J. I. González Hernández7; 8, B. Lavie5, J. Lillo-Box10, G. Lo Curto18, C. J. A. P. Martins1, D. Mégevand5, A. Mehner17, P. Molaro11; 16, N. J. Nunes3, E. Pallé7; 8, L. Pasquini18, E. Poretti13; 14, A. Sozzetti12, and S. Udry5 1 Instituto de Astrofísica e Ciências do Espaço, CAUP, Universidade do Porto, Rua das Estrelas, 4150-762, Porto, Portugal 2 Departamento de Física e Astronomia, Faculdade de Ciências, Universidade do Porto, Rua Campo Alegre, 4169-007, Porto, Portugal 3 Instituto de Astrofísica e Ciências do Espaço, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, PT1749-016 Lisboa, Portugal 4 Departamento de Física da Faculdade de Ciências da Universidade de Lisboa, Edifício C8, 1749-016 Lisboa, Portugal 5 Observatoire de Genève, Université de Genève, Chemin Pegasi, 51, 1290 Sauverny, Switzerland 6 Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland 7 Instituto de Astrofísica de Canarias (IAC), Calle Vía Láctea s/n, E-38205 La Laguna, Tenerife, Spain 8 Departamento de Astrofísica, Universidad de La Laguna (ULL), E-38206 La Laguna, Tenerife, Spain 9 Consejo Superior de Investigaciones Cientícas, Spain 10 Centro de Astrobiología (CSIC-INTA), Crta. -
Correlations Between Planetary Transit Timing Variations, Transit Duration Variations and Brightness fluctuations Due to Exomoons
Correlations between planetary transit timing variations, transit duration variations and brightness fluctuations due to exomoons April 4, 2017 K:E:Naydenkin1 and D:S:Kaparulin2 1 Academic Lyceum of Tomsk, High school of Physics and Math, Vavilova 8 [email protected] 2 Tomsk State University, Physics Faculty, Lenina av. 50 [email protected] Abstract Modern theoretical estimates show that with the help of real equipment we are able to detect large satellites of exoplanets (about the size of the Ganymede), although, numerical attempts of direct exomoon detection were unsuccessful. Lots of methods for finding the satellites of exoplanets for various reasons have not yielded results. Some of the proposed methods are oriented on a more accurate telescopes than those exist today. In this work, we propose a method based on relationship between the transit tim- ing variation (TTV) and the brightness fluctuations (BF) before and after the planetary transit. With the help of a numerical simulation of the Earth- Moon system transits, we have constructed data on the BF and the TTV for arXiv:1704.00202v1 [astro-ph.IM] 1 Apr 2017 any configuration of an individual transit. The experimental charts obtained indicate an easily detectable near linear dependence. Even with an artificial increase in orbital speed of the Moon and high-level errors in measurements the patterns suggest an accurate correlation. A significant advantage of the method is its convenience for multiple moons systems due to an additive properties of the TTV and the BF. Its also important that mean motion res- onance (MMR) in system have no affect on ability of satellites detection. -
Detection of Exoplanets Using the Transit Method
Detection of Exoplanets Using the Transit Method De nnis A fanase v , T h e Geo rg e W a s h i n g t o n Un i vers i t y *, Washington, DC 20052 [email protected] Abstract I conducted differential photometry on a star GSC 3281-0800, a known host to exoplanet HAT-P-32b, using analysis software AstroImageJ. I plotted the measurements from a series of images taken during the transit, via ADU count given from an earth-based digital CCD camera. I was able to establish a definite light curve and learn more about the properties of this exoplanet. * Columbian College of Arts and Sciences, 2020 Introduction Exoplanets are the planets found outside of the solar system. Since the first exoplanet was discovered in 1992, a number of methods for detection have been established. Specific to this paper, I will be evaluating the star known as HAT-P-32 (also catalogued as GSC 3281- 0800) and its exoplanet HAT-P-32b using the transit method. Figure 1. Light curve when planet passes in front of a star. When a planet passes in front of a star, the brightness of that star as Transit Method observed by us becomes dimmer; which I have conducted my research on depends on the size of the planet. The detecting exoplanets with the transit data we observe will show a dip in flux method. This method relies on taking if a planet is transiting the star we are the light flux of the target star and observing, as shown in Fig. -
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.