Roadmap for Solar System Science November 6, 2012
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MOONLITE : the SCIENTIFIC CASE. IA Crawford1, AJ Ball2, L. Wilson3
Lunar and Planetary Science XXXIX (2008) 1069.pdf * MOONLITE : THE SCIENTIFIC CASE. I.A. Crawford1, A.J. Ball2, L. Wilson3, A. Smith4, Y. Gao5 and the UK Pene- trator Consortium6. 1School of Earth Sciences, Birkbeck College, London, WC1E 7HX, UK. 2Planetary and Space Sciences Research Institute, Open University, Milton Keynes, UK. 3Department of Environmental Science, Lancaster University, UK. 4Mullard Space Science Laboratory, University College London, UK. 5Surrey Space Centre, University of Surrey, UK.6www.mssl.ucl.ac.uk/pages/general/news/UKLPC/UKLPC.pdf. *MoonLITE is a UK-led initiative which is currently the focus of a joint UK-NASA study. (Email: [email protected]). Introduction: The principal scientific importance the lunar crust and upper mantle [4,5]. However, the of the Moon is as a recorder of geological processes deep interior of the Moon was only very loosely con- active in the early history of terrestrial planets (e.g. strained by Apollo seismology due to the geographi- planetary differentiation, magma ocean formation and cally limited coverage of the network (essentially a evolution, etc), and of the near-Earth cosmic environ- triangle between the Apollo 12/14, 15 and 16 sites), so ment throughout Solar System history [1,2]. Although the information obtained on crustal thickness and man- the Clementine and Lunar Prospector missions have in tle structure may not be globally representative. There recent years greatly added to our knowledge of the is now a pressing need for a more widely-spaced net- geochemical and mineralogical makeup of the lunar work of lunar seismic stations, including stations at surface, and these observations will soon be supple- high latitudes and on the farside. -
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. -
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. -
Moonlite: a UK-Led Mission to the Moon Downloaded from by Guest on 24 September 2021
CRAWFORD, SMITH: MOONLITE MoonLITE: A UK-led mission to the Moon Downloaded from https://academic.oup.com/astrogeo/article/49/3/3.11/218588 by guest on 24 September 2021 Ian 1: Farside view of the Moon Crawford as seen by the and Alan Clementine spacecraft. Smith Penetrators discuss the launched by the MoonLITE orbiter scientific would allow surface objectives of investigations in areas not visited by Luna, the proposed Surveyor or Apollo missions. MoonLITE mission. (NASA/JPL/USGS) hile the surface missions to during the Apollo programme (see Wiec- the Moon of the 1960s and 1970s zorek et al. 2006, for a review). Moreover, the Wachieved a great deal, scientifically recent remote-sensing missions have themselves much was also left unresolved. The recent ABSTRACT raised questions that will require new surface plethora of lunar missions (flown or proposed) measurements for their resolution, of which reflects a resurgence in interest in the Moon, not MoonLITE is a proposal for a UK-led one of the most important is the circumstantial only in its own right, but also as a recorder of mission to the Moon that will place four evidence for water ice, and by implication other the early history of the Earth–Moon system and penetrators in the lunar surface in order volatiles, within permanently shaded craters at of the interplanetary environment 1 AU from the to make geochemical and geophysical the lunar poles (Feldman et al. 1998). Sun (e.g. Spudis 1996, Crawford 2004, Jolliff measurements that are impossible from In order to make significant further progress et al. -
Neptune and Uranus: Ice Or Rock Giants? Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 378(2187)
Teanby, N. A., Irwin, P. G. J., Moses, J. I., & Helled, R. (2020). Neptune and Uranus: ice or rock giants? Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 378(2187). https://doi.org/10.1098/rsta.2019.0489 Peer reviewed version Link to published version (if available): 10.1098/rsta.2019.0489 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via The Royal Society at https://royalsocietypublishing.org/doi/10.1098/rsta.2019.0489 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Submitted to Phil. Trans. R. Soc. A - Issue Page 2 of 19 1 2 3 4 5 Neptune and Uranus: ice or 6 7 rock giants? 8 rsta.royalsocietypublishing.org 1 2 3 9 N. A. Teanby , P. G. J. Irwin , J. I. Moses 10 4 11 and R. Helled 12 1 13 Research School of Earth Sciences, University of Bristol, Wills 14 Memorial Building, Queens Road, Bristol, BS8 1RJ, UK 15 2Atmospheric, Oceanic & Planetary Physics, University Article submitted to journal 16 of Oxford, Clarendon Laboratory, Parks Road, Oxford, 17 18 OX1 3PU. UK. 3 19 Subject Areas: Space Science Institute, 4750 Walnut Street, Suite 20 Solar System, Planetary Interiors,For Review205, Boulder, Only CO 80301, USA. -
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. -
Uranus Pathfinder: Exploring the Origins and Evolution of Ice Giant Planets
EPSC Abstracts Vol. 7 EPSC2012-660 2012 European Planetary Science Congress 2012 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2012 Uranus Pathfinder: Exploring the Origins and Evolution of Ice Giant Planets C.S. Arridge (1,2) for the Uranus Pathfinder Consortium (1) Mullard Space Science Laboratory, University College London, UK, (2) The Centre for Planetary Sciences at UCL/Birkbeck, London, UK ([email protected]) Abstract In this paper we discuss this European effort to explore Uranus and outline ongoing developments of The “Ice Giants” Uranus and Neptune are a different the mission concept. class of planet compared to Jupiter and Saturn. Studying these objects is important for furthering our References understanding of the formation and evolution of the planets, and unravelling the fundamental physical [1] Arridge, C.S., et al.: Uranus Pathfinder: Exploring the and chemical processes in the Solar System. The origins and evolution of ice giant planets, Exp. Astron., doi: 10.1007/s10686-011-9251-4, 2012. importance of filling these gaps in our knowledge of the Solar System is particularly acute when trying to apply our understanding to the numerous planetary systems that have been discovered around other stars. The Uranus Pathfinder (UP) mission [1] thus represents the quintessential aspects of the objectives of the European planetary community as expressed in ESA’s Cosmic Vision 2015–2025. UP was proposed to the European Space Agency’s M3 call for medium-class missions in 2010 and proposed to be the first orbiter of an Ice Giant planet. As the most accessible Ice Giant within the M-class mission envelope Uranus was identified as the mission target. -
Annual Report
The 2008 Annual Report of the International Space Exploration Coordination Group Released March 2009 International Space Exploration Coordination Group (ISECG) – Annual Report:2008 THIS PAGE INTENTIONALLY BLANK 1 International Space Exploration Coordination Group (ISECG) – Annual Report:2008 CONTENTS Introduction …………………………………………………………………………… 4 Part 1: The Role of the ISECG 1.1 Overview …………………………………………………………………………. 6 1.2 Working Groups of the ISECG …………………………………………………… 7 1.2.1 Enhancement of Public Engagement …………………………………………… 7 1.2.2 Establishment of Relationships with Existing International Working Groups …. 7 1.2.3 The International Space Exploration Coordination Tool (INTERSECT) ……. 8 1.2.4 The Space Exploration Interface Standards Working Group (ISWG) ………….. 8 1.2.5 Mapping the Space Exploration Journey ………………………………………... 8 Part 2: Current and Near-Term Activities of ISECG Members 2.1 Low Earth Orbit (LEO) …………………………………………………………… 10 2.1.1 The International Space Station (ISS) …………………………………………… 10 2.1.2 Emerging Government Capabilities …………………………………………….. 10 2.1.3 Emerging Commercial Providers ……………………………………………….. 11 2.2 Beyond LEO – The Moon and Mars ……………………………………………….. 11 2.2.1 Moon ……………………………………………………………………………… 11 2.2.2 Mars ………………………………………………………………………………. 12 Part 3: Progress in 2008 towards Opportunities for Integrated and Collaborative Space Exploration 3.1 Robotic Network Science – The International Lunar Network ……………………… 16 3.2 Joint Development for Robotic Exploration – Mars Sample Return ………………………… 17 3.3 Collaborative -
Phd Projects at the Institute of Origins
PhD projects at the Institute of Origins. A list of possible PhD projects at the Institute of Origins appear in the following pages. If you have any questions regarding any projects please contact the individual supervisors. Also if you have other suggestions for a project please contact us as well. The chemical composition of star forming regions near and far .................................... 3 ! Modelling the solubilities of organic solids in hydrocarbon liquids: application to the geology and astrobiology of Titan. .................................................................................... 4! Modeling turbulent flows in solar quiescent prominences ...............................................5! The zoo of exo-planets..................................................................................................8! Understanding the formation of heavy negative ions at Titan and Enceladus................9! Mapping anthropogenic versus natural sources of atmospheric CO2 ............................11! Probing Large Scale Structure with High Energy Neutrinos.........................................13! Future Moon Missions and High Energy Neutrinos ......................................................15! Measuring Cosmic Particles and the Upper Atmosphere with LOFAR.........................17! Mimicking planetary environments for assessing the survivability of bacterial organisms within an artificial environmental chamber. A combined planetary atmosphere and microbiological study for exploring panspermia................................ -
Moonlite Pendine Impact Trials
Penetrators for Planetary Exploration and Science Professor Alan Smith University College London’s Mullard Space Science Laboratory [email protected] 1 Landers and Impactors NASA Viking, 600kg, 1975, $1b NASA Spirit, 174kg, 2004, $820m NASA LCROSS, 2009, $79m NASA Deep Impact, 370kg, 2005 Penetrators . Low mass projectiles (<15kg) Detachable . High impact speed Propulsion Stage ~ up to 400 ms-1 Point of . Very tough ~10-50kgee Separation Payload . Penetrate surface and Instruments imbed therein . Undertake science- PDS bases measurements (Penetrator Delivery System) . Transmit results Penetrator Penetrator delivery Spin-Down Release from Spin-up & Orbiter Decelerate Reorient Penetrator Separation Penetrator & PDS surface Impact Delivery sequence courtesy SSTL Operate from below surface Why penetrators ? Advantages: Limitations: • Simpler architecture • Low mass limits payload • Low mass options • Low cost • Impact survival limits payload • Explore multiple sites option • Natural redundancy • Limited lifetime • Direct contact with sub-regolith • Limited telemetry capacity (drill, sampling) • Protected from environment (wind, radiation) Complementary to Soft Landers for in situ studies Heritage Military Heritage in instrumented impact projectiles Numerous laboratories looking at high velocity impacts with gas guns QinetiQ 1996: Mars96 (Russia/Lavochkin), 2 off, 60-80 ms-1 impact, each 65kg incl braking system. Lost when Mars96 failed to leave Earth orbit. 1999: Deep Space-2 (NASA/JPL), 2 off, 140-210ms-1 impact, each 3.6kg with entry shell. -
Risks of Space Colonization
Risks of space colonization Marko Kovic∗ July 2020 Abstract Space colonization is humankind's best bet for long-term survival. This makes the expected moral value of space colonization immense. However, colonizing space also creates risks | risks whose potential harm could easily overshadow all the benefits of humankind's long- term future. In this article, I present a preliminary overview of some major risks of space colonization: Prioritization risks, aberration risks, and conflict risks. Each of these risk types contains risks that can create enormous disvalue; in some cases orders of magnitude more disvalue than all the potential positive value humankind could have. From a (weakly) negative, suffering-focused utilitarian view, we there- fore have the obligation to mitigate space colonization-related risks and make space colonization as safe as possible. In order to do so, we need to start working on real-world space colonization governance. Given the near total lack of progress in the domain of space gover- nance in recent decades, however, it is uncertain whether meaningful space colonization governance can be established in the near future, and before it is too late. ∗[email protected] 1 1 Introduction: The value of colonizing space Space colonization, the establishment of permanent human habitats beyond Earth, has been the object of both popular speculation and scientific inquiry for decades. The idea of space colonization has an almost poetic quality: Space is the next great frontier, the next great leap for humankind, that we hope to eventually conquer through our force of will and our ingenuity. From a more prosaic point of view, space colonization is important because it represents a long-term survival strategy for humankind1. -
The Mystery and Majesty
The mystery and majesty Nearly 40 years after THE SPACE AGE BLASTED off when the Soviet Union launched the Voyager 2 visited Uranus world’s first artificial satellite in 1957. Since then, humanity has explored our cosmic and Neptune, scientists are backyard with vigor — and yet two planets have fallen to the planetary probe wayside. eager for new expeditions. In the 63 years since Sputnik, humanity has only visited Neptune and Uranus once BY JOEL DAVIS — when Voyager 2 flew past Uranus in January 1986 and Neptune in August 1989 40 ASTRONOMY • DECEMBER 2020 of the ICE GIANTS — and even that wasn’t entirely pre- interstellar mission, more than a dozen pro- In 1781, Uranus became the first planet planned. The unmitigated success of posals have been offered for return missions ever discovered using a telescope. Nearly 200 years later, Voyager 2 Voyager 1 and 2 on their original mission to one or both ice giants. So far, none have became the first spacecraft to visit to explore Jupiter and Saturn earned the made it past the proposal stage due to lack Uranus and Neptune, in 1986 and 1989 respectively. NASA/JPL twin spacecrafts further missions in our of substantial scientific interest. Effectively, solar system and beyond, with Neptune and the planetary research community has been Uranus acting as the last stops on a Grand giving the ice giants the cold shoulder. Tour of the outer solar system. But recently, exoplanet data began In the 31 years since Voyager 2 left the revealing the abundance of icy exoplanets Neptune system in 1989 and began its in our galaxy “and new questions about WWW.ASTRONOMY.COM 41 With a rotation axis tilted more than 90 degrees compared to its orbital plane, Neptune likewise has a highly tilted rotation axis and tilted magnetic axis.