Summary--Jones--ASE 2019 IAU Planetary Defense Conference
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Cross-References ASTEROID IMPACT Definition and Introduction History of Impact Cratering Studies
18 ASTEROID IMPACT Tedesco, E. F., Noah, P. V., Noah, M., and Price, S. D., 2002. The identification and confirmation of impact structures on supplemental IRAS minor planet survey. The Astronomical Earth were developed: (a) crater morphology, (b) geo- 123 – Journal, , 1056 1085. physical anomalies, (c) evidence for shock metamor- Tholen, D. J., and Barucci, M. A., 1989. Asteroid taxonomy. In Binzel, R. P., Gehrels, T., and Matthews, M. S. (eds.), phism, and (d) the presence of meteorites or geochemical Asteroids II. Tucson: University of Arizona Press, pp. 298–315. evidence for traces of the meteoritic projectile – of which Yeomans, D., and Baalke, R., 2009. Near Earth Object Program. only (c) and (d) can provide confirming evidence. Remote Available from World Wide Web: http://neo.jpl.nasa.gov/ sensing, including morphological observations, as well programs. as geophysical studies, cannot provide confirming evi- dence – which requires the study of actual rock samples. Cross-references Impacts influenced the geological and biological evolu- tion of our own planet; the best known example is the link Albedo between the 200-km-diameter Chicxulub impact structure Asteroid Impact Asteroid Impact Mitigation in Mexico and the Cretaceous-Tertiary boundary. Under- Asteroid Impact Prediction standing impact structures, their formation processes, Torino Scale and their consequences should be of interest not only to Earth and planetary scientists, but also to society in general. ASTEROID IMPACT History of impact cratering studies In the geological sciences, it has only recently been recog- Christian Koeberl nized how important the process of impact cratering is on Natural History Museum, Vienna, Austria a planetary scale. -
Arxiv:2001.00125V1 [Astro-Ph.EP] 1 Jan 2020
Draft version January 3, 2020 Typeset using LATEX default style in AASTeX61 SIZE AND SHAPE CONSTRAINTS OF (486958) ARROKOTH FROM STELLAR OCCULTATIONS Marc W. Buie,1 Simon B. Porter,1 et al. 1Southwest Research Institute 1050 Walnut St., Suite 300, Boulder, CO 80302 USA To be submitted to Astronomical Journal, Version 1.1, 2019/12/30 ABSTRACT We present the results from four stellar occultations by (486958) Arrokoth, the flyby target of the New Horizons extended mission. Three of the four efforts led to positive detections of the body, and all constrained the presence of rings and other debris, finding none. Twenty-five mobile stations were deployed for 2017 June 3 and augmented by fixed telescopes. There were no positive detections from this effort. The event on 2017 July 10 was observed by SOFIA with one very short chord. Twenty-four deployed stations on 2017 July 17 resulted in five chords that clearly showed a complicated shape consistent with a contact binary with rough dimensions of 20 by 30 km for the overall outline. A visible albedo of 10% was derived from these data. Twenty-two systems were deployed for the fourth event on 2018 Aug 4 and resulted in two chords. The combination of the occultation data and the flyby results provides a significant refinement of the rotation period, now estimated to be 15.9380 ± 0.0005 hours. The occultation data also provided high-precision astrometric constraints on the position of the object that were crucial for supporting the navigation for the New Horizons flyby. This work demonstrates an effective method for obtaining detailed size and shape information and probing for rings and dust on distant Kuiper Belt objects as well as being an important source of positional data that can aid in spacecraft navigation that is particularly useful for small and distant bodies. -
Mercurian Impact Ejecta: Meteorites and Mantle
Meteoritics & Planetary Science 44, Nr 2, 285–291 (2009) Abstract available online at http://meteoritics.org Mercurian impact ejecta: Meteorites and mantle Brett GLADMAN* and Jaime COFFEY University of British Columbia, Department of Physics and Astronomy, 6244 Agricultural Road, Vancouver, British Columbia V6T 1Z1, Canada *Corresponding author. E-mail: [email protected] (Submitted 28 January 2008; revision accepted 15 October2008) Abstract–We have examined the fate of impact ejecta liberated from the surface of Mercury due to impacts by comets or asteroids, in order to study 1) meteorite transfer to Earth, and 2) reaccumulation of an expelled mantle in giant-impact scenarios seeking to explain Mercury’s large core. In the context of meteorite transfer during the last 30 Myr, we note that Mercury’s impact ejecta leave the planet’s surface much faster (on average) than other planets in the solar system because it is the only planet where impact speeds routinely range from 5 to 20 times the planet’s escape speed; this causes impact ejecta to leave its surface moving many times faster than needed to escape its gravitational pull. Thus, a large fraction of Mercurian ejecta may reach heliocentric orbit with speeds sufficiently high for Earth-crossing orbits to exist immediately after impact, resulting in larger fractions of the ejecta reaching Earth as meteorites. We calculate the delivery rate to Earth on a time scale of 30 Myr (typical of stony meteorites from the asteroid belt) and show that several percent of the high-speed ejecta reach Earth (a factor of 2–3 less than typical launches from Mars); this is one to two orders of magnitude more efficient than previous estimates. -
Abstracts of the 50Th DDA Meeting (Boulder, CO)
Abstracts of the 50th DDA Meeting (Boulder, CO) American Astronomical Society June, 2019 100 — Dynamics on Asteroids break-up event around a Lagrange point. 100.01 — Simulations of a Synthetic Eurybates 100.02 — High-Fidelity Testing of Binary Asteroid Collisional Family Formation with Applications to 1999 KW4 Timothy Holt1; David Nesvorny2; Jonathan Horner1; Alex B. Davis1; Daniel Scheeres1 Rachel King1; Brad Carter1; Leigh Brookshaw1 1 Aerospace Engineering Sciences, University of Colorado Boulder 1 Centre for Astrophysics, University of Southern Queensland (Boulder, Colorado, United States) (Longmont, Colorado, United States) 2 Southwest Research Institute (Boulder, Connecticut, United The commonly accepted formation process for asym- States) metric binary asteroids is the spin up and eventual fission of rubble pile asteroids as proposed by Walsh, Of the six recognized collisional families in the Jo- Richardson and Michel (Walsh et al., Nature 2008) vian Trojan swarms, the Eurybates family is the and Scheeres (Scheeres, Icarus 2007). In this theory largest, with over 200 recognized members. Located a rubble pile asteroid is spun up by YORP until it around the Jovian L4 Lagrange point, librations of reaches a critical spin rate and experiences a mass the members make this family an interesting study shedding event forming a close, low-eccentricity in orbital dynamics. The Jovian Trojans are thought satellite. Further work by Jacobson and Scheeres to have been captured during an early period of in- used a planar, two-ellipsoid model to analyze the stability in the Solar system. The parent body of the evolutionary pathways of such a formation event family, 3548 Eurybates is one of the targets for the from the moment the bodies initially fission (Jacob- LUCY spacecraft, and our work will provide a dy- son and Scheeres, Icarus 2011). -
Dean Cain Bettina Zimmermann
DEAN CAIN BETTINA ZIMMERMANN POST IMPACT POST IMPACT In 2012, a meteor crashes into tion plane to Europe is destroyed Siberia with the force of several by a mysterious satellite signal, thousand nuclear warheads. In controlled from the ruins of Berlin, 2015, a few survivors will travel a city that was considered dead into “the death zone”, to try and and buried – under 30 feet of ice locate a device that could give and snow – the President of the mankind new hope – or forever New United Northern Sates orders finish it… a new expedition to find and destroy the base and the satellite. In 2012, a meteor strikes Earth, Tom Parker (Dean Cain) volunteers causing earthquakes, tidal waves, to lead a group of highly trained and a dust cloud that soon covers specialists on a suicide mission most of the Northern hemisphere, to Berlin – with ground vehicles, turning it into an ice-covered no reliable intel, and zero radio “death-zone”. contact. Three years later, most of the sur- In the ruins of what was once one vivors have settled in the only hab- of the most dynamic cities in itable territories below the equa- Europe, a desperate fight ensues tor. It’s a harsh life, with little hope for the power to change every- of Earth’s climate ever reverting thing – for better or for worse… back to normal. When an expedi- POST IMPACT SNOWBLIND LLC presents a TANDEM PRODUCTIONS GMBH, UFO IPS LLC in co-production with LUCKY 7 PRODUCTIONS LLC and AMERICAN FILM CINEMA in association with RTL TELEVISION GMBH and THE TOWER LIMITED LIABILITY PARTNERSHIP Production -
The Sky This Month – Oct 11 to Nov 15, 2017 (Times in EDT & EST) by Chris Vaughan
RASC Toronto Centre – www.rascto.ca The Sky This Month – Oct 11 to Nov 15, 2017 (times in EDT & EST) by Chris Vaughan NEWS Space Exploration – Public and Private Ref. http://spaceflightnow.com/launch-schedule/ Launches Oct 11 at Approx. 6:53-8:53 pm EDT - A SpaceX Falcon 9 (re-used) rocket from Kennedy Space Center, payload SES-11/EchoStar 105 hybrid comsat. TBD - United Launch Alliance Atlas 5 rocket from Cape Canaveral Air Force Station, classified payload for U.S. National Reconnaissance Office. Oct 12 at 5:32 am EDT - Soyuz rocket from Baikonur Cosmodrome, Kazakhstan, payload 68th Progress cargo delivery to the ISS. Oct 13 at 5:27 am EDT - Eurockot Rockot from Plesetsk Cosmodrome, Russia, payload Sentinel 5 Precursor Earth obs sat for ESA (measures atmospheric air quality, ozone, pollution and aerosols). Oct 17 at 5:37 pm EDT - Minotaur-C rocket from Vandenberg Air Force Base, CA, payload six SkySat Earth obs sats and CubeSats. Oct 30 at 3:34-5:58 pm EDT - Falcon 9 rocket from Cape Canaveral, payload Koreasat 5A comsat. Nov 7 at 8:42:30 pm EST - Arianespace Vega rocket from ZLV, Kourou, French Guiana, payload MN35-13 Earth obs sat for Morocco. Nov 10 at 4:47:03-4:48:05 am EST - United Launch Alliance Delta 2 rocket from Vandenberg Air Force Base, CA, payload 1st spacecraft in NOAA’s next-gen Joint Polar Satellite Weather Sat System. Nov 10 at 8:02 am EST - Orbital ATK Antares rocket from Wallops Island, Virginia, payload 9th Cygnus cargo freighter delivery flight to the ISS. -
Post-Impact Hydrothermal Activity in Meteorite Impact Craters and Potential Opportunities for Life
Bioastronomy 2002: Life Among the Stars IAU Symposium, Vol. 213, 2004 R.P.Norris and F.H.Stootman (eds.) Post-Impact Hydrothermal Activity in Meteorite Impact Craters and Potential Opportunities for Life Christian Koeberl Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria, [email protected] Wolf Uwe Reimold Impact Cratering Research Group, School of Geosciences, University of the Witwatersrand, Johannesburg 2050, South Africa, [email protected] Abstract. Impact craters are prominent landforms on all objects with a solid surface in the solar system. The formation of an impact structure is a high-energy, high-temperature transient event which introduces large amounts of energy into a limited area. This energy can, in part, be expanded on the creation and activation of a hydrothermal system within and even outside of the crater. Depending on the crater size and geology of the target region, this hydrothermal system may persist for extended periods of time. Such impact-induced hydrothermal systems could well have provided conditions supportive of the development of life on the early Earth and it is not unreasonable to assume that similar conditions could have led to life-favoring circumstances on other planets and satellites. 1. Introduction Studies during the last few decades have convinced most workers that the planets formed by collision and hierarchical growth starting from small objects, Le., from dust to planetesimals to planets. All planets and satellites of the solar system that have solid surfaces (e.g., Mercury, Venus, Mars, the asteroids) are covered by craters. Impact cratering has been either the most important, or one of the most important processes that affected the shaping of their surfaces. -
Revisitfrom2012
A Revisit From Near-Earth Object (NEO) 2012 TC4 Eight days after its discovery, near-Earth object (NEO) 2012 TC4 approached our planet to within 95,000 km, or 25% of the Moon's distance, when it reached perigee at 05:29 UT on 12 October 2012. In this close flyby, 2012 TC4 crossed Earth's orbit travelling inbound toward perihelion on 25.0 November 2012 UT, when it was about 91% of our distance from the Sun. Even in the Earth's night sky before perigee, 2012 TC4 was difficult to observe. Its absolute magnitude H = 26.525 placed its diameter somewhere in the 7.5-30 m range, depending on its unknown surface reflectivity, making observations possible only at very close range. Upon entering Earth's daytime sky as it passed through perigee, 2012 TC4's orbit condition code (OCC) stood at 4 thanks to 281 visible light telescopic observations spanning a 7-day arc. At OCC = 4, 2012 TC4 along-track heliocentric position uncertainty would increase at rates up to 382 arc- seconds per decade.1 Predicted position precision, together with knowledge of 2012 TC4's size and shape, can be vastly improved with radar observations. Although observations were attempted with the Goldstone, California DSS-14 planetary radar in 2012, no echoes were obtained before pointing uncertainties quickly exceeded the precision required to detect 2012 TC4. As it was lost to further observations in 2012, Earth gravity perturbations to 2012 TC4 had increased the NEO's heliocentric orbit period from 1.455 years to 1.667 years. -
Roberto Furfaro(2), Eric Christensen(1), Rob Seaman(1), Frank Shelly(1)
SYNERGISTIC NEO-DEBRIS ACTIVITIES AT UNIVERSITY OF ARIZONA Vishnu Reddy(1), Roberto Furfaro(2), Eric Christensen(1), Rob Seaman(1), Frank Shelly(1) (1) Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona, USA, Email:[email protected]. (2) Department of Systems and Industrial Engineering, University of Arizona, Tucson, Arizona, USA. ABSTRACT and its neighbour, the 61-inch Kuiper telescope (V06) for deep follow-up. Our survey telescopes rely on 111 The University of Arizona (UoA) is a world leader in megapixel 10K cameras that give G96 a 5 square-degree the detection and characterization of near-Earth objects and 703 a 19 square-degree field of view. (NEOs). More than half of all known NEOs have been Catalina Sky Survey has been a dominant contributor to discovered by two surveys (Catalina Sky Survey or CSS the discovery of near Earth asteroids and comets over its and Spacewatch) based at UoA. All three known Earth more than two decades of operation. In 2018, CSS was impactors (2008 TC3, 2014 AA and 2018 LA) were the first NEO survey to discover >1000 new NEOs in a discovered by the Catalina Sky Survey prior to impact single year, including five larger than one kilometre, enabling scientists to recover samples for two of them. and more than 200 > 140 metres. Capitalizing on our nearly half century of leadership in NEO discovery and characterization, UoA has Our survey was a major contributor satisfying the embarked on a comprehensive space situational international Spaceguard Goal (1992) [4] of finding awareness program to resolve the debris problem in cis- 90% of the NEAs larger than 1-km in diameter, and has lunar space. -
Facts, Theories and Further Questions Around the Ries-Steinheim Simultaneous Impact Event: a Review
40th Lunar and Planetary Science Conference (2009) 1542.pdf FACTS, THEORIES AND FURTHER QUESTIONS AROUND THE RIES-STEINHEIM SIMULTANEOUS IMPACT EVENT: A REVIEW. K. Mihályi1, A. Gucsik2,3, J. Szabó1, Sz. Bérczi4. 1University of Debrecen, Department of Physical Geography and Geoinformatics, H-4032 Debrecen, Egyetem tér 1., Hungary, P.O. box 9., email: [email protected]; 2Max Planck Institute for Chemistry, Department of Geochemistry, D-55020 Mainz, Germany; 3Savaria University Center, University of West of Hungary, Károlyi Gáspár tér 4., H-9700, Szombathely, Hungary; 4Eötvös University, Faculty of Science, Institute of Physics, Department of Materials Physics, H-1117 Budapest, Pázmány Péter sétány 1/a, Hungary Introduction: Nördlingen-Ries impact structure event. However, Steinheim structure hasn’t such well (Germany, Bavaria) is one of the best known terrestrial preserved distal ejecta remnants, but assuming some impact structures. Steinheim meteorite crater (often kind of linking between meteorites formed Ries and called Steinheim-basin) is located ~40 km from Ries, Steinheim (as mentioned above), angle and direction of in the southwestern direction. Diameter of Ries is impact must be similar to Ries. Stöffler et al. [1] found about 24 km, Steinheim is about 3.8 km. Their age is 30-45° for ideal impact angle to produce Ries-type the same: 15.1 million years [1,2], which is a key-point tektite (moldavite) strewn-field. for these two impact forms: it is strongly suggested not Binary asteroid or broken-up asteroid? Speaking about ’some kind’ of relationship between impacting only the occurrence of simultaneous (or nearly meteorites during double-impact, there are two simultaneous) impact, but also some kind of possible ways: (1) the asteroids were formed relationship between parental meteorites of these two separately, but later the smaller became satellite- craters (because chance of simultaneous impact of two asteroid of the bigger one, captured by gravitational meteorites in such a small area, without any linking or forces. -
Michael W. Busch Updated June 27, 2019 Contact Information
Curriculum Vitae: Michael W. Busch Updated June 27, 2019 Contact Information Email: [email protected] Telephone: 1-612-269-9998 Mailing Address: SETI Institute 189 Bernardo Ave, Suite 200 Mountain View, CA 94043 USA Academic & Employment History BS Physics & Astrophysics, University of Minnesota, awarded May 2005. PhD Planetary Science, Caltech, defended April 5, 2010. JPL Planetary Science Summer School, July 2006. Hertz Foundation Graduate Fellow, September 2007 to June 2010. Postdoctoral Researcher, University of California Los Angeles, August 2010 – August 2011. Jansky Fellow, National Radio Astronomy Observatory, August 2011 – August 2014. Visiting Scholar, University of Colorado Boulder, July – August 2012. Research Scientist, SETI Institute, August 2013 – present. Current Funding Sources: NASA Near Earth Object Observations. Research Interests: • Shapes, spin states, trajectories, internal structures, and histories of asteroids. • Identifying and characterizing targets for both robotic and human spacecraft missions. • Ruling out potential future asteroid-Earth impacts. • Radio and radar astronomy techniques. Selected Recent Papers: Marshall, S.E., and 24 colleagues, including Busch, M.W., 2019. Shape modeling of potentially hazardous asteroid (85989) 1999 JD6 from radar and lightcurve data, Icarus submitted. Reddy, V., and 69 colleagues, including Busch, M.W., 2019. Near-Earth asteroid 2012 TC4 campaign: results from global planetary defense exercise, Icarus 326, 133-150. Brozović, M., and 16 colleagues, including Busch, M.W., 2018. Goldstone and Arecibo radar observations of (99942) Apophis in 2012-2013, Icarus 300, 115-128. Brozović, M., and 19 colleagues, including Busch, M.W., 2017. Goldstone radar evidence for short-axis mode non-principal axis rotation of near-Earth asteroid (214869) 2007 PA8. Icarus 286, 314-329. -
The Geology and Geophysics of Kuiper Belt Object (486958) Arrokoth
science.sciencemag.org/cgi/content/full/science.aay3999/DC1 Supplementary Materials for The geology and geophysics of Kuiper Belt object (486958) Arrokoth J. R. Spencer*, S. A. Stern, J. M Moore, H. A. Weaver, K. N. Singer, C. B Olkin, A. J. Verbiscer, W. B. McKinnon, J. Wm. Parker, R. A. Beyer, J. T. Keane, T. R. Lauer, S. B. Porter, O. L. White, B. J. Buratti, M. R. El-Maarry, C. M. Lisse, A. H. Parker, H. B. Throop, S. J. Robbins, O. M. Umurhan, R. P. Binzel, D. T. Britt, M. W. Buie, A. F. Cheng, D. P. Cruikshank, H. A. Elliott, G. R. Gladstone, W. M. Grundy, M. E. Hill, M. Horanyi, D. E. Jennings, J. J. Kavelaars, I. R. Linscott, D. J. McComas, R. L. McNutt Jr., S. Protopapa, D. C. Reuter, P. M. Schenk, M. R. Showalter, L. A. Young, A. M. Zangari, A. Y. Abedin, C. B. Beddingfield, S. D. Benecchi, E. Bernardoni, C. J. Bierson, D. Borncamp, V. J. Bray, A. L. Chaikin, R. D. Dhingra, C. Fuentes, T. Fuse, P. L Gay, S. D. J. Gwyn, D. P. Hamilton, J. D. Hofgartner, M. J. Holman, A. D. Howard, C. J. A. Howett, H. Karoji, D. E. Kaufmann, M. Kinczyk, B. H. May, M. Mountain, M. Pätzold, J. M. Petit, M. R. Piquette, I. N. Reid, H. J. Reitsema, K. D. Runyon, S. S. Sheppard, J. A. Stansberry, T. Stryk, P. Tanga, D. J. Tholen, D. E. Trilling, L. H. Wasserman *Corresponding author. Email: [email protected] Published 13 February 2020 on Science First Release DOI: 10.1126/science.aay3999 This PDF file includes: Materials and Methods Supplementary Text Figs.