Bepicolombo - a Mission to Mercury
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Ices on Mercury: Chemistry of Volatiles in Permanently Cold Areas of Mercury’S North Polar Region
Icarus 281 (2017) 19–31 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Ices on Mercury: Chemistry of volatiles in permanently cold areas of Mercury’s north polar region ∗ M.L. Delitsky a, , D.A. Paige b, M.A. Siegler c, E.R. Harju b,f, D. Schriver b, R.E. Johnson d, P. Travnicek e a California Specialty Engineering, Pasadena, CA b Dept of Earth, Planetary and Space Sciences, University of California, Los Angeles, CA c Planetary Science Institute, Tucson, AZ d Dept of Engineering Physics, University of Virginia, Charlottesville, VA e Space Sciences Laboratory, University of California, Berkeley, CA f Pasadena City College, Pasadena, CA a r t i c l e i n f o a b s t r a c t Article history: Observations by the MESSENGER spacecraft during its flyby and orbital observations of Mercury in 2008– Received 3 January 2016 2015 indicated the presence of cold icy materials hiding in permanently-shadowed craters in Mercury’s Revised 29 July 2016 north polar region. These icy condensed volatiles are thought to be composed of water ice and frozen Accepted 2 August 2016 organics that can persist over long geologic timescales and evolve under the influence of the Mercury Available online 4 August 2016 space environment. Polar ices never see solar photons because at such high latitudes, sunlight cannot Keywords: reach over the crater rims. The craters maintain a permanently cold environment for the ices to persist. Mercury surface ices magnetospheres However, the magnetosphere will supply a beam of ions and electrons that can reach the frozen volatiles radiolysis and induce ice chemistry. -
The Search for Another Earth – Part II
GENERAL ARTICLE The Search for Another Earth – Part II Sujan Sengupta In the first part, we discussed the various methods for the detection of planets outside the solar system known as the exoplanets. In this part, we will describe various kinds of exoplanets. The habitable planets discovered so far and the present status of our search for a habitable planet similar to the Earth will also be discussed. Sujan Sengupta is an 1. Introduction astrophysicist at Indian Institute of Astrophysics, Bengaluru. He works on the The first confirmed exoplanet around a solar type of star, 51 Pe- detection, characterisation 1 gasi b was discovered in 1995 using the radial velocity method. and habitability of extra-solar Subsequently, a large number of exoplanets were discovered by planets and extra-solar this method, and a few were discovered using transit and gravi- moons. tational lensing methods. Ground-based telescopes were used for these discoveries and the search region was confined to about 300 light-years from the Earth. On December 27, 2006, the European Space Agency launched 1The movement of the star a space telescope called CoRoT (Convection, Rotation and plan- towards the observer due to etary Transits) and on March 6, 2009, NASA launched another the gravitational effect of the space telescope called Kepler2 to hunt for exoplanets. Conse- planet. See Sujan Sengupta, The Search for Another Earth, quently, the search extended to about 3000 light-years. Both Resonance, Vol.21, No.7, these telescopes used the transit method in order to detect exo- pp.641–652, 2016. planets. Although Kepler’s field of view was only 105 square de- grees along the Cygnus arm of the Milky Way Galaxy, it detected a whooping 2326 exoplanets out of a total 3493 discovered till 2Kepler Telescope has a pri- date. -
Mariner to Mercury, Venus and Mars
NASA Facts National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109 Mariner to Mercury, Venus and Mars Between 1962 and late 1973, NASA’s Jet carry a host of scientific instruments. Some of the Propulsion Laboratory designed and built 10 space- instruments, such as cameras, would need to be point- craft named Mariner to explore the inner solar system ed at the target body it was studying. Other instru- -- visiting the planets Venus, Mars and Mercury for ments were non-directional and studied phenomena the first time, and returning to Venus and Mars for such as magnetic fields and charged particles. JPL additional close observations. The final mission in the engineers proposed to make the Mariners “three-axis- series, Mariner 10, flew past Venus before going on to stabilized,” meaning that unlike other space probes encounter Mercury, after which it returned to Mercury they would not spin. for a total of three flybys. The next-to-last, Mariner Each of the Mariner projects was designed to have 9, became the first ever to orbit another planet when two spacecraft launched on separate rockets, in case it rached Mars for about a year of mapping and mea- of difficulties with the nearly untried launch vehicles. surement. Mariner 1, Mariner 3, and Mariner 8 were in fact lost The Mariners were all relatively small robotic during launch, but their backups were successful. No explorers, each launched on an Atlas rocket with Mariners were lost in later flight to their destination either an Agena or Centaur upper-stage booster, and planets or before completing their scientific missions. -
ESA & ESOC Overview
NASA PM Challenge 2010 Developing the International Program/Project Management Community 9/10 February 2010 Dr. Bettina Böhm Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 1 Used with Permission PURPOSE OF ESA / ACTIVITIES “To provide for and promote, for exclusively Space science peaceful purposes, cooperation among Human spaceflight European states in space research and Exploration technology and their space applications.” Earth observation Launchers [Article 2 of ESA Convention] Navigation ESA is one of the few space agencies Telecommunications in the world to combine responsibility Technology in all areas of space activity. Operations Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 2 ESA FACTS AND FIGURES Over 30 years of experience 18 Member States 2080 staff, thereof 880 in Program Directorates, 790 in Operations and Technical Support and 410 in other Support Directorates 3 500 million Euros budget Over 60 satellites designed and tested Over 60 satellites operated in-flight and 8 missions rescued 16 scientific satellites in operation Five types of launcher developed More than 180 launches made Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 3 ESA Locations EAC (Cologne) Salmijaervi ESTEC Astronaut training (Noordwijk) Satellite technology development and testing Harwell ESOC ESA HQ (Darmstadt) (Paris) Brussels Satellite operations and ground system technology development ESAC (Villanueva de la Cañada Oberpfaffenhofen -
Moon & Mercury Overview
Moon & Mercury Overview • Both Small • Mercury: Densest Planet! • Moon: Density less than Earth Mercury Venus Earth Moon Mars Distance (Sun) 0.39 AU 1 AU 1 AU Orbital Period 88 days 1 year 27.3 days** Rotation Period 59 days 23.9 hours 27.3 days Radius (km) 6378 km Radius (R⊕) 0.38 R⊕ 1 R⊕ 0.25 R⊕ Mass (kg) 6.0x1024 kg Mass (M⊕) 0.055 M⊕ 1 M⊕ 0.012 M⊕ Avg. Surface T -290 to 800 F̊ 59 F̊ -240 to 240 F̊ ** around Earth Lunar Surface • Cratered – 30,000 big (> 1km) – millions of smaller craters MercurianMercury Surface - Surface Features Messenger Images Era of Heavy Bombardment Period of intense impacts in the inner S.S. by leftover planetesimals from outer S.S. 4.1-3.8 billion yrs ago affects all Terr. planets Lunar Surface • Dark Maria (“Seas”) • Lighter Highlands (“Lands”, Terrae) Lunar Surface • Maria What’s different? Why? • Highlands Apollo Lunar Surface Maria: smooth, flat, fewer craters Highlands: VERY cratered Maria have been resurfaced! Maria Formation After Heavy Bombardment Volcanic Activity caused by heat from radioactive decay flooded old craters Dating the Lunar Surface Crater Counting! Which is oldest? The Moon - Space Exploration • Luna 3 (Russia), 1959 Luna 3 farside • NASA Rangers (Impactors), 1961-1965 • Orbiters (99% mapped), 1966-1967 • Surveyors (landers), 1966-1968 • Apollo (manned), 1968-1972 • Clementine (Multi-wavel. mapping), 1994 • Prospector (polar orbiter), 1998 • SMART-1 (ESA Impactor), 2003-2006 • Kaguya (Japan), 2007- Prospector • Chang-e 1 (China), 2007- • Chandrayaan (India), 2008- Orbiter • Lunar Recon. -
The Composition of Planetary Atmospheres 1
The Composition of Planetary Atmospheres 1 All of the planets in our solar system, and some of its smaller bodies too, have an outer layer of gas we call the atmosphere. The atmosphere usually sits atop a denser, rocky crust or planetary core. Atmospheres can extend thousands of kilometers into space. The table below gives the name of the kind of gas found in each object’s atmosphere, and the total mass of the atmosphere in kilograms. The table also gives the percentage of the atmosphere composed of the gas. Object Mass Carbon Nitrogen Oxygen Argon Methane Sodium Hydrogen Helium Other (kilograms) Dioxide Sun 3.0x1030 71% 26% 3% Mercury 1000 42% 22% 22% 6% 8% Venus 4.8x1020 96% 4% Earth 1.4x1021 78% 21% 1% <1% Moon 100,000 70% 1% 29% Mars 2.5x1016 95% 2.7% 1.6% 0.7% Jupiter 1.9x1027 89.8% 10.2% Saturn 5.4x1026 96.3% 3.2% 0.5% Titan 9.1x1018 97% 2% 1% Uranus 8.6x1025 2.3% 82.5% 15.2% Neptune 1.0x1026 1.0% 80% 19% Pluto 1.3x1014 8% 90% 2% Problem 1 – Draw a pie graph (circle graph) that shows the atmosphere constituents for Mars and Earth. Problem 2 – Draw a pie graph that shows the percentage of Nitrogen for Venus, Earth, Mars, Titan and Pluto. Problem 3 – Which planet has the atmosphere with the greatest percentage of Oxygen? Problem 4 – Which planet has the atmosphere with the greatest number of kilograms of oxygen? Problem 5 – Compare and contrast the objects with the greatest percentage of hydrogen, and the least percentage of hydrogen. -
First Look at Mercury
PLANETARY SCIENCE Mariner 10 was launched to Mercury by way of Venus on November 3, 1973. It was not the first probe to visit Venus. Both the United States and the Soviet Union previously have sent probes to that mysterious, cloud-shrouded planet. However, Mariner 10 was the first to photographically explore the close-up appearance of the planet, and did so both in visibIe and in ultraviolet light. And Mariner 10 was the first probe of any kind to penetrate interplanetary space beyond the orbit of Venus and to achieve a close look at the planet Mercury. First Look Why go to Mercury? Who needs it? There basically are two kinds of reasons. The first is simple and profound and at Mercury difficult to quantify: The very act of exploration is a positive, cultural activity. No one knows what is going to be found. Finding out what Mercury, what Mars, or BRUCE C. MURRAY what the moon is really like, enlarges the consciousness of all the people who partake of that new reality. TV pictures are of special importance because they provide a way both for the scientist to discover features and concepts he could not have imagined and for the public to directly appreciate and participate in the exploration of a new world. Why go to Mercury? Who needs it? But there are more specific scientific objectives as well. For Mercury, the basic-and anomalous-scientific fact is A planetary scientist that it is a very dense planet: It contains a great amount of tells what the voyage mass for its size. -
Mariner 10 Observations of Field-Aligned Currents at Mercury
Planet. Space Sci., Vol. 45, No. 1, pp. 133-141, 1997 Pergamon #I? 1997 Published bv Elsevier Science Ltd P&ted in Great Brit& All rights reserved 0032-0633/97 $17.00+0.00 PII: S0032-0633(96)00104-3 Mariner 10 observations of field-aligned currents at Mercury J. A. Slavin,’ J. C. J. Owen,’ J. E. P. Connerney’ and S. P. Christon ‘Laboratory for Extraterrestrial Physics, NASA/GSFC, Greenbelt, MD 20771, U.S.A. ‘Astronomy Unit, Queen Mary and Westfield College, London, U.K. 3Department of Physics, University of Maryland, College Park, MD 20742, U.S.A. Received 5 October 1995; revised 11 April 1996; accepted 13 April 1996 magnetic field at Mercury with a dipole moment of about 300nT R& (see review by Connerney and Ness (1988)). This magnetic field is sufficient to stand-off the average solar wind at an altitude of about 1 RM as depicted in Fig. 1 (see review by Russell et al. (1988)). For the purposes of comparison the diameter of the Earth is indicated at the bottom of the figure (i.e. 1 RE = 6380 km ; 1 RM = 2439 km). Whether or not the solar wind is ever able to compress and/or erode the dayside magnetosphere to the point where solar wind ions could directly impact the surface remains a topic of considerable controversy (Siscoe and Christopher, 1975 ; Slavin and Holzer, 1979 ; Hood and Schubert, 1979; Suess and Goldstein, 1979; Goldstein et al., 1981). Overall, the basic morphology of this small mag- netosphere appears quite similar to that of the Earth. -
Mysterious Mercury Bepicolumbo Heads for the World of Ice and Fire
A Digital Supplement to Astronomy Insights Astronomy Magazine © 2018 Kalmbach Media Mysterious Mercury BepiColumbo Heads for the World of Ice and Fire Dcember 2018 • Astronomy.com Voyage to a world Color explodes from Mercury’s surface in this enhanced-color mosaic taken through several filters. The yellow and orange hues signify relatively young plains likely formed when fluid lavas erupted from volcanoes. Medium- and dark-blue regions are older terrain, while the light-blue and white streaks represent fresh material excavated from relatively recent impacts. ALL IMAGES, UNLESS OTHERWISE NOTED: NASA/JHUAPL/CIW 2 ASTRONOMY INSIGHTS • DECEMBER 2018 A world of both fire and ice, Mercury excites and confounds scientists. The BepiColombo probe aims to make sense of this mysterious world. by Ben Evans of extremesWWW.ASTRONOMY.COM 3 Mercury is a land of contrasts. The solar system’s smallest planet boasts the largest core relative to its size. Temperatures at noon can soar as high as 800 degrees Fahrenheit (425 degrees Celsius) — hot enough to melt lead — but dip as low as –290 F (–180 C) before dawn. Mercury resides nearest the Sun, and it has the most eccentric orbit. At its closest, the planet lies only 29 mil- lion miles (46 million kilometers) from the Sun — less than one-third Earth’s distance — but swings out as far as 43 million miles (70 million km). Its rapid movement across our sky earned it a reputation among ancient skywatchers as the fleet-footed messenger of the gods: Italian scientist Giuseppe “Bepi” Colombo helped develop a technique for sending a space Hermes to the Greeks and Mercury to the Romans. -
Sized Exoplanet Thomas Barclay1,2, Jason F
A sub-Mercury-sized exoplanet Thomas Barclay1,2, Jason F. Rowe1,3, Jack J. Lissauer1, Daniel Huber1,4, François Fressin5, Steve B. Howell1, Stephen T. Bryson1, William J. Chaplin6, Jean-Michel Désert5, Eric D. Lopez7, Geoffrey W. Marcy8, Fergal Mullally1,3, Darin Ragozzine5,9, Guillermo Torres5, Elisabeth R. Adams5, Eric Agol10, David Barrado11,12, Sarbani Basu13, Timothy R. Bedding14, Lars A. Buchhave15,16, David Charbonneau5, Jessie L. Christiansen1,3, Jørgen Christensen-Dalsgaard17, David Ciardi18, William D. Cochran19, Andrea K. Dupree5, Yvonne Elsworth6, Mark Everett20, Debra A. Fischer13, Eric B. Ford9, Jonathan J. Fortney7, John C. Geary5, Michael R. Haas1, Rasmus Handberg17, Saskia Hekker6,21, Christopher E. Henze1, Elliott Horch22, Andrew W. Howard23, Roger C. Hunter1, Howard Isaacson8, Jon M. Jenkins1,3, Christoffer Karoff17, Steven D. Kawaler24, Hans Kjeldsen17, Todd C. Klaus25, David W. Latham5, Jie Li1,3, Jorge Lillo-Box12, Mikkel N. Lund17, Mia Lundkvist17, Travis S. Metcalfe26, Andrea Miglio6, Robert L. Morris1,3, Elisa V. Quintana1,3, Dennis Stello14, Jeffrey C. Smith1,3, Martin Still1,2, & Susan E. Thompson1,3 1 NASA Ames Research Center, Moffett Field, CA 94035, USA 2 Bay Area Environmental Research Institute, 596 First St West, Sonoma, CA 95476, USA 3 SETI Institute, 189 Bernardo Ave, Mountain View, CA 94043, USA 4 NASA Postdoctoral Program Fellow 5 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA 6 School of Physics and Astronomy, University of Birmingham, Edgbaston, B15 2TT, UK 7 Department of Astronomy and Astrophysics, University of California, Santa Cruz, CA 95064, USA 8 Department of Astronomy, UC Berkeley, Berkeley, CA 94720, USA 9 Astronomy Department, University of Florida, 211 Bryant Space Sciences Center, Gainesville, FL 32111, USA 10 Department of Astronomy, Box 351580, University of Washington, Seattle, WA 98195, USA 11 Calar Alto Observatory, Centro Astronómico Hispano Alemán, C/ Jesús Durbán Remón, E- 04004 Almería, Spain 12 Depto. -
Japan's Asteroid Missions Hayabusa and Hayabusa2
Japan's Asteroid Missions Hayabusa and Hayabusa2 COPUOS 2013 February 15, 2013, Vienna, Austria Makoto Yoshikawa Hayabusa & Hayabusa2 Project Team, JAXA Lunar and Planetary Missions of Japan ×LUNAR- Hiten A ×Nozom Moon IKAROS 1985 i Moon Sakigake Kaguya 1990 Mars △Akatsuki 1998 Moon Suisei 2003 Hayabusa Venus 2007 BepiColombo 2010 2014 Comet Halley Asteroid Itokawa Hayabusa2 Mercury Asteroid 1999 JU3 February 15, 2013 COPUOS 2013 2 Challenges of Hayabusa and Hayabusa2 Development of the technology for asteroid sample return •Ion engine •Autonomous navigation •Sample collection system •Reentry capsule Impactor system * Study of the origin and evolution of the solar system Molecular cloud Proto solar system disk Solar system Evolution of planets Minerals, H 2O *, Organic matters * (*Hayabusa2) February 15, 2013 COPUOS 2013 3 History of Hayabusa and Hayabusa2 Idea for sample Serious troubles return began in1985 in Hayabusa Now Year 200 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 0 Sample MUSES-C Hayabusa Analysis ▲ ▲ launch Earth return project Started Hayabusa Mk2 in 1996 Post MUSES-C Post Hayabusa Post Marco Polo Haybusa2 Launch Hyabusa2 Phase-B ▲ Initial proposal in 2006 New proposal in 2009 Copy of Hayabusa but modified Modified Hayabusa adding new challenges Target : C-type asteroid 1999 JU3 Target : C-type asteroid 1999 JU3 Launch: 2010 Launch: 2014 February 15, 2013 COPUOS 2013 4 Starting point of Hayabusa Small Meeting for Asteroid Sample Return Mission ISAS June 29, 1985 Cover of meeting February 15, 2013 COPUOS 2013 5 Mission Scenario of Hayabusa Observations, sampling Earth Swingby Launch 19 May 2004 9 May 2003 Asteroid Arrival 12 Sept. -
Bepicolombo Quick-Look Analysis Interface Status
EPSC Abstracts Vol. 13, EPSC-DPS2019-921-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. BepiColombo Quick-Look Analysis interface status Thomas Cornet (1), Mark S. Bentley (2), Alan Macfarlane (3), Santa Martínez (4) and the BepiColombo SGS Team. (1) Aurora Technology BV for ESA, (2) HE Space for ESA, (3) Serco Nederland BV for ESA, (4) ESA/ESAC, Villanueva de la Cañada, Madrid, Spain. ([email protected]) Abstract by allowing them to share information in a centralised place. The ESA/JAXA BepiColombo mission to Mercury [1] was launched on the October 20th, 2018. During 2. Development and status its seven years Cruise phase, BepiColombo will perform several flybys of the Earth, Venus and The QLA is the end part of the BepiColombo Science Mercury before its insertion into orbit and start of Operation Control System (BSCS) [2] architecture. science phase at the beginning of 2026. In the harsh The BSCS includes several subsystems retrieving hermean environment, the mission various and processing the spacecraft and instruments instruments will allow studying Mercury as a whole telemetry. Science data are stored according to PDS4 system where the interior, surface and space weather standards in the Planetary Science Archive (PSA) [3]. science will be inter-connected. In this context, the The SGS is responsible of the first step of data ESA Science Ground Segment (SGS) aims at conversion from telemetry to raw data. The providing a support tool for data visualisation and subsequent data levels (partially processed, calibrated) analysis, suited to the specific needs of each are in vast majority produced by the ITs and then instrument team, and facilitating scientific delivered to the SGS.