IEEE Waves and Devices Phoenix Chapter: Space Communications

Total Page:16

File Type:pdf, Size:1020Kb

IEEE Waves and Devices Phoenix Chapter: Space Communications IEEE Waves and Devices Phoenix Chapter: Space Communications Bob Anderson 24 June 2010 Introduction Why communicate? Must control the spacecraft/experiment In human spaceflight, lives depend on it Must track the craft Ranging (distance/position) Relative speed (Doppler effect) Collect science data Usually the purpose of the mission in the first place 2 Communications TRANSMITTER RECEIVER RECEIVER TRANSMITTER COMMUNICATIONS DID THE RECEIVER RECEIVE THE SIGNAL? DID THE RECEIVER PROCESS THE SIGNAL CORRECTLY? DID I RECEIVE THE CORRECT TELEMETRY/DATA BACK? 3 Radio Po f AUDIO RF CARRIER AM MODULATED AM MODULATED (TIME DOMAIN) (FREQUENCY DOMAIN) Po f AUDIO PULSE CODE PCM PCM (TIME DOMAIN) (FREQUENCY DOMAIN) 4 TT&C Telemetry Tracking and Command (TT&C) Monitor received telemetry Health and mode analysis Perform tracking Distance and position measurements Doppler measurements – spacecraft velocity Send commands Command the spacecraft for attitude, position, and miscellaneous functions 5 Transponder GROUND STATION TRANSPONDER TRANSMITTER RECEIVER RECEIVER TRANSMITTER BENT PIPE TRANSPONDER TRANSMITS EXACTLY WHAT IT RECEIVES 6 Transponder GROUND STATION TRANSPONDER TRANSMITTER RECEIVER RECEIVER TRANSMITTER TWO WAY TRANSPONDER RECEIVES COMMANDS TRANSMITS SCIENCE DATA AND TELEMETRY 7 U.S. Space Program Timeline NRL V2, SPUTNIK, EXPLORER, PIONEER, MERCURY Vanguard RANGER, GEMINI Space Programs (USA) APOLLO, LUNAR ORBITER, MARINER, SURVEYOR SKY LAB, PIONEER 10, MARINER 10, HELIOS VIKING, VOYAGER I, II, PIONEER VENUS, INTERNATIONAL SUN-EARTH, SOLAR MAXIMUM 1956-1962 1963-1965 1966-1967 1968-1969 1970-1975 1976-1980 TDRSS I, SPACE SHUTTLE GD (Motorola) contributions VOYAGER, NASA STDN S-BAND SPECIAL TEST EQUIPMENT, MARINER MARS APOLLO TRANSPONDERS, LUNAR ORBITER RANGER AND MARINER TRANSPONDERS, APOLLO STUDY JPL X-BAND, RANGER AND MARINER TRANSPONDERS 8 U.S. Space Program Timeline MAGELLAN, GALILEO, HUBBLE SPACE TELESCOPE, ULYSSES Space Programs MARS OBSERVER, CLEMENTINE, SOHO (USA) SPACE STATION, NEAR, MARS GLOBAL SURVEYOR, MARS PATHFINDER, CASSINI/HUYGENS LUNAR PROSPECTOR, DEEP SPACE I, STARDUST, MARS POLAR LANDER IMAGE, MARS ODYSSEY, GENESIS, CONTOUR, MARS EXPRESS MRO, JUNO, LRO, STEREO, DAWN (NEW HORIZONS), MARS LANDER 1981-1985 1986-1990 1991-1995 1996-2000 2001-2005 2006-2010 MRO, JUNO, LRO, STEREO, DAWN (NEW HORIZONS), MARS LANDER GD (Motorola) contributions SDST, CASSINI, MARS ODYSSEY, STARDUST, SPITZER SPACE TELESCOPE, MARS ROVERS, DEEP IMPACT, MERCURY MESSINGER, MARS EXPRESS DST, TDRSS IV, SPACE STATION, NEAR, MARS GLOBAL SURVEYOR, MARS PATHFINDER, CASSINI/HUYGENS, DEEP SPACE I, STARDUST, MARS POLAR LANDER, MARS ODYSSEY IRIDIUM, MARS OBSERVER, SOHO JPL DSN 3, MAGELLAN, GALILEO, HUBBLE SPACE TELESCOPE JPL DSN, TDRSS II, III 9 Link Budget E = + − b − − − − − M (dB ) EIRP (dBW ) Gr (dBi ) (dB ) R(dB bit / s) kT (dBW / Hz ) Ls (dB ) Lo (dB ) N o reqd EIRP = Effective Isotropic Radiated Power, or Transmitted Power in dB-Watts Gr = Antenna Gain, dBi – referenced to isotropic Eb/No = Average energy per bit per unit of noise, required, dB R = Data rate, referenced to 1 bit/sec – dB-bit/sec kT = Boltzmann’s constant times temperature in Kelvins – (dBW/Hz) Ls = Path loss, dB – proportional to (4pd) 2 Lo = All other losses, dB (rain, solar effects, etc.) Source: Sklar, B., Digital Communications, Prentice Hall, NJ, 1988 10 Link Budget Source: Sklar, B., Digital Communications, Prentice Hall, NJ, 1988 11 Link Budget Source: Sklar, B., Digital Communications, Prentice Hall, NJ, 1988 12 Van Allen Radiation Belt Discovered by Explorer I and II in 1958 under direction of Dr. James Van Allen. A satellite shielded by 3 mm of aluminum in an elliptic orbit (200 by 20,000 miles) passing through the radiation belts will receive about 2,500 rem (25 Sv) per year. Almost all radiation will be received while passing the inner belt. 25 Sv = 25 J/kg. The inner belt is 60 to 6,200 miles high Source: NASA 13 South Atlantic Anomaly The South Atlantic Anomaly (SAA) refers to the area where the Earth's inner Van Allen radiation belt comes closest to the Earth’s surface. This leads to an increased flux of energetic particles in this region and exposes orbiting satellites to higher than usual levels of radiation. The effect is caused by the non- concentricity of the Earth and its magnetic dipole, and the SAA is the near-Earth region where the Earth’s magnetic field is weakest. SAA Source: NASA 14 Space Debris Problem Source: National Geographic July 2010 15 Space Debris Problem Source: National Geographic July 2010 16 Space Debris Problem Source: National Geographic July 2010 17 Earth Satellite Communications Geo-synchronous/stationary Weather Broadcast TDRSS Earth orbital IRIDIUM Scientific Study Space Station 18 Weather GOES-8 Satellite and Weather Map (22,236 mi. High Orbit) Source: NASA 19 TDRSS Tracking and Data Satellite System (TDRSS) Source: NASA/GD (Motorola) 20 TDRSS Tracking and Data Satellite System (TDRSS) Source: NASA 21 Iridium Iridium Satellite (485 mi. High Orbit) Source: Iridium/GD (Motorola) 22 Space Station Space Station (181 – 189 mi. high Orbit) Source: NASA/GD (Motorola) 23 Space Station Space Station Source: NASA 24 Space Station Space Station Source: NASA/JSC 25 Manned Missions Communications Mercury Gemini Apollo Space Shuttle Space Station 26 Manned Missions GD (Motorola) supported various phases of Apollo program Unified s-band transponder Command module unified amplifier Functional communications link that carried astronauts’ pictures and voice from the Moon’s surface back to Earth 27 Apollo Apollo Command Module Unified S-Band Transponder (manufactured by Motorola, Inc., Military Electronics Division, Scottsdale, Ariz.). The Unified S-Band Transponder was the only method of exchanging voice communications, tracking, biomedical, and ranging, transmission of pulse code modulated (PCM) data and television, and reception of uplinked data from Mission Control once the Apollo Command Module was outside a range of 1500 nautical miles and line of sight from Manned Space Flight Network (MSFN) ground stations strung around the Earth (within that range, VHF was available). The term "Unified" is applicable because the communications system combined the functions of (signal) acquisition, telemetry, command, voice, television and tracking on one radio link. The Unified S-Band Equipment (USBE) onboard the Apollo Command Module, Lunar Module, Lunar Rover were absolutely critical to the successful execution of the Apollo program; and reliability was assured through the implementation of full redundant, heavily tested design. Source: SpaceAholic.com 28 Apollo APOLLO COMMAND MODULE UNIFIED S-BAND TRANSPONDER Source: SpaceAholic.com 29 Apollo The location of artifacts discussed in this when installed in their native environment (within the Block II Apollo Command Module). This profile depicts the Lower Equipment bay where the majority of the spacecraft telecommunications subsystem electronics were housed). For reference the Astronauts feet (when laying in the crew couch) are oriented towards the Equipment bay). Source: SpaceAholic.com 30 Apollo Motorola Corporation News Bureau release photograph of Apollo Command Module Unified S-Band Equipment (USBE) Transponder - the release reads: "The two-way radio on the Apollo Command Module requires less power to communicate with Earth from the vicinity of the Moon then the power used by the light bulbs in your refrigerator. The small unit, produced by Motorola Government Electronics Division, is the only communications link with the Apollo Command Module crew has with Earth from beyond 30,000 miles away providing all voice contact, TV pictures and mission data. Lovely Motorola technician Mandy Biondi shows the sophisticated unit which has functioned perfectly on every mission." (Image courtesy Motorola/GDAIS). Source: SpaceAholic.com 31 Space Probe Communications Early missions Sputnik Explorer Ranger Mariner Pioneer Surveyor Voyager I, II Magellan Galileo 32 Sputnik Launched October 4, 1957; operated for 3 months Source: University of Colorado Students for the Exploration and Development of Space 33 Vanguard I Launched March 17, 1958; operated for 6 years ~ 2,200 days (first solar-powered satellite) Source: NASA 34 Voyager Voyager I,II Source: NASA/JPL 35 Voyager Voyager I,II Source: NASA/JPL 36 Galileo Galileo Source: NASA/JPL 37 Magellan Venus Radar Mapper (Magellan) Source: NASA/JPL 38 Space Probe Communications Cassini Mars Lunar Other probes 39 SDST Small Deep Space Transponder (SDST) Source: GD (Motorola) 40 Cassini Cassini Source: NASA/JPL 41 Cassini 42 Cassini 43 Cassini 44 Mars Source: NASA/JPL 45 Mars Source: NASA/JPL 46 Mars Source: NASA/JPL 47 Mars Source: NASA/JPL 48 Mars Panoramic Camera (Pancam): for determining the mineralogy, texture, and structure of the local terrain Miniature Thermal Emission Spectrometer (Mini- TES): for identifying promising rocks and soils for closer examination and for determining the processes that formed Martian rocks. The instrument is designed to look skyward to provide temperature profiles of the Martian atmosphere. Mössbauer Spectrometer (MB): for close-up investigations of the mineralogy of iron-bearing rocks and soils. Source: NASA/JPL 49 Mars Alpha Particle X-Ray Spectrometer (APXS): for close-up analysis of the abundances of elements that make up rocks and soils. Magnets: for collecting magnetic dust particles. The Mössbauer Spectrometer and the Alpha Particle X-ray Spectrometer are designed to analyze
Recommended publications
  • New Views of the Moon Enabled by Combined Remotely Sensed and Lunar Sample Data Sets, a Lunar Initiative
    New Views of the Moon Enabled by Combined Remotely Sensed and Lunar Sample Data Sets, A Lunar Initiative Using the hand tool on your Reader, click on the links below to view that particular section of the proposal. Proposal Summary Scientific/Technical/Management Objectives and Expected Significance Background and Impact Approach and Methodology: The Role of Integration in Fundamental Problems of Lunar Geoscience Workshop 2: New Views of the Moon II: Understanding the Moon Through the Integration of Diverse Datasets. Abstract Volume and Subsequent Publications Statement of Relevance Work Plan Potential Workshop (2000): Thermal and Magmatic Evolution of the Moon Potential Workshop (2001): Early Lunar Differentiation, Core Formation, Effects of Early Planetesimal Impacts, and the Origin of the Moon’s Global Asymmetry Potential Workshop (2002): Selection of Sites for Future Sample Return Capstone Publication Timeline for the New Views of the Moon Initiative Personnel: Initiative Management and Proposal Management References Facilities: The LPI Appendix 1. Workshop on New Views of the Moon: Integrated Remotely Sensed, Geophysical, and Sample Datasets. List of presentations Appendix 2. LPSC 30 (1999) special sessions related to the Lunar Initiative. List of presentations (oral and poster) Appendix 3. Lunar Initiative Steering Committee Web Note: This is the text of a proposal submitted on behalf of the Lunar Science Community to support ongoing workshops and activities associated with the CAPTEM Lunar Initiative. It was submitted in May, 1999, in response to the ROSS 99 NRA, which solicits such proposals to be submitted to the relevant research programs. This proposal was submitted jointly to Cosmo- chemistry and Planetary Geology and Geophysics.
    [Show full text]
  • Atlas V Launches LRO/LCROSS Mission Overview
    Atlas V Launches LRO/LCROSS Mission Overview Atlas V 401 Cape Canaveral Air Force Station, FL Space Launch Complex-41 AV-020/LRO/LCROSS United Launch Alliance is proud to be a part of the Lunar Reconnaissance Orbiter (LRO) and the Lunar Crater Observation and Sensing Satellite (LCROSS) mission with the National Aeronautics and Space Administration (NASA). The LRO/LCROSS mission marks the sixteenth Atlas V launch and the seventh flight of an Atlas V 401 configuration. LRO/LCROSS is a dual-spacecraft (SC) launch. LRO is a lunar orbiter that will investigate resources, landing sites, and the lunar radiation environment in preparation for future human missions to the Moon. LCROSS will search for the presence of water ice that may exist on the permanently shadowed floors of lunar polar craters. The LCROSS mission will use two Lunar Kinetic Impactors, the inert Centaur upper stage and the LCROSS SC itself, to produce debris plumes that may reveal the presence of water ice under spectroscopic analysis. My thanks to the entire Atlas team for its dedication in bringing LRO/LCROSS to launch, and to NASA for selecting Atlas for this ground-breaking mission. Go Atlas, Go Centaur, Go LRO/LCROSS! Mark Wilkins Vice President, Atlas Product Line Atlas V Launch History Flight Config. Mission Mission Date AV-001 401 Eutelsat Hotbird 6 21 Aug 2002 AV-002 401 HellasSat 13 May 2003 AV-003 521 Rainbow 1 17 Jul 2003 AV-005 521 AMC-16 17 Dec 2004 AV-004 431 Inmarsat 4-F1 11 Mar 2005 AV-007 401 Mars Reconnaissance Orbiter 12 Aug 2005 AV-010 551 Pluto New Horizons 19 Jan 2006 AV-008 411 Astra 1KR 20 Apr 2006 AV-013 401 STP-1 08 Mar 2007 AV-009 401 NROL-30 15 Jun 2007 AV-011 421 WGS SV-1 10 Oct 2007 AV-015 401 NROL-24 10 Dec 2007 AV-006 411 NROL-28 13 Mar 2008 AV-014 421 ICO G1 14 Apr 2008 AV-016 421 WGS-2 03 Apr 2009 Payload Fairing Number of Solid Atlas V Size (meters) Rocket Boosters Flight/Configuration Key AV-XXX ### Number of Centaur Engines 3-digit Tail Number 3-digit Configuration Number LRO Overview LRO is the first mission in NASA’s planned return to the Moon.
    [Show full text]
  • Protons in the Near Lunar Wake Observed by the SARA Instrument on Board Chandrayaan-1
    FUTAANA ET AL. PROTONS IN DEEP WAKE NEAR MOON 1 Protons in the Near Lunar Wake Observed by the SARA 2 Instrument on Board Chandrayaan-1 3 Y. Futaana, 1 S. Barabash, 1 M. Wieser, 1 M. Holmström, 1 A. Bhardwaj, 2 M. B. Dhanya, 2 R. 4 Sridharan, 2 P. Wurz, 3 A. Schaufelberger, 3 K. Asamura 4 5 --- 6 Y. Futaana, Swedish Institute of Space Physics, Box 812, Kiruna, SE-98128, Sweden. 7 ([email protected]) 8 9 10 1 Swedish Institute of Space Physics, Box 812, Kiruna, SE-98128, Sweden 11 2 Space Physics Laboratory, Vikram Sarabhai Space Center, Trivandrum 695 022, India 12 3 Physikalisches Institut, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland 13 4 Institute of Space and Astronautical Science, 3-1-1 Yoshinodai, Sagamihara, Japan 14 Index Terms 15 6250 Moon 16 5421 Interactions with particles and fields 17 2780 Magnetospheric Physics: Solar wind interactions with unmagnetized bodies 18 7807 Space Plasma Physics: Charged particle motion and acceleration 19 Abstract 20 Significant proton fluxes were detected in the near wake region of the Moon by an ion mass 21 spectrometer on board Chandrayaan-1. The energy of these nightside protons is slightly higher than 22 the energy of the solar wind protons. The protons are detected close to the lunar equatorial plane at 23 a 140˚ solar zenith angle, i.e., ~50˚ behind the terminator at a height of 100 km. The protons come 24 from just above the local horizon, and move along the magnetic field in the solar wind reference 25 frame.
    [Show full text]
  • Global Mapping of Elemental Abundance on Lunar Surface by SELENE Gamma-Ray Spectrometer
    Lunar and Planetary Science XXXVI (2005) 2092.pdf Global Mapping of elemental abundance on lunar surface by SELENE gamma-ray spectrometer. 1M. -N. Kobayashi, 1A. A. Berezhnoy, 6C. d’Uston, 1M. Fujii, 1N. Hasebe, 3T. Hiroishi, 4H. Kaneko, 1T. Miyachi, 5K. Mori, 6S. Maurice, 4M. Nakazawa, 3K. Narasaki, 1O. Okudaira, 1E. Shibamura, 2T. Takashima, 1N. Yamashita, 1Advanced Research Institute of Sci.& Eng., Waseda Univ., 3-4-1, Okubo, Shinjuku-ku, Tokyo, 169-8555, Japan, (masa- [email protected]), 2Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3-1-1 Yoshinodai, Sagamihara, Kanagawa, 229-8510, 3Niihama Works, Sumitomo Heavy Industry Ltd., Niihama, Ehime, Japan, Moriya Works, 4Meisei Electric Co., Ltd., 3-249-1, Yuri-ga-oka, Moriya-shi, Ibaraki, 302-0192, 5Clear Pulse Co., 6-25-17, Chuo, Ohta-ku, Tokyo, Japan, 143-0024, 6Centre d’Etude Spatiale des Rayonnements, CNRS/UPS, Colonel Roche, B.P 4346, France. Introduction: Elemental composition on the sur- face of a planet is very important information for solv- ing the origin and the evolution of the planet and also very necessary for understanding the origin and the evolution of solar system. Planetary gamma-ray spec- troscopy is extremely powerful approach for the ele- mental composition measurement. Gamma-ray spec- trometer (GRS) will be on board SELENE, advanced lunar polar orbiter, and employ a large-volume Ge detector of 252cc as the main detector [1]. SELENE GRS is, therefore, approximately twice more sensitiv- ity than Lunar Prospector GRS, four times more sensi- Figure 1: The schematic drawing of SELENE Gamma- tive than APOLLO GRS.
    [Show full text]
  • Mission Design for the Lunar Reconnaissance Orbiter
    AAS 07-057 Mission Design for the Lunar Reconnaissance Orbiter Mark Beckman Goddard Space Flight Center, Code 595 29th ANNUAL AAS GUIDANCE AND CONTROL CONFERENCE February 4-8, 2006 Sponsored by Breckenridge, Colorado Rocky Mountain Section AAS Publications Office, P.O. Box 28130 - San Diego, California 92198 AAS-07-057 MISSION DESIGN FOR THE LUNAR RECONNAISSANCE ORBITER † Mark Beckman The Lunar Reconnaissance Orbiter (LRO) will be the first mission under NASA’s Vision for Space Exploration. LRO will fly in a low 50 km mean altitude lunar polar orbit. LRO will utilize a direct minimum energy lunar transfer and have a launch window of three days every two weeks. The launch window is defined by lunar orbit beta angle at times of extreme lighting conditions. This paper will define the LRO launch window and the science and engineering constraints that drive it. After lunar orbit insertion, LRO will be placed into a commissioning orbit for up to 60 days. This commissioning orbit will be a low altitude quasi-frozen orbit that minimizes stationkeeping costs during commissioning phase. LRO will use a repeating stationkeeping cycle with a pair of maneuvers every lunar sidereal period. The stationkeeping algorithm will bound LRO altitude, maintain ground station contact during maneuvers, and equally distribute periselene between northern and southern hemispheres. Orbit determination for LRO will be at the 50 m level with updated lunar gravity models. This paper will address the quasi-frozen orbit design, stationkeeping algorithms and low lunar orbit determination. INTRODUCTION The Lunar Reconnaissance Orbiter (LRO) is the first of the Lunar Precursor Robotic Program’s (LPRP) missions to the moon.
    [Show full text]
  • Planetary Science
    Mission Directorate: Science Theme: Planetary Science Theme Overview Planetary Science is a grand human enterprise that seeks to discover the nature and origin of the celestial bodies among which we live, and to explore whether life exists beyond Earth. The scientific imperative for Planetary Science, the quest to understand our origins, is universal. How did we get here? Are we alone? What does the future hold? These overarching questions lead to more focused, fundamental science questions about our solar system: How did the Sun's family of planets, satellites, and minor bodies originate and evolve? What are the characteristics of the solar system that lead to habitable environments? How and where could life begin and evolve in the solar system? What are the characteristics of small bodies and planetary environments and what potential hazards or resources do they hold? To address these science questions, NASA relies on various flight missions, research and analysis (R&A) and technology development. There are seven programs within the Planetary Science Theme: R&A, Lunar Quest, Discovery, New Frontiers, Mars Exploration, Outer Planets, and Technology. R&A supports two operating missions with international partners (Rosetta and Hayabusa), as well as sample curation, data archiving, dissemination and analysis, and Near Earth Object Observations. The Lunar Quest Program consists of small robotic spacecraft missions, Missions of Opportunity, Lunar Science Institute, and R&A. Discovery has two spacecraft in prime mission operations (MESSENGER and Dawn), an instrument operating on an ESA Mars Express mission (ASPERA-3), a mission in its development phase (GRAIL), three Missions of Opportunities (M3, Strofio, and LaRa), and three investigations using re-purposed spacecraft: EPOCh and DIXI hosted on the Deep Impact spacecraft and NExT hosted on the Stardust spacecraft.
    [Show full text]
  • The Lunar Dust-Plasma Environment Is Crucial
    TheThe LunarLunar DustDust --PlasmaPlasma EnvironmentEnvironment Timothy J. Stubbs 1,2 , William M. Farrell 2, Jasper S. Halekas 3, Michael R. Collier 2, Richard R. Vondrak 2, & Gregory T. Delory 3 [email protected] Lunar X-ray Observatory(LXO)/ Magnetosheath Explorer (MagEX) meeting, Hilton Garden Inn, October 25, 2007. 1 University of Maryland, Baltimore County 2 NASA Goddard Space Flight Center 3 University of California, Berkeley TheThe ApolloApollo AstronautAstronaut ExperienceExperience ofof thethe LunarLunar DustDust --PlasmaPlasma EnvironmentEnvironment “… one of the most aggravating, restricting facets of lunar surface exploration is the dust and its adherence to everything no matter what kind of material, whether it be skin, suit material, metal, no matter what it be and it’s restrictive friction-like action to everything it gets on. ” Eugene Cernan, Commander Apollo 17. EvidenceEvidence forfor DustDust AboveAbove thethe LunarLunar SurfaceSurface Horizon glow from forward scattered sunlight • Dust grains with radius of 5 – 6 m at about 10 to 30 cm from the surface, where electrostatic and gravitational forces balance. • Horizon glow ~10 7 too bright to be explained by micro-meteoroid- generated ejecta [Zook et al., 1995]. Composite image of morning and evening of local western horizon [Criswell, 1973]. DustDust ObservedObserved atat HighHigh AltitudesAltitudes fromfrom OrbitOrbit Schematic of situation consistent with Apollo 17 observations [McCoy, 1976]. Lunar dust at high altitudes (up to ~100 km). 0.1 m-scale dust present Gene Cernan sketches sporadically (~minutes). [McCoy and Criswell, 1974]. InIn --SituSitu EvidenceEvidence forfor DustDust TransportTransport Terminators Berg et al. [1976] Apollo 17 Lunar Ejecta and Meteorites (LEAM) experiment. PossiblePossible DustyDusty HorizonHorizon GlowGlow seenseen byby ClementineClementine StarStar Tracker?Tracker? Above: image of possible horizon glow above the lunar surface.
    [Show full text]
  • The Moon and Eclipses
    Lecture 10 The Moon and Eclipses Jiong Qiu, MSU Physics Department Guiding Questions 1. Why does the Moon keep the same face to us? 2. Is the Moon completely covered with craters? What is the difference between highlands and maria? 3. Does the Moon’s interior have a similar structure to the interior of the Earth? 4. Why does the Moon go through phases? At a given phase, when does the Moon rise or set with respect to the Sun? 5. What is the difference between a lunar eclipse and a solar eclipse? During what phases do they occur? 6. How often do lunar eclipses happen? When one is taking place, where do you have to be to see it? 7. How often do solar eclipses happen? Why are they visible only from certain special locations on Earth? 10.1 Introduction The moon looks 14% bigger at perigee than at apogee. The Moon wobbles. 59% of its surface can be seen from the Earth. The Moon can not hold the atmosphere The Moon does NOT have an atmosphere and the Moon does NOT have liquid water. Q: what factors determine the presence of an atmosphere? The Moon probably formed from debris cast into space when a huge planetesimal struck the proto-Earth. 10.2 Exploration of the Moon Unmanned exploration: 1950, Lunas 1-3 -- 1960s, Ranger -- 1966-67, Lunar Orbiters -- 1966-68, Surveyors (first soft landing) -- 1966-76, Lunas 9-24 (soft landing) -- 1989-93, Galileo -- 1994, Clementine -- 1998, Lunar Prospector Achievement: high-resolution lunar surface images; surface composition; evidence of ice patches around the south pole.
    [Show full text]
  • Lunar Occultation Observer (LOCO)
    Ex Luna, Scientia From the Moon, Knowledge Lunar Occultation Observer (LOCO) A Nuclear Astrophysics All-Sky Survey Mission Concept using the Moon as a Platform for Science A White Paper Submission to Planetary Science Decadal Survey April 1, 2009 Contact: RICHARD S. MILLER University of Alabama in Huntsville [email protected] (256) 824-2454 M. Bonamente, S. O’Brien, W. S. Paciesas University of Alabama in Huntsville D. J. Lawrence Johns Hopkins University/Applied Physics Laboratory C. A. Young ADNET Systems/NASA-GSFC D. Ebbets Ball Aerospace R.S. Miller, UAH Lunar Occultation Observer (LOCO) Ex Luna, Scientia From the Moon, Knowledge Summary The long-term goal of our program is the development of a next-generation mission capable of surveying the Cosmos in the nuclear regime (~0.02-10 MeV). The Lunar Occultation Observer (LOCO) [1-3] is a new γ-ray astrophysics mission concept having unprecedented flux sensitivity, high spectral resolution, excellent spatial resolution, and very uniform sky coverage. It meets or exceeds the capabilities required of the next-generation nuclear astrophysics mission, and is therefore capable of addressing multiple high-priority science goals. LOCO will be a pioneering mission in high-energy astrophysics: the first to utilize the moon as a scientific platform, and the first to successfully employ occultation imaging as the principle detec- tion method. This is a powerful, yet relatively simple, approach to imaging in regimes where traditional imaging approaches are inappropriate, complex, or cost prohibitive. Specifically, LOCO will utilize the Lunar Occultation Technique (LOT) - the temporal modulation of source fluxes as the are repeatedly occulted by the Moon - to detect and image both point- and extended-sources.
    [Show full text]
  • 02. Solar System (2001) 9/4/01 12:28 PM Page 2
    01. Solar System Cover 9/4/01 12:18 PM Page 1 National Aeronautics and Educational Product Space Administration Educators Grades K–12 LS-2001-08-002-HQ Solar System Lithograph Set for Space Science This set contains the following lithographs: • Our Solar System • Moon • Saturn • Our Star—The Sun • Mars • Uranus • Mercury • Asteroids • Neptune • Venus • Jupiter • Pluto and Charon • Earth • Moons of Jupiter • Comets 01. Solar System Cover 9/4/01 12:18 PM Page 2 NASA’s Central Operation of Resources for Educators Regional Educator Resource Centers offer more educators access (CORE) was established for the national and international distribution of to NASA educational materials. NASA has formed partnerships with universities, NASA-produced educational materials in audiovisual format. Educators can museums, and other educational institutions to serve as regional ERCs in many obtain a catalog and an order form by one of the following methods: States. A complete list of regional ERCs is available through CORE, or electroni- cally via NASA Spacelink at http://spacelink.nasa.gov/ercn NASA CORE Lorain County Joint Vocational School NASA’s Education Home Page serves as a cyber-gateway to informa- 15181 Route 58 South tion regarding educational programs and services offered by NASA for the Oberlin, OH 44074-9799 American education community. This high-level directory of information provides Toll-free Ordering Line: 1-866-776-CORE specific details and points of contact for all of NASA’s educational efforts, Field Toll-free FAX Line: 1-866-775-1460 Center offices, and points of presence within each State. Visit this resource at the E-mail: [email protected] following address: http://education.nasa.gov Home Page: http://core.nasa.gov NASA Spacelink is one of NASA’s electronic resources specifically devel- Educator Resource Center Network (ERCN) oped for the educational community.
    [Show full text]
  • Stationkeeping for the Lunar Reconnaissance Orbiter (Lro)
    https://ntrs.nasa.gov/search.jsp?R=20080012683 2019-08-29T19:07:49+00:00Z View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by NASA Technical Reports Server STATIONKEEPING FOR THE LUNAR RECONNAISSANCE ORBITER (LRO) Mark Beckman 1 and Rivers Lamb 2 The Lunar Reconnaissance Orbiter (LRO) is scheduled to launch in 2008 as the first mission under NASA’s Vision for Space Exploration. Following several weeks in a quasi-frozen commissioning orbit, LRO will fly in a 50 km mean altitude lunar polar orbit. During the one year mission duration, the orbital dynamics of a low lunar orbit force LRO to perform periodic sets of stationkeeping maneuvers. This paper explores the characteristics of low lunar orbits and explains how the LRO stationkeeping plan is designed to accommodate the dynamics in such an orbit. The stationkeeping algorithm used for LRO must meet five mission constraints. These five constraints are to maintain ground station contact during maneuvers, to control the altitude variation of the orbit, to distribute periselene equally between northern and southern hemispheres, to match eccentricity at the beginning and the end of the sidereal period, and to minimize stationkeeping ∆V. This paper addresses how the maneuver plan for LRO is designed to meet all of the above constraints. INTRODUCTION The Lunar Reconnaissance Orbiter (LRO) is the first mission under NASA’s Vision for Space Exploration. LRO will launch on an Atlas V launch vehicle in late 2008 using a direct minimum energy transfer to reach the moon. The spacecraft has a one year mission duration in a low lunar polar orbit.
    [Show full text]
  • Physics of Solar Wind and Terrestrial Magnetospheric Plasma Interactions with the Moon
    Physics of Solar Wind and Terrestrial Magnetospheric Plasma Interactions With the Moon R.P. Lin Physics Dept & Space Sciences Laboratory University of California, Berkeley with help from J. Halekas, M. Oieroset, & M. Fillingim Plasma Interaction with the Moon and Dust Plasma Physics of the Distant Magnetotail Plasma Interaction with Mini-Magnetospheres The Lunar Environment Dipolar E-Fields? Extreme Surface Charging Surface potentials of up to several kV (negative) found: • In the terrestrial plasmasheet, where 4 KeV Beam we encounter high plasma temperature. • During Solar Energetic Particle events Frequency of Extreme Charging Events During the Entire Lunar Prospector Mission • Green in color bar indicates magnetospheric tail passages, red indicates major SEP events The Earth’s magnetic shield DuringBefore reconnectionreconnection Dungey, Philos. Mag. 55, (1953) Wind observed 10 hours of reconnection flows at lunar distance (XGSE=-60 RE) lobe NP plasma Wind alternately inside plasma sheet sheet and lobe High speed reconnection flows always TP observed when the spacecraft was in the plasma sheet → 10 hours of continuous reconnection VX High speed Reconnection flows Bx Bz B (GSM) (Oieroset et al., 2000) By Wind satellite observations in distant magnetotail, 60RE • Measurements within the ion diffusion region reveal: Strong anisotropy in fe. Log(f) M. Øieroset et al. Nature 412, (2001) M. Øieroset et al. PRL 89, (2002) A trapped electron in the magnetotail mv 2 m(v2 - v 2 ) The magnetic moment: µ = ! = || 2B 2B Drift kinetic modeling of Wind data • Applying f(x0,v0) = f∞(|v1|) to an X-line geometry consistent with the Wind measurements • A potential,Φ∞ needed for trapping at low energies • Ion outflow: 400 km/s, consistent with acceleration in Φ ∞ ~ -300V Φ∞ Theory Wind Φ∞~ -800V Φ∞~ -1150V J.
    [Show full text]