Astronomical Instruments on the Moon: Concepts for Fully-Steerable and Survey Vlsts at a Manned Base at the Moon’S South Pole
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Craters in Shadow
Section 3: Craters in Shadow Kepler Copernicus Eratosthenes Seen it Clavius Seen it Section 3: Craters in Shadow Visibility: A pair of binoculars is the minimum requirement to see these features. When: Look for them when the terminator’s close by, typically a day before last quarter. Not all craters are best seen when the Sun is high in the lunar sky - in fact most aren’t! If craters aren’t par- ticularly bright or dark, they tend to disappear into the background when the Moon’s phase is close to full. These craters are best seen when the ‘terminator’ is nearby, or when the Sun is low in the lunar sky as seen from the crater. This causes oblique lighting to fall on the crater and create exaggerated shadows. Ultimately, this makes the crater look more dramatic and easier to see. We’ll use this effect for the next section on lunar mountains, but before we do, there are a couple of craters that we’d like to bring to your attention. Actually, the Moon is covered with a whole host of wonderful craters that look amazing when the lighting is oblique. During the summer and into the early autumn, it’s the later phases of the Moon are best positioned in the sky - the phases following full Moon. Unfortunately, this means viewing in the early hours but don’t worry as we’ve kept things simple. We just want to give you a taste of what a shadowed crater looks like for this marathon, so the going here is really pretty easy! First, locate the two craters Kepler and Copernicus which were marathon targets pointed out in Section 2. -
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. -
List of Missions Using SPICE (PDF)
1/7/20 Data Restorations Selected Past Users Current/Pending Users Examples of Possible Future Users Apollo 15, 16 [L] Magellan [L] Cassini Orbiter NASA Discovery Program Mariner 2 [L] Clementine (NRL) Mars Odyssey NASA New Frontiers Program Mariner 9 [L] Mars 96 (RSA) Mars Exploration Rover Lunar IceCube (Moorehead State) Mariner 10 [L] Mars Pathfinder Mars Reconnaissance Orbiter LunaH-Map (Arizona State) Viking Orbiters [L] NEAR Mars Science Laboratory Luna-Glob (RSA) Viking Landers [L] Deep Space 1 Juno Aditya-L1 (ISRO) Pioneer 10/11/12 [L] Galileo MAVEN Examples of Users not Requesting NAIF Help Haley armada [L] Genesis SMAP (Earth Science) GOLD (LASP, UCF) (Earth Science) [L] Phobos 2 [L] (RSA) Deep Impact OSIRIS REx Hera (ESA) Ulysses [L] Huygens Probe (ESA) [L] InSight ExoMars RSP (ESA, RSA) Voyagers [L] Stardust/NExT Mars 2020 Emmirates Mars Mission (UAE via LASP) Lunar Orbiter [L] Mars Global Surveyor Europa Clipper Hayabusa-2 (JAXA) Helios 1,2 [L] Phoenix NISAR (NASA and ISRO) Proba-3 (ESA) EPOXI Psyche Parker Solar Probe GRAIL Lucy EUMETSAT GEO satellites [L] DAWN Lunar Reconnaissance Orbiter MOM (ISRO) Messenger Mars Express (ESA) Chandrayan-2 (ISRO) Phobos Sample Return (RSA) ExoMars 2016 (ESA, RSA) Solar Orbiter (ESA) Venus Express (ESA) Akatsuki (JAXA) STEREO [L] Rosetta (ESA) Korean Pathfinder Lunar Orbiter (KARI) Spitzer Space Telescope [L] [L] = limited use Chandrayaan-1 (ISRO) New Horizons Kepler [L] [S] = special services Hayabusa (JAXA) JUICE (ESA) Hubble Space Telescope [S][L] Kaguya (JAXA) Bepicolombo (ESA, JAXA) James Webb Space Telescope [S][L] LADEE Altius (Belgian earth science satellite) ISO [S] (ESA) Armadillo (CubeSat, by UT at Austin) Last updated: 1/7/20 Smart-1 (ESA) Deep Space Network Spectrum-RG (RSA) NAIF has or had project-supplied funding to support mission operations, consultation for flight team members, and SPICE data archive preparation. -
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. -
10Great Features for Moon Watchers
Sinus Aestuum is a lava pond hemming the Imbrium debris. Mare Orientale is another of the Moon’s large impact basins, Beginning observing On its eastern edge, dark volcanic material erupted explosively and possibly the youngest. Lunar scientists think it formed 170 along a rille. Although this region at first appears featureless, million years after Mare Imbrium. And although “Mare Orien- observe it at several different lunar phases and you’ll see the tale” translates to “Eastern Sea,” in 1961, the International dark area grow more apparent as the Sun climbs higher. Astronomical Union changed the way astronomers denote great features for Occupying a region below and a bit left of the Moon’s dead lunar directions. The result is that Mare Orientale now sits on center, Mare Nubium lies far from many lunar showpiece sites. the Moon’s western limb. From Earth we never see most of it. Look for it as the dark region above magnificent Tycho Crater. When you observe the Cauchy Domes, you’ll be looking at Yet this small region, where lava plains meet highlands, con- shield volcanoes that erupted from lunar vents. The lava cooled Moon watchers tains a variety of interesting geologic features — impact craters, slowly, so it had a chance to spread and form gentle slopes. 10Our natural satellite offers plenty of targets you can spot through any size telescope. lava-flooded plains, tectonic faulting, and debris from distant In a geologic sense, our Moon is now quiet. The only events by Michael E. Bakich impacts — that are great for telescopic exploring. -
Relative Ages
CONTENTS Page Introduction ...................................................... 123 Stratigraphic nomenclature ........................................ 123 Superpositions ................................................... 125 Mare-crater relations .......................................... 125 Crater-crater relations .......................................... 127 Basin-crater relations .......................................... 127 Mapping conventions .......................................... 127 Crater dating .................................................... 129 General principles ............................................. 129 Size-frequency relations ........................................ 129 Morphology of large craters .................................... 129 Morphology of small craters, by Newell J. Fask .................. 131 D, method .................................................... 133 Summary ........................................................ 133 table 7.1). The first three of these sequences, which are older than INTRODUCTION the visible mare materials, are also dominated internally by the The goals of both terrestrial and lunar stratigraphy are to inte- deposits of basins. The fourth (youngest) sequence consists of mare grate geologic units into a stratigraphic column applicable over the and crater materials. This chapter explains the general methods of whole planet and to calibrate this column with absolute ages. The stratigraphic analysis that are employed in the next six chapters first step in reconstructing -
Astrophysics
National Aeronautics and Space Administration Astrophysics Committee on NASA Science Paul Hertz Mission Extensions Director, Astrophysics Division NRC Keck Center Science Mission Directorate Washington DC @PHertzNASA February 1-2, 2016 Why Astrophysics? Astrophysics is humankind’s scientific endeavor to understand the universe and our place in it. 1. How did our universe 2. How did galaxies, stars, 3. Are We Alone? begin and evolve? and planets come to be? These national strategic drivers are enduring 1972 1982 1991 2001 2010 2 Astrophysics Driving Documents http://science.nasa.gov/astrophysics/documents 3 Astrophysics Programs Physics of the Cosmos Cosmic Origins Exoplanet Exploration Program Program Program 1. How did our universe 2. How did galaxies, stars, 3. Are We Alone? begin and evolve? and planets come to be? Astrophysics Explorers Program Astrophysics Research Program James Webb Space Telescope Program (managed outside of Astrophysics Division until commissioning) 4 Astrophysics Programs and Missions Physics of the Cosmos Cosmic Origins Exoplanet Exploration Program Program Program Chandra Hubble Spitzer Kepler/K2 XMM-Newton (ESA) Herschel (ESA) WFIRST Fermi SOFIA Planck (ESA) LISA Pathfinder (ESA) Astrophysics Explorers Program Euclid (ESA) NuSTAR Swift Suzaku (JAXA) Athena (ESA) ASTRO-H (JAXA) NICER TESS L3 GW Obs (ESA) 3 SMEX and 2 MO in Phase A James Webb Space Telescope Program: Webb 5 Astrophysics Programs and Missions Physics of the Cosmos Cosmic Origins Exoplanet Exploration Program Program Program Missions in extended phase Chandra Hubble Spitzer Kepler/K2 XMM-Newton (ESA) Herschel (ESA) WFIRST Fermi SOFIA Planck (ESA) LISA Pathfinder (ESA) Astrophysics Explorers Program Euclid (ESA) NuSTAR Swift Suzaku (JAXA) Athena (ESA) ASTRO-H (JAXA) NICER TESS L3 GW Obs (ESA) 3 SMEX and 2 MO in Phase A James Webb Space Telescope Program: Webb 6 Astrophysics Mission Portfolio • NASA Astrophysics seeks to advance NASA’s strategic objectives in astrophysics as well as the science priorities of the Decadal Survey in Astronomy and Astrophysics. -
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 -
Issue #1 – 2012 October
TTSIQ #1 page 1 OCTOBER 2012 Introducing a new free quarterly newsletter for space-interested and space-enthused people around the globe This free publication is especially dedicated to students and teachers interested in space NEWS SECTION pp. 3-22 p. 3 Earth Orbit and Mission to Planet Earth - 13 reports p. 8 Cislunar Space and the Moon - 5 reports p. 11 Mars and the Asteroids - 5 reports p. 15 Other Planets and Moons - 2 reports p. 17 Starbound - 4 reports, 1 article ---------------------------------------------------------------------------------------------------- ARTICLES, ESSAYS & MORE pp. 23-45 - 10 articles & essays (full list on last page) ---------------------------------------------------------------------------------------------------- STUDENTS & TEACHERS pp. 46-56 - 9 articles & essays (full list on last page) L: Remote sensing of Aerosol Optical Depth over India R: Curiosity finds rocks shaped by running water on Mars! L: China hopes to put lander on the Moon in 2013 R: First Square Kilometer Array telescopes online in Australia! 1 TTSIQ #1 page 2 OCTOBER 2012 TTSIQ Sponsor Organizations 1. About The National Space Society - http://www.nss.org/ The National Space Society was formed in March, 1987 by the merger of the former L5 Society and National Space institute. NSS has an extensive chapter network in the United States and a number of international chapters in Europe, Asia, and Australia. NSS hosts the annual International Space Development Conference in May each year at varying locations. NSS publishes Ad Astra magazine quarterly. NSS actively tries to influence US Space Policy. About The Moon Society - http://www.moonsociety.org The Moon Society was formed in 2000 and seeks to inspire and involve people everywhere in exploration of the Moon with the establishment of civilian settlements, using local resources through private enterprise both to support themselves and to help alleviate Earth's stubborn energy and environmental problems. -
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. -
KISS Lunar Volatiles Workshop 7-22-2013
Future Lunar Missions: Plans and Opportunities Leon Alkalai, JPL New Approaches to Lunar Ice Detection and Mapping Workshop Keck Institute of Space Studies July 22nd – July 25th, 2013 California Institute of Technology Some Lunar Robotic Science & Exploration Mission Formulation Studies at JPL (2003 – 2013) MoonRise New Frontiers GRAIL (2005-2007) Moonlight (2003-2004) (2005-2012) Lunette – Discovery Proposal Pre-Phase A Network of small landers (2005-2011) MIRANDA: cold trap access (2010) Lunar Impactor (2006) Other Lunar Science & Exploration Studies at JPL (2003 – 2013) • Sample Acquisition and Transfer Systems (SATS) • Landers: hard landers, soft landers, powered descent, hazard avoidance, nuclear powered lander and rover • Sub-surface access: penetrators deployed from orbit, drills, heat- flow probe, etc. • Surface mobility: Short-range, long-range, access to cold traps in deep craters • CubeSats and other micro-spacecraft deployed e.g. gravity mapping • International Studies & Discussions: – MoonLITE lunar orbiter and probes with UKSA – Farside network of lunar landers, with ESA, CNES, IPGP – Lunar Exploration Orbiter (LEO) with DLR – Lunar Com Relay Satellite with ISRO – Canadian Space Agency: robotics, surface mobility – In-situ science with RSA, landers, rovers – JAXA lunar landers, rovers – Korean Space Agency 7/23/2013 L. Alkalai, JPL 3 Robotic Missions to the Moon: Just in the last decade: 2003 - 2013 • Smart-1 ESA September 2003 • Chang’e-1 China October 2007 • SELENE-1 Japan September 2007 • Chandrayaan-1 India October 2008 – M3, Mini-SAR USA • LRO USA June 2009 • LCROSS USA June 2009 • Chang’e-2 China October 2010 • GRAIL USA September 2011 • LADEE USA September 6 th , 2013 7/23/2013 L.