Design and Analysis of Optimal Operational Orbits Around Venus for the Envision Mission Proposal
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Art Gallery of New South Wales Annual Report 2012 – 13
ART GALLERY OF NEW SOUTH WALES ANNUAL REPORT 2012 – 13 1 CONTENTS 4 Vision and strategic direction 2010 – 15 5 President’s foreword 9 Director’s statement 13 At a glance 15 Access 15 Exhibitions and audience programs 19 Future exhibitions 21 Publishing 23 Engaging 23 Digital engagement 23 Community 30 Education 35 Outreach Regional NSW 40 Stewarding 40 Building and environmental management 42 Corporate Governance 58 Collecting 58 Major collection acquisitions 67 Other collection activity 70 Appendices 123 General Access Information 131 Financial statements 2 ART GALLERY OF NSW ANNUAL REPORT 12-13 The Hon George Souris MP Minister for Tourism, Major Events, Hospitality and Racing, and Minister for the Arts Parliament House Macquarie Street SYDNEY NSW 2000 Dear Minister It is our pleasure to forward to you for presentation to the NSW Parliament the annual report for the Art Gallery of NSW for the year ended 30 June 2013. This report has been prepared in accordance with the provisions of the Annual Report (Statutory Bodies) Act 1984 and the Annual Reports (Statutory Bodies) Regulations 2010. Yours sincerely Steven Lowy Michael Brand President Director Art Gallery of NSW Trust 21 October 2013 3 VISION AND STRATEGIC DIRECTION 2010 – 2015 Vision The Gallery is dedicated to serving the widest possible audience, both nationally and internationally, as a centre of excellence for the collection, preservation, documentation, . interpretation and display of Australian and international art. The Gallery is also dedicated to providing a forum for scholarship, art education and the exchange of ideas. Strategic Directions Access To continue to improve access to our collection, resources and expertise through exhibitions, publishing, programs, new technologies and partnerships. -
Venus Aerobot Multisonde Mission
w AIAA Balloon Technology Conference 1999 Venus Aerobot Multisonde Mission By: James A. Cutts ('), Viktor Kerzhanovich o_ j. (Bob) Balaram o), Bruce Campbell (2), Robert Gershman o), Ronald Greeley o), Jeffery L. Hall ('), Jonathan Cameron o), Kenneth Klaasen v) and David M. Hansen o) ABSTRACT requires an orbital relay system that significantly Robotic exploration of Venus presents many increases the overall mission cost. The Venus challenges because of the thick atmosphere and Aerobot Multisonde (VAMuS) Mission concept the high surface temperatures. The Venus (Fig 1 (b) provides many of the scientific Aerobot Multisonde mission concept addresses capabilities of the VGA, with existing these challenges by using a robotic balloon or technology and without requiring an orbital aerobot to deploy a number of short lifetime relay. It uses autonomous floating stations probes or sondes to acquire images of the (aerobots) to deploy multiple dropsondes capable surface. A Venus aerobot is not only a good of operating for less than an hour in the hot lower platform for precision deployment of sondes but atmosphere of Venus. The dropsondes, hereafter is very effective at recovering high rate data. This described simply as sondes, acquire high paper describes the Venus Aerobot Multisonde resolution observations of the Venus surface concept and discusses a proposal to NASA's including imaging from a sufficiently close range Discovery program using the concept for a that atmospheric obscuration is not a major Venus Exploration of Volcanoes and concern and communicate these data to the Atmosphere (VEVA). The status of the balloon floating stations from where they are relayed to deployment and inflation, balloon envelope, Earth. -
Appendix 1: Venus Missions
Appendix 1: Venus Missions Sputnik 7 (USSR) Launch 02/04/1961 First attempted Venus atmosphere craft; upper stage failed to leave Earth orbit Venera 1 (USSR) Launch 02/12/1961 First attempted flyby; contact lost en route Mariner 1 (US) Launch 07/22/1961 Attempted flyby; launch failure Sputnik 19 (USSR) Launch 08/25/1962 Attempted flyby, stranded in Earth orbit Mariner 2 (US) Launch 08/27/1962 First successful Venus flyby Sputnik 20 (USSR) Launch 09/01/1962 Attempted flyby, upper stage failure Sputnik 21 (USSR) Launch 09/12/1962 Attempted flyby, upper stage failure Cosmos 21 (USSR) Launch 11/11/1963 Possible Venera engineering test flight or attempted flyby Venera 1964A (USSR) Launch 02/19/1964 Attempted flyby, launch failure Venera 1964B (USSR) Launch 03/01/1964 Attempted flyby, launch failure Cosmos 27 (USSR) Launch 03/27/1964 Attempted flyby, upper stage failure Zond 1 (USSR) Launch 04/02/1964 Venus flyby, contact lost May 14; flyby July 14 Venera 2 (USSR) Launch 11/12/1965 Venus flyby, contact lost en route Venera 3 (USSR) Launch 11/16/1965 Venus lander, contact lost en route, first Venus impact March 1, 1966 Cosmos 96 (USSR) Launch 11/23/1965 Possible attempted landing, craft fragmented in Earth orbit Venera 1965A (USSR) Launch 11/23/1965 Flyby attempt (launch failure) Venera 4 (USSR) Launch 06/12/1967 Successful atmospheric probe, arrived at Venus 10/18/1967 Mariner 5 (US) Launch 06/14/1967 Successful flyby 10/19/1967 Cosmos 167 (USSR) Launch 06/17/1967 Attempted atmospheric probe, stranded in Earth orbit Venera 5 (USSR) Launch 01/05/1969 Returned atmospheric data for 53 min on 05/16/1969 M. -
SFSC Search Down to 4
C M Y K www.newssun.com EWS UN NHighlands County’s Hometown-S Newspaper Since 1927 Rivalry rout Deadly wreck in Polk Harris leads Lake 20-year-old woman from Lake Placid to shutout of AP Placid killed in Polk crash SPORTS, B1 PAGE A2 PAGE B14 Friday-Saturday, March 22-23, 2013 www.newssun.com Volume 94/Number 35 | 50 cents Forecast Fire destroys Partly sunny and portable at Fred pleasant High Low Wild Elementary Fire alarms “Myself, Mr. (Wally) 81 62 Cox and other administra- Complete Forecast went off at 2:40 tors were all called about PAGE A14 a.m. Wednesday 3 a.m.,” Waldron said Wednesday morning. Online By SAMANTHA GHOLAR Upon Waldron’s arrival, [email protected] the Sebring Fire SEBRING — Department along with Investigations into a fire DeSoto City Fire early Wednesday morning Department, West Sebring on the Fred Wild Volunteer Fire Department Question: Do you Elementary School cam- and Sebring Police pus are under way. Department were all on think the U.S. govern- The school’s fire alarms the scene. ment would ever News-Sun photo by KATARA SIMMONS Rhoda Ross reads to youngsters Linda Saraniti (from left), Chyanne Carroll and Camdon began going off at approx- State Fire Marshal seize money from pri- Carroll on Wednesday afternoon at the Lake Placid Public Library. Ross was reading from imately 2:40 a.m. and con- investigator Raymond vate bank accounts a children’s book she wrote and illustrated called ‘A Wildflower for all Seasons.’ tinued until about 3 a.m., Miles Davis was on the like is being consid- according to FWE scene for a large part of ered in Cyprus? Principal Laura Waldron. -
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. -
Venus in Two Acts Saidiya Hartman
Venus in Two Acts Saidiya Hartman Small Axe, Number 26 (Volume 12, Number 2), June 2008, pp. 1-14 (Article) Published by Duke University Press For additional information about this article https://muse.jhu.edu/article/241115 Access provided by University Of Maryland @ College Park (13 Mar 2017 20:04 GMT) Venus in Two Acts Saidiya Hartman ABSTR A CT : This essay examines the ubiquitous presence of Venus in the archive of Atlantic slavery and wrestles with the impossibility of discovering anything about her that hasn’t already been stated. As an emblematic figure of the enslaved woman in the Atlantic world, Venus makes plain the convergence of terror and pleasure in the libidinal economy of slavery and, as well, the intimacy of history with the scandal and excess of literature. In writing at the limit of the unspeak- able and the unknown, the essay mimes the violence of the archive and attempts to redress it by describing as fully as possible the conditions that determine the appearance of Venus and that dictate her silence. In this incarnation, she appears in the archive of slavery as a dead girl named in a legal indict- ment against a slave ship captain tried for the murder of two Negro girls. But we could have as easily encountered her in a ship’s ledger in the tally of debits; or in an overseer’s journal—“last night I laid with Dido on the ground”; or as an amorous bed-fellow with a purse so elastic “that it will contain the largest thing any gentleman can present her with” in Harris’s List of Covent- Garden Ladies; or as the paramour in the narrative of a mercenary soldier in Surinam; or as a brothel owner in a traveler’s account of the prostitutes of Barbados; or as a minor character in a nineteenth-century pornographic novel.1 Variously named Harriot, Phibba, Sara, Joanna, Rachel, Linda, and Sally, she is found everywhere in the Atlantic world. -
Determination of Venus' Interior Structure with Envision
remote sensing Technical Note Determination of Venus’ Interior Structure with EnVision Pascal Rosenblatt 1,*, Caroline Dumoulin 1 , Jean-Charles Marty 2 and Antonio Genova 3 1 Laboratoire de Planétologie et Géodynamique, UMR-CNRS6112, Université de Nantes, 44300 Nantes, France; [email protected] 2 CNES, Space Geodesy Office, 31401 Toulouse, France; [email protected] 3 Department of Mechanical and Aerospace Engineering, Sapienza University of Rome, 00184 Rome, Italy; [email protected] * Correspondence: [email protected] Abstract: The Venusian geological features are poorly gravity-resolved, and the state of the core is not well constrained, preventing an understanding of Venus’ cooling history. The EnVision candidate mission to the ESA’s Cosmic Vision Programme consists of a low-altitude orbiter to investigate geological and atmospheric processes. The gravity experiment aboard this mission aims to determine Venus’ geophysical parameters to fully characterize its internal structure. By analyzing the radio- tracking data that will be acquired through daily operations over six Venusian days (four Earth’s years), we will derive a highly accurate gravity field (spatial resolution better than ~170 km), allowing detection of lateral variations of the lithosphere and crust properties beneath most of the geological ◦ features. The expected 0.3% error on the Love number k2, 0.1 error on the tidal phase lag and 1.4% error on the moment of inertia are fundamental to constrain the core size and state as well as the mantle viscosity. Keywords: planetary interior structure; gravity field determination; deep space mission Citation: Rosenblatt, P.; Dumoulin, C.; Marty, J.-C.; Genova, A. -
18Th Meeting of the Venus Exploration Analysis Group (Vexag)
18TH MEETING OF THE VENUS EXPLORATION ANALYSIS GROUP (VEXAG) Program and Abstracts LPI Contribution No. 2356 18th Meeting of the Venus Exploration Analysis Group November 16–17, 2020 Institutional Support Lunar and Planetary Institute Universities Space Research Association Convener Noam Izenberg Johns Hopkins Applied Physics Laboratory Darby Dyar Mount Holyoke College Science Organizing Committee Darby Dyar Planetary Science Institute, Mount Holyoke College Noam Izenberg JHU Applied Physics Laboratory Megan Andsell NASA Headquarters Natasha Johnson NASA Goddard Jennifer Jackson California Institute of Technology Jim Cutts Jet Propulsion Laboratory Tommy Thompson Jet Propulsion Laboratory Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Compiled in 2020 by Meeting and Publication Services Lunar and Planetary Institute USRA Houston 3600 Bay Area Boulevard, Houston TX 77058-1113 This material is based upon work supported by NASA under Award No. 80NSSC20M0173. Any opinions, findings, and conclusions or recommendations expressed in this volume are those of the author(s) and do not necessarily reflect the views of the National Aeronautics and Space Administration. The Lunar and Planetary Institute is operated by the Universities Space Research Association under a cooperative agreement with the Science Mission Directorate of the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. ISSN No. 0161-5297 Abstracts for this meeting are available via the meeting website at https://www.hou.usra.edu/meetings/vexag2020/ Abstracts can be cited as Author A. -
A New Approach to Geophysical Real-Time Measurements on a Deep-Sea floor Using Decommissioned Submarine Cables
Earth Planets Space, 50, 913–925, 1998 A new approach to geophysical real-time measurements on a deep-sea floor using decommissioned submarine cables Junzo Kasahara1, Toshinori Sato1, Hiroyasu Momma2, and Yuichi Shirasaki3 1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi-cho, Bunkyo-ku, Tokyo 113-0032, Japan 2JAMSTEC (Japan Marine Science and Technology Center), 2-15 Natsushima, Yokosuka, Kanagawa 237-0061, Japan 3KDD R & D Laboratories, 2-1-15 Ohara, Kamifukuoka-shi, Saitama 356-0003, Japan (Received April 8, 1998; Revised October 16, 1998; Accepted October 17, 1998) In order to better understand earthquake generation, tectonics at plate boundaries, and better image the Earth’s deep structures, real-time geophysical measurements in the ocean are required. We therefore attempted to use decommissioned submarine cables, TPC-1 and TPC-2. An OBS was successfully linked to the TPC-1 on the landward slope of the Izu-Bonin Trench in 1997. The OBS detected co-seismic and gradual changes during a Mw 6.1 earthquake just below the station at 80 km depth on November 11, 1997. A pressure sensor co-registered a change equivalent to 50 cm sea-level change. This suggests a high possibility detecting silent earthquakes or earthquake precursors if they exist. A multi-disciplinary geophysical station has been developed for deep-sea floor using TPC-2 since 1995. The station comprises eight instrument sets: broadband seismometers, geodetic measurements, hydrophone array, deep- sea digital camera, CTD, etc. These activities are examples that decommissioned submarine cables can be great global resources for real-time cost-effective geophysical measurements on a deep-sea floor. -
Habitable Zone ? UE Zu Habitable Planeten Präsentation 1
Venus Habitable Zone ? UE zu Habitable Planeten Präsentation 1. Juni 2006 Eisenkölbl, Grohs, Hren, Lendl Venus 1. Raumsonden zur Venus Überblick • Raumfahrt zur Venus – Allgemeines – Beweggründe – Technische Hintergründe • Venus – Missionen – Zeittafel und Überblick – erfolgreiche Missionen – Zukünftige Missionen Raumfahrt zur Venus Allgemeines • Venus ist der meistbesuchte Planet in unserem Sonnensystem. (~ 25 erfolgreiche Missionen von 44) • Heutige Daten der Venus sind ein Ergebnis der zahlreichen Raummissionen Raumfahrt zur Venus Beweggründe • Dichte Wolkendecke – keine Beobachtungsmöglichkeit von der Erde aus im sichtbaren Licht • Vorstellung von Leben auf Venus • Suche nach habitabler Zone • Ressourcensuche Raumfahrt zur Venus technische Hintergründe • Venus ist der Planet mit der geringsten Entfernung von der Erde – Minimum 38.2 x 106 km – Maximum 261.0 x 106 km • Sonden leisten Pionierarbeit – Erprobung von Raumsonden • Technik • Material • Bauart Raumfahrt zur Venus – Zeittafel 1 (1961-1967) 1961 Sputnik 7 - 4 February 1961 - Attempted Venus Impact Venera 1 - 12 February 1961 - Venus Flyby (Contact Lost) 1962 Mariner 1 - 22 July 1962 - Attempted Venus Flyby (Launch Failure) Sputnik 19 - 25 August 1962 - Attempted Venus Flyby Mariner 2 - 27 August 1962 - Venus Flyby Sputnik 20 - 1 September 1962 - Attempted Venus Flyby Sputnik 21 - 12 September 1962 - Attempted Venus Flyby 1963 Cosmos 21 - 11 November 1963 - Attempted Venera Test Flight? 1964 Venera 1964A - 19 February 1964 - Attempted Venus Flyby (Launch Failure) Venera 1964B -
Life on Venus, and How to Explore Venus with High-Temperature Electronics Carl-Mikael Zetterling [email protected]
Life on Venus, and How to Explore Venus with High-Temperature Electronics Carl-Mikael Zetterling [email protected] www.WorkingonVenus.se Outline Life on Venus (phosphine in the clouds) Previous missions to Venus Life on Venus (photos from the ground) High temperature electronics Future missions to Venus, including Working on Venus (KTH Project 2014 - 2018) www.WorkingonVenus.se 3 Phosphine gas in the cloud decks of Venus Trace amounts of phosphine (20 ppb, PH3) seen by the ALMA and JCMT telescopes, with millimetre wave spectral detection 4 Phosphine gas in the cloud decks of Venus 5 Phosphine gas in the cloud decks of Venus https://www.nature.com/articles/s41550-020-1174-4 https://arxiv.org/pdf/2009.06499.pdf https://www.nytimes.com/2020/09/14/science/venus-life- clouds.html?smtyp=cur&smid=fb-nytimesfindings https://www.scientificamerican.com/article/is-there-life-on- venus-these-missions-could-find-it/ 6 Did NASA detect phosphine 1978? Pioneer 13 Large Probe Neutral Mass Spectrometer (LNMS) https://www.livescience.com/life-on-venus-pioneer-13.html 7 Why Venus? From Wikimedia Commons, the free media repository Our closest planet, but least known Similar to earth in size and core, has an atmosphere Volcanoes Interesting for climate modeling Venus Long-life Surface Package (ultimate limit of global warming) C. Wilson, C.-M. Zetterling, W. T. Pike IAC-17-A3.5.5, Paper 41353 arXiv:1611.03365v1 www.WorkingonVenus.se 8 Venus Atmosphere 96% CO2 (Also sulphuric acids) Pressure of 92 bar (equivalent to 1000 m water) Temperature 460 °C From Wikimedia Commons, the free media repository Difficult to explore Life is not likely www.WorkingonVenus.se 9 Previous Missions Venera 1 – 16 (1961 – 1983) USSR Mariner 2 (1962) NASA, USA Pioneer (1978 – 1992) NASA, USA Magellan (1989) NASA, USA Venus Express (2005 - ) ESA, Europa From Wikimedia Commons, the free media repository Akatsuki (2010) JAXA, Japan www.WorkingonVenus.se 10 Steps to lunar and planetary exploration: 1. -
Deep Space Chronicle Deep Space Chronicle: a Chronology of Deep Space and Planetary Probes, 1958–2000 | Asifa
dsc_cover (Converted)-1 8/6/02 10:33 AM Page 1 Deep Space Chronicle Deep Space Chronicle: A Chronology ofDeep Space and Planetary Probes, 1958–2000 |Asif A.Siddiqi National Aeronautics and Space Administration NASA SP-2002-4524 A Chronology of Deep Space and Planetary Probes 1958–2000 Asif A. Siddiqi NASA SP-2002-4524 Monographs in Aerospace History Number 24 dsc_cover (Converted)-1 8/6/02 10:33 AM Page 2 Cover photo: A montage of planetary images taken by Mariner 10, the Mars Global Surveyor Orbiter, Voyager 1, and Voyager 2, all managed by the Jet Propulsion Laboratory in Pasadena, California. Included (from top to bottom) are images of Mercury, Venus, Earth (and Moon), Mars, Jupiter, Saturn, Uranus, and Neptune. The inner planets (Mercury, Venus, Earth and its Moon, and Mars) and the outer planets (Jupiter, Saturn, Uranus, and Neptune) are roughly to scale to each other. NASA SP-2002-4524 Deep Space Chronicle A Chronology of Deep Space and Planetary Probes 1958–2000 ASIF A. SIDDIQI Monographs in Aerospace History Number 24 June 2002 National Aeronautics and Space Administration Office of External Relations NASA History Office Washington, DC 20546-0001 Library of Congress Cataloging-in-Publication Data Siddiqi, Asif A., 1966 Deep space chronicle: a chronology of deep space and planetary probes, 1958-2000 / by Asif A. Siddiqi. p.cm. – (Monographs in aerospace history; no. 24) (NASA SP; 2002-4524) Includes bibliographical references and index. 1. Space flight—History—20th century. I. Title. II. Series. III. NASA SP; 4524 TL 790.S53 2002 629.4’1’0904—dc21 2001044012 Table of Contents Foreword by Roger D.