Non-Gravitational Motion of the Jupiter-Family Comet 81P/Wild 2
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Observational Constraints on Surface Characteristics of Comet Nuclei
Observational Constraints on Surface Characteristics of Comet Nuclei Humberto Campins ([email protected] u) Lunar and Planetary Laboratory, University of Arizona Yanga Fernandez University of Hawai'i Abstract. Direct observations of the nuclear surfaces of comets have b een dicult; however a growing number of studies are overcoming observational challenges and yielding new information on cometary surfaces. In this review, we fo cus on recent determi- nations of the alb edos, re ectances, and thermal inertias of comet nuclei. There is not much diversity in the geometric alb edo of the comet nuclei observed so far (a range of 0.025 to 0.06). There is a greater diversity of alb edos among the Centaurs, and the sample of prop erly observed TNOs (2) is still to o small. Based on their alb edos and Tisserand invariants, Fernandez et al. (2001) estimate that ab out 5% of the near-Earth asteroids have a cometary origin, and place an upp er limit of 10%. The agreement between this estimate and two other indep endent metho ds provide the strongest constraint to date on the fraction of ob jects that comets contribute to the p opulation of near-Earth asteroids. There is a diversity of visible colors among comets, extinct comet candidates, Centaurs and TNOs. Comet nuclei are clearly not as red as the reddest Centaurs and TNOs. What Jewitt (2002) calls ultra-red matter seems to be absent from the surfaces of comet nuclei. Rotationally resolved observations of b oth colors and alb edos are needed to disentangle the e ects of rotational variability from other intrinsic qualities. -
KAREN J. MEECH February 7, 2019 Astronomer
BIOGRAPHICAL SKETCH – KAREN J. MEECH February 7, 2019 Astronomer Institute for Astronomy Tel: 1-808-956-6828 2680 Woodlawn Drive Fax: 1-808-956-4532 Honolulu, HI 96822-1839 [email protected] PROFESSIONAL PREPARATION Rice University Space Physics B.A. 1981 Massachusetts Institute of Tech. Planetary Astronomy Ph.D. 1987 APPOINTMENTS 2018 – present Graduate Chair 2000 – present Astronomer, Institute for Astronomy, University of Hawaii 1992-2000 Associate Astronomer, Institute for Astronomy, University of Hawaii 1987-1992 Assistant Astronomer, Institute for Astronomy, University of Hawaii 1982-1987 Graduate Research & Teaching Assistant, Massachusetts Inst. Tech. 1981-1982 Research Specialist, AAVSO and Massachusetts Institute of Technology AWARDS 2018 ARCs Scientist of the Year 2015 University of Hawai’i Regent’s Medal for Research Excellence 2013 Director’s Research Excellence Award 2011 NASA Group Achievement Award for the EPOXI Project Team 2011 NASA Group Achievement Award for EPOXI & Stardust-NExT Missions 2009 William Tylor Olcott Distinguished Service Award of the American Association of Variable Star Observers 2006-8 National Academy of Science/Kavli Foundation Fellow 2005 NASA Group Achievement Award for the Stardust Flight Team 1996 Asteroid 4367 named Meech 1994 American Astronomical Society / DPS Harold C. Urey Prize 1988 Annie Jump Cannon Award 1981 Heaps Physics Prize RESEARCH FIELD AND ACTIVITIES • Developed a Discovery mission concept to explore the origin of Earth’s water. • Co-Investigator on the Deep Impact, Stardust-NeXT and EPOXI missions, leading the Earth-based observing campaigns for all three. • Leads the UH Astrobiology Research interdisciplinary program, overseeing ~30 postdocs and coordinating the research with ~20 local faculty and international partners. -
Investigation of Dust and Water Ice in Comet 9P/Tempel 1 from Spitzer Observations of the Deep Impact Event
A&A 542, A119 (2012) Astronomy DOI: 10.1051/0004-6361/201118718 & c ESO 2012 Astrophysics Investigation of dust and water ice in comet 9P/Tempel 1 from Spitzer observations of the Deep Impact event A. Gicquel1, D. Bockelée-Morvan1 ,V.V.Zakharov1,2,M.S.Kelley3, C. E. Woodward4, and D. H. Wooden5 1 LESIA, Observatoire de Paris, CNRS, UPMC, Université Paris-Diderot, 5 place Jules Janssen, 92195 Meudon, France e-mail: [adeline.gicquel;dominique.bockelee;vladimir.zakharov]@obspm.fr 2 Gordien Strato, France 3 Department of Astronomy, University of Maryland, College Park, MD 20742-2421, USA e-mail: [email protected] 4 Minnesota Institute for Astrophysics, University of Minnesota, 116 Church St SE, Minneapolis, MN 55455, USA e-mail: [email protected] 5 NASA Ames Research Center, Space Science Division, USA e-mail: [email protected] Received 22 December 2011 / Accepted 9 February 2012 ABSTRACT Context. The Spitzer spacecraft monitored the Deep Impact event on 2005 July 4 providing unique infrared spectrophotometric data that enabled exploration of comet 9P/Tempel 1’s activity and coma properties prior to and after the collision of the impactor. Aims. The time series of spectra take with the Spitzer Infrared Spectrograph (IRS) show fluorescence emission of the H2O ν2 band at 6.4 μm superimposed on the dust thermal continuum. These data provide constraints on the properties of the dust ejecta cloud (dust size distribution, velocity, and mass), as well as on the water component (origin and mass). Our goal is to determine the dust-to-ice ratio of the material ejected from the impact site. -
Early Observations of the Interstellar Comet 2I/Borisov
geosciences Article Early Observations of the Interstellar Comet 2I/Borisov Chien-Hsiu Lee NSF’s National Optical-Infrared Astronomy Research Laboratory, Tucson, AZ 85719, USA; [email protected]; Tel.: +1-520-318-8368 Received: 26 November 2019; Accepted: 11 December 2019; Published: 17 December 2019 Abstract: 2I/Borisov is the second ever interstellar object (ISO). It is very different from the first ISO ’Oumuamua by showing cometary activities, and hence provides a unique opportunity to study comets that are formed around other stars. Here we present early imaging and spectroscopic follow-ups to study its properties, which reveal an (up to) 5.9 km comet with an extended coma and a short tail. Our spectroscopic data do not reveal any emission lines between 4000–9000 Angstrom; nevertheless, we are able to put an upper limit on the flux of the C2 emission line, suggesting modest cometary activities at early epochs. These properties are similar to comets in the solar system, and suggest that 2I/Borisov—while from another star—is not too different from its solar siblings. Keywords: comets: general; comets: individual (2I/Borisov); solar system: formation 1. Introduction 2I/Borisov was first seen by Gennady Borisov on 30 August 2019. As more observations were conducted in the next few days, there was growing evidence that this might be an interstellar object (ISO), especially its large orbital eccentricity. However, the first astrometric measurements do not have enough timespan and are not of same quality, hence the high eccentricity is yet to be confirmed. This had all changed by 11 September; where more than 100 astrometric measurements over 12 days, Ref [1] pinned down the orbit elements of 2I/Borisov, with an eccentricity of 3.15 ± 0.13, hence confirming the interstellar nature. -
Make a Comet Materials: Students Should First Line Their Mixing Bowls with Trash Bags
Build Your Own Comet Prep Time: 30 minutes Grades: 6-8 Lesson Time: 55 minutes Essential Questions: • What is a comet composed of? • What gives a comet its tail? • What makes a comet different from other Near-Earth Objects (NEOs)? Objectives: • Create a physical representation of a comet and its properties. • Observe distinguishable factors between comets and other NEOs. Standards: • MS – PS1-4: Develop a model that predicts and describes changes in particle motion, temperature, and state of a pure substance when thermal energy is added or removed. • CCSS.ELA-LITERACY.RST.6-8.3 - Follow precisely a multistep procedure when carrying out experiments, taking measurements, or performing technical tasks. Teacher Prep: • Materials per comet: o 5 lbs. dry ice, ice chest, paper cups, towels, small container (for scooping), wooden or plastic mixing spoon, trash bag, mixing bowl, heavy work gloves, 1 tablespoon or less of starch, 1 tablespoon or less of dark corn syrup (or soda), 1 tablespoon or less of vinegar, 1 tablespoon or less of rubbing alcohol, large beaker, water, 1 c dirt/sand, 1 L of water. • Additional materials: o Hammer or mallet, paper cups, towels, flashlight, hair dryer. • Most of the dry ice needs to be in a fine powder before the students arrive, so use the hammer to do this ahead of time. There should be about 50-60% fine powder in order to hold the comet together. It is best to separate the dry ice ahead of time with towels. • This can also be done as a class demonstration. Teacher Notes/Background: • This lesson was adapted from NASA’s Make Your Own Comet activity. -
Initial Characterization of Interstellar Comet 2I/Borisov
Initial characterization of interstellar comet 2I/Borisov Piotr Guzik1*, Michał Drahus1*, Krzysztof Rusek2, Wacław Waniak1, Giacomo Cannizzaro3,4, Inés Pastor-Marazuela5,6 1 Astronomical Observatory, Jagiellonian University, Kraków, Poland 2 AGH University of Science and Technology, Kraków, Poland 3 SRON, Netherlands Institute for Space Research, Utrecht, the Netherlands 4 Department of Astrophysics/IMAPP, Radboud University, Nijmegen, the Netherlands 5 Anton Pannekoek Institute for Astronomy, University of Amsterdam, Amsterdam, the Netherlands 6 ASTRON, Netherlands Institute for Radio Astronomy, Dwingeloo, the Netherlands * These authors contributed equally to this work; email: [email protected], [email protected] Interstellar comets penetrating through the Solar System had been anticipated for decades1,2. The discovery of asteroidal-looking ‘Oumuamua3,4 was thus a huge surprise and a puzzle. Furthermore, the physical properties of the ‘first scout’ turned out to be impossible to reconcile with Solar System objects4–6, challenging our view of interstellar minor bodies7,8. Here, we report the identification and early characterization of a new interstellar object, which has an evidently cometary appearance. The body was discovered by Gennady Borisov on 30 August 2019 UT and subsequently identified as hyperbolic by our data mining code in publicly available astrometric data. The initial orbital solution implies a very high hyperbolic excess speed of ~32 km s−1, consistent with ‘Oumuamua9 and theoretical predictions2,7. Images taken on 10 and 13 September 2019 UT with the William Herschel Telescope and Gemini North Telescope show an extended coma and a faint, broad tail. We measure a slightly reddish colour with a g′–r′ colour index of 0.66 ± 0.01 mag, compatible with Solar System comets. -
Isotopic Ratios in Outbursting Comet C/2015 ER61
Astronomy & Astrophysics manuscript no. draft_Dec_07 c ESO 2018 September 10, 2018 Isotopic ratios in outbursting comet C/2015 ER61 Bin Yang1; 2, Damien Hutsemékers3, Yoshiharu Shinnaka4, Cyrielle Opitom1, Jean Manfroid3, Emmanuël Jehin3, Karen J. Meech5, Olivier R. Hainaut1, Jacqueline V. Keane5, and Michaël Gillon3 (Affiliations can be found after the references) September 10, 2018 ABSTRACT Isotopic ratios in comets are critical to understanding the origin of cometary material and the physical and chemical conditions in the early solar nebula. Comet C/2015 ER61 (PANSTARRS) underwent an outburst with a total brightness increase of 2 magnitudes on the night of 2017 April 4. The sharp increase in brightness offered a rare opportunity to measure the isotopic ratios of the light elements in the coma of this comet. We obtained two high-resolution spectra of C/2015 ER61 with UVES/VLT on the nights of 2017 April 13 and 17. At the time of our observations, the comet was fading gradually following the outburst. We measured the nitrogen and carbon isotopic ratios from the CN violet (0,0) band and found that 12C/13C=100 ± 15, 14N/15N=130 ± 15. 14 15 14 15 In addition, we determined the N/ N ratio from four pairs of NH2 isotopolog lines and measured N/ N=140 ± 28. The measured isotopic ratios of C/2015 ER61 do not deviate significantly from those of other comets. Key words. comets: general - comets: individual (C/2015 ER61) - methods: observational 1. Introduction Understanding how planetary systems form from proto- planetary disks remains one of the great challenges in as- tronomy. -
Detection of Exocometary CO Within the 440 Myr Old Fomalhaut Belt: a Similar CO+CO2 Ice Abundance in Exocomets and Solar System Comets
UCLA UCLA Previously Published Works Title Detection of Exocometary CO within the 440 Myr Old Fomalhaut Belt: A Similar CO+CO2 Ice Abundance in Exocomets and Solar System Comets Permalink https://escholarship.org/uc/item/1zf7t4qn Journal Astrophysical Journal, 842(1) ISSN 0004-637X Authors Matra, L MacGregor, MA Kalas, P et al. Publication Date 2017-06-10 DOI 10.3847/1538-4357/aa71b4 Peer reviewed eScholarship.org Powered by the California Digital Library University of California The Astrophysical Journal, 842:9 (15pp), 2017 June 10 https://doi.org/10.3847/1538-4357/aa71b4 © 2017. The American Astronomical Society. All rights reserved. Detection of Exocometary CO within the 440 Myr Old Fomalhaut Belt: A Similar CO+CO2 Ice Abundance in Exocomets and Solar System Comets L. Matrà1, M. A. MacGregor2, P. Kalas3,4, M. C. Wyatt1, G. M. Kennedy1, D. J. Wilner2, G. Duchene3,5, A. M. Hughes6, M. Pan7, A. Shannon1,8,9, M. Clampin10, M. P. Fitzgerald11, J. R. Graham3, W. S. Holland12, O. Panić13, and K. Y. L. Su14 1 Institute of Astronomy, University of Cambridge, Madingley Road, Cambridge CB3 0HA, UK; [email protected] 2 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA 3 Astronomy Department, University of California, Berkeley CA 94720-3411, USA 4 SETI Institute, Mountain View, CA 94043, USA 5 Univ. Grenoble Alpes/CNRS, IPAG, F-38000 Grenoble, France 6 Department of Astronomy, Van Vleck Observatory, Wesleyan University, 96 Foss Hill Dr., Middletown, CT 06459, USA 7 MIT Department of Earth, Atmospheric, and -
Cliff Collapses on Comet 67P/Churyumov-Gerasimenko Following Outbursts As Observed by the Rosetta Mission
EPSC Abstracts Vol. 13, EPSC-DPS2019-1727-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. Cliff Collapses on Comet 67P/Churyumov-Gerasimenko Following Outbursts as Observed by the Rosetta Mission 1 1 M.R. El-Maarry , G. Driver (1) Birkbeck, University of London, WC12 7HX, London, UK ([email protected]) Abstract region. Indeed, a cliff collapse in the so-called Aswan area in the northern hemisphere reported in [3] We are undergoing an intensive search for surface and [4] suggests that it was associated with an changes on comet 67P/Churyumov-Gerasimenko outburst or a dust plume event. We are investigating making use of the wealth of data that was collected the source regions of outbursts that were reported in by the Rosetta mission over more than two years, [2] to look for surface changes that may have which could help constrain the processes that drive occurred as a result of these outbursts so we can surface evolution in comets on a seasonal, and better understand their mechanism, effect on surface possibly longer term, scales. Focusing on regions that evolution, and any potential controls the source have been subjected to strong outbursts gives us the region morphology may have on the morphology or highest chance of detecting surface changes and scale of the outbursts themselves. We focus here on better understanding the effect of sublimation-driven an outburst that occurred in mid September 2015 outgassing on cometary surfaces. Here, we focus on (Figure 1), roughly one month following perihelion. the detection of a previously unobserved cliff collapse event near the sharp boundary of the comet’s northern and southern hemispheres in the small lobe. -
Activities and Origins of Interstellar Comet 2I/Borisov
EPSC Abstracts Vol. 14, EPSC2020-993, 2020, updated on 28 Sep 2021 https://doi.org/10.5194/epsc2020-993 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Activities and origins of interstellar comet 2I/Borisov Ze-Xi Xing1,2, Dennis Bodewits2, John W. Noonan3, Paul D. Feldman4, Michele T. Bannister5, Davide Farnocchia6, Walt M. Harris7, Jian-Yang Li8, Kathleen E. Mandt9, and Joel Wm. Parker10 1The University of Hong Kong, Laboratory for Space Research, Department of Physics, Hong Kong, Hong Kong ([email protected]) 2Department of Physics, Leach Science Center, Auburn University, Auburn, AL, USA ([email protected]) 3Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ, USA ([email protected]) 4Department of Physics and Astronomy, Johns Hopkins University, Baltimore, MD, USA ([email protected]) 5School of Physical and Chemical Sciences—Te Kura Matū, University of Canterbury, Christchurch, New Zealand ([email protected]) 6Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA ([email protected]) 7Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ, USA ([email protected]) 8Planetary Science Institute, Tucson, AZ, USA ([email protected]) 9Space Exploration Sector, Johns Hopkins Applied Physics Laboratory, Laurel, MD, USA ([email protected]) 10Department of Space Studies, Southwest Research Institute, Boulder, CO, USA ([email protected]) We will present the results of coordinated observations of 2I/Borisov with the Neil Gehrels-Swift observatory (Swift) and Hubble Space Telescope (HST), which allowed us to provide the first glimpse into the ice content and chemical composition of the protoplanetary disk of another star. -
Make a Comet on a Stick Activity
UAMN Virtual Junior Curators: Solar System Make a Comet on a Stick! Make your own comet that can fly around the room! Comets are chunks of ice, rock, and gas that orbit the Sun. When they get close to the sun, they heat up, forming a glowing tail. Materials Needed: Wooden stick (a chopstick or popsicle stick works well), aluminum foil, ribbons, scissors. Instructions: Step 1: Cut five pieces of ribbon: two long pieces (about 3 feet or 91 cm long), two medium pieces, and one short piece. Tie your ribbons around the end of your wooden stick. Step 2: Cut three square pieces of aluminum foil. Hold the ribbon pieces off to one side and gather the foil around the end of the stick, where the ribbon is tied. Step 3: Form the foil into a ball while holding the ribbon tail off to the side. Step 4: Repeat with two more sheets of foil. If you want a bigger comet, add more foil! Step 5: Take your comet on a stick and fly it around the room! Left: Example comet on a stick. Right: Comet ISON in 2013. Image: NASA/MSFC/Aaron Kingery. A ctivity and images from NASA SpacePlace: spaceplace.nasa.gov/comet-stick/en/ UAMN Virtual Junior Curators: Solar System All About Comets Comets are balls of frozen gases, rock and dust that orbit the Sun. When a comet's orbit brings it close to the Sun, it heats up and spews dust and gases, forming a tail that stretches away from the Sun for millions of miles. -
Characterization of the Physical Properties of the ROSETTA Target Comet 67P/Churyumov-Gerasimenko
Characterization of the physical properties of the ROSETTA target comet 67P/Churyumov-Gerasimenko Von der Fakultät für Elektrotechnik, Informationstechnik, Physik der Technischen Universität Carolo-Wilhelmina zu Braunschweig zur Erlangung des Grades einer Doktorin der Naturwissenschaften (Dr.rer.nat.) genehmigte Dissertation von Cecilia Tubiana aus Moncalieri/Italien Bibliografische Information Der Deutschen Bibliothek Die Deutsche Bibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.ddb.de abrufbar. 1. Referentin oder Referent: Prof. Dr. Jürgen Blum 2. Referentin oder Referent: Prof. Dr. Michael A’Hearn eingereicht am: 18 August 2008 mündliche Prüfung (Disputation) am: 30 Oktober 2008 ISBN 978-3-936586-89-3 Copernicus Publications 2008 http://publications.copernicus.org c Cecilia Tubiana Printed in Germany Contents Summary 7 1 Comets: introduction 11 1.1 Physical properties of cometary nuclei . 15 1.1.1 Size and shape of a cometary nucleus . 18 1.1.2 Rotational period of a cometary nucleus . 22 1.1.3 Albedo of cometary nuclei . 24 1.1.4 Bulk density of cometary nuclei . 25 1.1.5 Colors indices and spectra of the nucleus . 25 1.2 Dust trail and neck-line . 27 2 67P/Churyumov-Gerasimenko and the ESA’s ROSETTA mission 29 2.1 Discovery and orbital evolution . 29 2.2 Nucleus properties . 30 2.3 Annual light curve . 32 2.4 Gas and dust production . 32 2.5 Coma features, trail and neck-line . 35 2.6 ESA’s ROSETTA mission . 35 2.7 Motivations of the thesis . 39 3 Observing strategy and performance of the observations of 67P/C-G 41 3.1 Observations: strategy and preparation .