Probing the Interior Structure of Venus

Total Page:16

File Type:pdf, Size:1020Kb

Probing the Interior Structure of Venus Probing the Interior Structure of Venus Report by: Keck Institute for Space Studies (KISS) Venus Seismology Study Team April 1, 2015 Authors and Study Participants Name Institution Discipline E-mail Study Co-leaders David Stevenson Caltech Planetary geophysics [email protected] James Cutts JPL Mission analysis and space technology [email protected] David Mimoun ISAE/U-Toulouse Planetary instrumentation [email protected] Study Participants Stephen Arrowsmith Los Alamos National Lab Seismology, infrasonics [email protected] Bruce Banerdt JPL Geophysics—seismology [email protected] Philip Blom Los Alamos National Lab Infrasonics—postdoc [email protected] Emily Brageot JPL Infrared systems analysis—postdoc [email protected] Quentin Brissaud ISAE/Toulouse Systems analysis [email protected] Gordon Chin GSFC Venus, submillimeter spectroscopy [email protected] Peter Gao Caltech Planetary science, graduate student [email protected] Raphael Garcia ISAE/Toulouse Remote sensing of Venus seismic [email protected] events Jeffery Hall JPL Venus balloons, extreme environment [email protected] Gary Hunter NASA Glenn High-temperature sensors [email protected] Jennifer Jackson Caltech Geophysics, mineral physics [email protected] Viktor Kerzhanovich JPL (retired), former IKI Venus science, Venera missions [email protected] Walter Kiefer Lunar and Planetary Geophysics, planetary seismology [email protected] Institute Attila Komjathy JPL GPS sounding of Earth’s ionosphere [email protected] Christopher Lee Ashima Research Venus atmospheric science [email protected] Philippe Lognonné IPGP Univ, Paris Diderot Planetary geophysics [email protected] Ralph Lorenz APL Planetary science, Venus seismology [email protected] Walid Majid JPL Radio astronomy, planetary science [email protected] Mohammed Mojarradi JPL High-temperature electronics [email protected] Guust Nolet University of Nice Seismology, hydroacoustics [email protected] Joseph O’Rourke Caltech Planetary science—graduate student [email protected] Lucie Rolland Los Alamos National Lab Ionosphere seismology [email protected] Gerald Shubert UCLA Geophysics, interiors and atmospheres [email protected] Mark Simons Caltech Geophysics [email protected] Christophe Sotin JPL Venus thermal and tectonic history [email protected] Tom Spilker Consultant Planetary mission design, seismology [email protected] Victor Tsai Caltech Geophysics—seismology [email protected] Acknowledgments We would like to thank members of the study team for their contributions to this report during the initial teleconferences, at the workshop itself, and in the preparation of the report. Without the diverse talents and enthusiasm of our study team, this report never could have happened. On behalf of members of the study team, we would like to thank Michelle Judd, Managing Director of the Keck Institute for Space Studies, for her role in creating the collaborative environment that was so vital to the success of our study. We would also like to thank Prof. Tom Prince, Director of the Keck Institute for Space Studies, for his guidance and the KISS Steering Committee for the confidence they placed in our team by selecting our study for funding. In the preparation of this report, we would like to acknowledge Samantha Ozyildirim of JPL for her thorough review and editing and layout of the report. Corby Waste, also of JPL, was responsible for creating the cover art. Dr. Suzanne Smrekar provided insightful comments. We acknowledge NASA’s Jet Propulsion Laboratory and the California Institute of Technology for their support of the study and for making it possible for key study participants to be involved. Finally, we would like to thank the W.M. Keck Foundation for their foresight in establishing the Keck Institute for Space Studies and the new facilities, which were so conducive to the workshop process. James A. Cutts David Mimoun David J. Stevenson Co-leads of the KISS study on Venus Seismology Table of Contents Executive Summary ....................................................................................................................................................... 1 1 Introduction ............................................................................................................................................................. 4 2 Science ................................................................................................................................................................... 5 2.1 Venus—its Atmosphere, Surface, and Interior ............................................................................................. 5 2.2 The Importance of Venus ............................................................................................................................. 7 2.3 The Scientific Case for Venus Seismology .................................................................................................. 8 3 Seismic Sources on Venus ..................................................................................................................................... 9 3.1 Venus Quakes .............................................................................................................................................. 9 3.1.1 Active Faulting ................................................................................................................................. 9 3.1.2 Seismic or Aseismic Strain Relief .................................................................................................. 10 3.1.3 Estimates of Seismic Activity ......................................................................................................... 10 3.2 Volcanic Activity ......................................................................................................................................... 11 3.3 Impacting Bolides ....................................................................................................................................... 11 3.4 Atmospheric Sources ................................................................................................................................. 11 3.5 Artificial Sources ........................................................................................................................................ 12 3.5.1 Airburst vs. Ground Source ........................................................................................................... 12 3.5.2 Chemical vs. Phase Change Explosive Sources ........................................................................... 13 3.5.3 Discussion ..................................................................................................................................... 13 4 Seismology Techniques ........................................................................................................................................ 14 4.1 Historical Perspective ................................................................................................................................. 14 4.2 Seismology Basics ..................................................................................................................................... 15 4.2.1 Classical Seismology ..................................................................................................................... 15 4.2.2 Propagation of the Seismic Waves in the Atmosphere .................................................................. 16 4.2.3 A ‘Generalized’ Seismology Approach........................................................................................... 18 4.3 Surface, Middle Atmosphere, and Space Vantage Points.......................................................................... 19 5 Seismology on the Venus Surface ........................................................................................................................ 20 5.1 Prior Planetary Surface Seismic Experiments ............................................................................................ 20 5.1.1 Lunar—Apollo Lunar Seismic Experiments ................................................................................... 20 5.1.2 Mars—Viking 1 and 2 .................................................................................................................... 20 5.1.3 Venus—Venera 13 and 14 ............................................................................................................ 21 5.1.4 Mars—InSight Seismic Interior Structure Experiment .................................................................... 22 5.2 Key Constraints for a Seismic Experiment on the Surface of Venus .......................................................... 23 5.3 Performance Requirements ....................................................................................................................... 23 5.4 Seismic Backgrounds on the Venus Surface ............................................................................................. 24 5.4.1 Natural Environment ...................................................................................................................... 25 5.4.2 Spacecraft (Anthropogenic) Effects ............................................................................................... 25 5.5 Technology Status ....................................................................................................................................
Recommended publications
  • Astronomy 330 HW 2 Presentations Outline
    Astronomy 330 HW 2 •! Stanley Swat This class (Lecture 12): http://www.ufohowto.com/ Life in the Solar System •! Lucas Guthrie Next Class: http://www.crystalinks.com/abduction.html Life in the Solar System HW 5 is due Wednesday Music: We Are All Made of Stars– Moby Presentations Outline •! Daniel Borup •! Life on Venus? Futurama •! Life on Mars? Life in the Solar System? Earth – Venus comparison •! We want to examine in more detail the backyard of humans. •! What we find may change our estimates of ne. Radius 0.95 Earth Surface gravity 0.91 Earth Venus is the hottest Mass 0.81 Earth planet, the closest in Distance from Sun 0.72 AU size to Earth, the closest Average Temp 475 C in distance to Earth, and Year 224.7 Earth days the planet with the Length of Day 116.8 Earth days longest day. Atmosphere 96% CO2 What We Used to Think Turns Out that Venus is Hell Venus must be hotter, as it is closer the Sun, but the cloud •! The surface is hot enough to melt lead cover must reflect back a large amount of the heat. •! There is a runaway greenhouse effect •! There is almost no water In 1918, a Swedish chemist and Nobel laureate concluded: •! There is sulfuric acid rain •! Everything on Venus is dripping wet. •! Most of the surface is no doubt covered with swamps. •! Not a place to visit for Spring Break. •! The constantly uniform climatic conditions result in an entire absence of adaptation to changing exterior conditions. •! Only low forms of life are therefore represented, mostly no doubt, belonging to the vegetable kingdom; and the organisms are nearly of the same kind all over the planet.
    [Show full text]
  • Selection of the Insight Landing Site M. Golombek1, D. Kipp1, N
    Manuscript Click here to download Manuscript InSight Landing Site Paper v9 Rev.docx Click here to view linked References Selection of the InSight Landing Site M. Golombek1, D. Kipp1, N. Warner1,2, I. J. Daubar1, R. Fergason3, R. Kirk3, R. Beyer4, A. Huertas1, S. Piqueux1, N. E. Putzig5, B. A. Campbell6, G. A. Morgan6, C. Charalambous7, W. T. Pike7, K. Gwinner8, F. Calef1, D. Kass1, M. Mischna1, J. Ashley1, C. Bloom1,9, N. Wigton1,10, T. Hare3, C. Schwartz1, H. Gengl1, L. Redmond1,11, M. Trautman1,12, J. Sweeney2, C. Grima11, I. B. Smith5, E. Sklyanskiy1, M. Lisano1, J. Benardino1, S. Smrekar1, P. Lognonné13, W. B. Banerdt1 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109 2State University of New York at Geneseo, Department of Geological Sciences, 1 College Circle, Geneseo, NY 14454 3Astrogeology Science Center, U.S. Geological Survey, 2255 N. Gemini Dr., Flagstaff, AZ 86001 4Sagan Center at the SETI Institute and NASA Ames Research Center, Moffett Field, CA 94035 5Southwest Research Institute, Boulder, CO 80302; Now at Planetary Science Institute, Lakewood, CO 80401 6Smithsonian Institution, NASM CEPS, 6th at Independence SW, Washington, DC, 20560 7Department of Electrical and Electronic Engineering, Imperial College, South Kensington Campus, London 8German Aerospace Center (DLR), Institute of Planetary Research, 12489 Berlin, Germany 9Occidental College, Los Angeles, CA; Now at Central Washington University, Ellensburg, WA 98926 10Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996 11Institute for Geophysics, University of Texas, Austin, TX 78712 12MS GIS Program, University of Redlands, 1200 E. Colton Ave., Redlands, CA 92373-0999 13Institut Physique du Globe de Paris, Paris Cité, Université Paris Sorbonne, France Diderot Submitted to Space Science Reviews, Special InSight Issue v.
    [Show full text]
  • Mechanisms for Space Applications
    Mechanisms for space applications M. Meftah a,* , A. Irbah a, R. Le Letty b, M. Barr´ ec, S. Pasquarella d, M. Bokaie e, A. Bataille b, and G. Poiet a a CNRS/INSU, LATMOS-IPSL, Universit´ e Versailles St-Quentin, Guyancourt, France b Cedrat Technologies SA, 15 Ch. de Malacher, 38246 Meylan, France c Thales Avionics Electrical Motors, 78700 Conflans Sainte-Honorine, France d Vincent Associates, 803 Linden Ave., Rochester, NY 14625,United States e TiNi Aerospace, 2505 Kerner Blvd., San Rafael, CA 94901, United States ABSTRACT All space instruments contain mechanisms or moving mechanical assemblies that must move (sliding, rolling, rotating, or spinning) and their successful operati on is usually mission-critical. Generally, mechanisms are not redundant and therefore represent potential single point failure modes. Several space missions have suered anomalies or failures due to problems in applying space mechanisms technology. Mechanisms require a specific qualification through a dedicated test campaign. This paper covers the design, development, testing, production, and in-flight experience of the PICARD/SODISM mechanisms. PICARD is a space mission dedicated to the study of the Sun. The PICARD Satellite was successfully launched, on June 15, 2010 on a DNEPR launcher from Dombarovskiy Cosmodrome, near Yasny (Russia). SODISM (SOlar Diameter Imager and Surface Mapper) is a 11 cm Ritchey-Chretien imaging telescope, taking solar images at five wavelengths. SODISM uses several mechanisms (a system to unlock the door at the entrance of the instrument, a system to open/closed the door using a stepper motor, two filters wheels usingastepper motor, and a mechanical shutter). For the fine pointing, SODISM uses three piezoelectric devices acting on th e primary mirror of the telescope.
    [Show full text]
  • LCROSS (Lunar Crater Observation and Sensing Satellite) Observation Campaign: Strategies, Implementation, and Lessons Learned
    Space Sci Rev DOI 10.1007/s11214-011-9759-y LCROSS (Lunar Crater Observation and Sensing Satellite) Observation Campaign: Strategies, Implementation, and Lessons Learned Jennifer L. Heldmann · Anthony Colaprete · Diane H. Wooden · Robert F. Ackermann · David D. Acton · Peter R. Backus · Vanessa Bailey · Jesse G. Ball · William C. Barott · Samantha K. Blair · Marc W. Buie · Shawn Callahan · Nancy J. Chanover · Young-Jun Choi · Al Conrad · Dolores M. Coulson · Kirk B. Crawford · Russell DeHart · Imke de Pater · Michael Disanti · James R. Forster · Reiko Furusho · Tetsuharu Fuse · Tom Geballe · J. Duane Gibson · David Goldstein · Stephen A. Gregory · David J. Gutierrez · Ryan T. Hamilton · Taiga Hamura · David E. Harker · Gerry R. Harp · Junichi Haruyama · Morag Hastie · Yutaka Hayano · Phillip Hinz · Peng K. Hong · Steven P. James · Toshihiko Kadono · Hideyo Kawakita · Michael S. Kelley · Daryl L. Kim · Kosuke Kurosawa · Duk-Hang Lee · Michael Long · Paul G. Lucey · Keith Marach · Anthony C. Matulonis · Richard M. McDermid · Russet McMillan · Charles Miller · Hong-Kyu Moon · Ryosuke Nakamura · Hirotomo Noda · Natsuko Okamura · Lawrence Ong · Dallan Porter · Jeffery J. Puschell · John T. Rayner · J. Jedadiah Rembold · Katherine C. Roth · Richard J. Rudy · Ray W. Russell · Eileen V. Ryan · William H. Ryan · Tomohiko Sekiguchi · Yasuhito Sekine · Mark A. Skinner · Mitsuru Sôma · Andrew W. Stephens · Alex Storrs · Robert M. Suggs · Seiji Sugita · Eon-Chang Sung · Naruhisa Takatoh · Jill C. Tarter · Scott M. Taylor · Hiroshi Terada · Chadwick J. Trujillo · Vidhya Vaitheeswaran · Faith Vilas · Brian D. Walls · Jun-ihi Watanabe · William J. Welch · Charles E. Woodward · Hong-Suh Yim · Eliot F. Young Received: 9 October 2010 / Accepted: 8 February 2011 © The Author(s) 2011.
    [Show full text]
  • Glossary Glossary
    Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts.
    [Show full text]
  • Solar Radius Determined from PICARD/SODISM Observations and Extremely Weak Wavelength Dependence in the Visible and the Near-Infrared
    A&A 616, A64 (2018) https://doi.org/10.1051/0004-6361/201832159 Astronomy c ESO 2018 & Astrophysics Solar radius determined from PICARD/SODISM observations and extremely weak wavelength dependence in the visible and the near-infrared M. Meftah1, T. Corbard2, A. Hauchecorne1, F. Morand2, R. Ikhlef2, B. Chauvineau2, C. Renaud2, A. Sarkissian1, and L. Damé1 1 Université Paris Saclay, Sorbonne Université, UVSQ, CNRS, LATMOS, 11 Boulevard d’Alembert, 78280 Guyancourt, France e-mail: [email protected] 2 Université de la Côte d’Azur, Observatoire de la Côte d’Azur (OCA), CNRS, Boulevard de l’Observatoire, 06304 Nice, France Received 23 October 2017 / Accepted 9 May 2018 ABSTRACT Context. In 2015, the International Astronomical Union (IAU) passed Resolution B3, which defined a set of nominal conversion constants for stellar and planetary astronomy. Resolution B3 defined a new value of the nominal solar radius (RN = 695 700 km) that is different from the canonical value used until now (695 990 km). The nominal solar radius is consistent with helioseismic estimates. Recent results obtained from ground-based instruments, balloon flights, or space-based instruments highlight solar radius values that are significantly different. These results are related to the direct measurements of the photospheric solar radius, which are mainly based on the inflection point position methods. The discrepancy between the seismic radius and the photospheric solar radius can be explained by the difference between the height at disk center and the inflection point of the intensity profile on the solar limb. At 535.7 nm (photosphere), there may be a difference of 330 km between the two definitions of the solar radius.
    [Show full text]
  • CRATER MORPHOMETRY on VENUS. C. G. Cochrane, Imperial College, London ([email protected])
    Lunar and Planetary Science XXXIV (2003) 1173.pdf CRATER MORPHOMETRY ON VENUS. C. G. Cochrane, Imperial College, London ([email protected]). Introduction: Most impact craters on Venus are propagating east and north/south. Can be minimised if pristine, and provide probably the best available ana- framelets have good texture on the left-hand side. logs for craters on Earth soon after impact; hence the Prominence extension – features extend down value of measuring their 3-D shape to known accuracy. range into a ridge, eg central peak linked to the rim. The USGS list 967 craters: from the largest, Mead at Probably due to radar shadowing differences, these are 270 km diameter, to the smallest, unnamed at 1.3 km. easily recognised and avoided during analysis. Initially, research focussed on the larger craters. Araration (from Latin: Arare to plough) consists of Schaber et al [1] (11 craters >50 km) and Ivanov et al parallel furrows some 50 pixels apart, oriented north- [2] (31 craters >70 km) took crater depth from Magel- south, and at least tens of metres deep. Fig 2, a lan altimetry. Sharpton [3] (94 craters >18 km) used floor-offsets in Synthetic Aperture Radar (SAR) F- MIDR pairs, as did Herrick & Phillips [4]. They list many parameters but not depth for 891 craters. The LPI database1 now numbers 941. Herrick & Sharpton [5] made Digital Elevation Models (DEMs) of all cra- ters at least partially imaged twice down to 12 km, and 20 smaller craters down to 3.6 km. Using FMAP im- ages and the Magellan Stereo Toolkit (MST) v.1, they automated matches every 900m but then manually ed- ited the resultant data.
    [Show full text]
  • Production and Saturation of Porosity in the Lunar Highlands from Impact Cratering
    The fractured Moon: Production and saturation of porosity in the lunar highlands from impact cratering The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Soderblom, Jason M., et al. “The Fractured Moon: Production and Saturation of Porosity in the Lunar Highlands from Impact Cratering.” Geophysical Research Letters, vol. 42, no. 17, Sept. 2015, pp. 6939–44. © 2015 American Geophysical Union As Published http://dx.doi.org/10.1002/2015GL065022 Publisher American Geophysical Union (AGU) Version Final published version Citable link http://hdl.handle.net/1721.1/118615 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. PUBLICATIONS Geophysical Research Letters RESEARCH LETTER The fractured Moon: Production and saturation 10.1002/2015GL065022 of porosity in the lunar highlands Key Points: from impact cratering • The relation between impact-generated porosity and crater size is quantified Jason M. Soderblom1, Alexander J. Evans2, Brandon C. Johnson1, H. Jay Melosh3, Katarina Miljković1,4, • Impacts into highly porous targets 5 6 7 8 3 result in positive gravity anomalies Roger J. Phillips , Jeffrey C. Andrews-Hanna , Carver J. Bierson , James W. Head III , Colleen Milbury , 9 7 1 2,10 11 • The cratering record of the oldest Gregory A. Neumann , Francis Nimmo , David E. Smith , Sean C. Solomon , Michael M. Sori , lunar surfaces is preserved in the
    [Show full text]
  • Direct Fusion Drive Rocket for Asteroid Deflection
    Direct Fusion Drive Rocket for Asteroid Deflection IEPC-2013-296 Presented at the 33rd International Electric Propulsion Conference, The George Washington University, Washington, D.C., USA October 6{10, 2013 Joseph B. Mueller∗ and Yosef S. Raziny and Michael A. Paluszek z and Amanda J. Knutson x and Gary Pajer { Princeton Satellite Systems, 6 Market St, Suite 926, Plainsboro, NJ, 08536, USA Samuel A. Cohenk Plasma Physics Laboratory, 100 Stellarator Road, Princeton, NJ, 08540 and Allan H. Glasser∗∗ University of Washington, Department of Aeronautics and Astronautics, Guggenheim Hall, Seattle, WA 98195 Traditional thinking presumes that planetary defense is only achievable with years of warning, so that a mission can launch in time to deflect the asteroid. However, the danger posed by hard-to-detect small meteors was dramatically demonstrated by the 20 meter Chelyabinsk meteor that exploded over Russia in 2013 with the force of 440 kilotons of TNT. A 5-MW Direct Fusion Drive (DFD) engine allows rockets to rapidly reach threaten- ing asteroids that and deflect them using clean burning deuterium-helium-3 fuel, a compact field-reversed configuration, and heated by odd-parity rotating magnetic fields. This paper presents the latest development of the DFD rocket engine based on recent simulations and experiments as well as calculations for an asteroid deflection envelope and a mission plan to deflect an Apophis-type asteroid given just one year of warning. Armed with this new defense technology, we will finally have achieved a vital capability for ensuring our planet's safety from impact threats. ∗Senior Technical Staff, [email protected].
    [Show full text]
  • "Is There Life on Venus?" Pdf File
    Home / Space / Specials Is there life on Venus? We call them "Martians" because, in science fiction, Mars has always been the natural home of extraterrestrials. In fact, of all the planets in the solar system, Mars is the prime candidate to host life, after Earth, of course. Indeed, Mars is on the outer edge of the habitable zone, that area around the Sun that delimits the space where the temperature is low enough to ensure that the water remains in a liquid state. And where there's water, it is well known, there's probably life. Yet it's cold on Mars today, and so far, all the probes and rovers we have sent to the surface of the red planet have found no signs of life. Planet Venus At the opposite end of the habitable belt there is Venus, similar in size and "geological" characteristics to our planet – that is, like Earth, it is a rocky planet. However, unlike Earth, Venus is probably one of the most inhospitable places in the Solar System: the temperature on the ground is about 500°C, higher than that recorded on Mercury, the planet closest to the Sun, so the Sun is not directly responsible for that infernal climate. The blame lies with the very extreme greenhouse effect on Venus. We know that the greenhouse effect is due to the presence of gases that trap solar radiation and heat the atmosphere. The main greenhouse gases are carbon dioxide (CO2), methane, water vapour and nitrogen oxides. On Earth we are rightly concerned because the amount of carbon dioxide is increasing due to human activities and with the increase in CO2, temperatures are rising.
    [Show full text]
  • Investigating Mineral Stability Under Venus Conditions: a Focus on the Venus Radar Anomalies Erika Kohler University of Arkansas, Fayetteville
    University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 5-2016 Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies Erika Kohler University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/etd Part of the Geochemistry Commons, Mineral Physics Commons, and the The unS and the Solar System Commons Recommended Citation Kohler, Erika, "Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies" (2016). Theses and Dissertations. 1473. http://scholarworks.uark.edu/etd/1473 This Dissertation is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Space and Planetary Sciences by Erika Kohler University of Oklahoma Bachelors of Science in Meteorology, 2010 May 2016 University of Arkansas This dissertation is approved for recommendation to the Graduate Council. ____________________________ Dr. Claud H. Sandberg Lacy Dissertation Director Committee Co-Chair ____________________________ ___________________________ Dr. Vincent Chevrier Dr. Larry Roe Committee Co-chair Committee Member ____________________________ ___________________________ Dr. John Dixon Dr. Richard Ulrich Committee Member Committee Member Abstract Radar studies of the surface of Venus have identified regions with high radar reflectivity concentrated in the Venusian highlands: between 2.5 and 4.75 km above a planetary radius of 6051 km, though it varies with latitude.
    [Show full text]
  • Planetary Defence Activities Beyond NASA and ESA
    Planetary Defence Activities Beyond NASA and ESA Brent W. Barbee 1. Introduction The collision of a significant asteroid or comet with Earth represents a singular natural disaster for a myriad of reasons, including: its extraterrestrial origin; the fact that it is perhaps the only natural disaster that is preventable in many cases, given sufficient preparation and warning; its scope, which ranges from damaging a city to an extinction-level event; and the duality of asteroids and comets themselves---they are grave potential threats, but are also tantalising scientific clues to our ancient past and resources with which we may one day build a prosperous spacefaring future. Accordingly, the problems of developing the means to interact with asteroids and comets for purposes of defence, scientific study, exploration, and resource utilisation have grown in importance over the past several decades. Since the 1980s, more and more asteroids and comets (especially the former) have been discovered, radically changing our picture of the solar system. At the beginning of the year 1980, approximately 9,000 asteroids were known to exist. By the beginning of 2001, that number had risen to approximately 125,000 thanks to the Earth-based telescopic survey efforts of the era, particularly the emergence of modern automated telescopic search systems, pioneered by the Massachusetts Institute of Technology’s (MIT’s) LINEAR system in the mid-to-late 1990s.1 Today, in late 2019, about 840,000 asteroids have been discovered,2 with more and more being found every week, month, and year. Of those, approximately 21,400 are categorised as near-Earth asteroids (NEAs), 2,000 of which are categorised as Potentially Hazardous Asteroids (PHAs)3 and 2,749 of which are categorised as potentially accessible.4 The hazards posed to us by asteroids affect people everywhere around the world.
    [Show full text]