Astrobiology in Low Earth Orbit
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Global Ionosphere-Thermosphere-Mesosphere (ITM) Mapping Across Temporal and Spatial Scales a White Paper for the NRC Decadal
Global Ionosphere-Thermosphere-Mesosphere (ITM) Mapping Across Temporal and Spatial Scales A White Paper for the NRC Decadal Survey of Solar and Space Physics Andrew Stephan, Scott Budzien, Ken Dymond, and Damien Chua NRL Space Science Division Overview In order to fulfill the pressing need for accurate near-Earth space weather forecasts, it is essential that future measurements include both temporal and spatial aspects of the evolution of the ionosphere and thermosphere. A combination of high altitude global images and low Earth orbit altitude profiles from simple, in-the-medium sensors is an optimal scenario for creating continuous, routine space weather maps for both scientific and operational interests. The method presented here adapts the vast knowledge gained using ultraviolet airglow into a suggestion for a next-generation, near-Earth space weather mapping network. Why the Ionosphere, Thermosphere, and Mesosphere? The ionosphere-thermosphere-mesosphere (ITM) region of the terrestrial atmosphere is a complex and dynamic environment influenced by solar radiation, energy transfer, winds, waves, tides, electric and magnetic fields, and plasma processes. Recent measurements showing how coupling to other regions also influences dynamics in the ITM [e.g. Immel et al., 2006; Luhr, et al, 2007; Hagan et al., 2007] has exposed the need for a full, three- dimensional characterization of this region. Yet the true level of complexity in the ITM system remains undiscovered primarily because the fundamental components of this region are undersampled on the temporal and spatial scales that are necessary to expose these details. The solar and space physics research community has been driven over the past decade toward answering scientific questions that have a high level of practical application and relevance. -
Marina Galand
Thermosphere - Ionosphere - Magnetosphere Coupling! Canada M. Galand (1), I.C.F. Müller-Wodarg (1), L. Moore (2), M. Mendillo (2), S. Miller (3) , L.C. Ray (1) (1) Department of Physics, Imperial College London, London, U.K. (2) Center for Space Physics, Boston University, Boston, MA, USA (3) Department of Physics and Astronomy, University College London, U.K. 1." Energy crisis at giant planets Credit: NASA/JPL/Space Science Institute 2." TIM coupling Cassini/ISS (false color) 3." Modeling of IT system 4." Comparison with observaons Cassini/UVIS 5." Outstanding quesAons (Pryor et al., 2011) SATURN JUPITER (Gladstone et al., 2007) Cassini/UVIS [UVIS team] Cassini/VIMS (IR) Credit: J. Clarke (BU), NASA [VIMS team/JPL, NASA, ESA] 1. SETTING THE SCENE: THE ENERGY CRISIS AT THE GIANT PLANETS THERMAL PROFILE Exosphere (EARTH) Texo 500 km Key transiLon region Thermosphere between the space environment and the lower atmosphere Ionosphere 85 km Mesosphere 50 km Stratosphere ~ 15 km Troposphere SOLAR ENERGY DEPOSITION IN THE UPPER ATMOSPHERE Solar photons ion, e- Neutral Suprathermal electrons B ion, e- Thermal e- Ionospheric Thermosphere Ne, Nion e- heang Te P, H * + Airglow Neutral atmospheric Exothermic reacAons heang IS THE SUN THE MAIN ENERGY SOURCE OF PLANERATY THERMOSPHERES? W Main energy source: UV solar radiaon Main energy source? EartH Outer planets CO2 atmospHeres Exospheric temperature (K) [aer Mendillo et al., 2002] ENERGY CRISIS AT THE GIANT PLANETS Observed values at low to mid-latudes solsce equinox Modeled values (Sun only) [Aer -
FASTSAT a Mini-Satellite Mission…..A Way Ahead”
Proposed Abstract: Under the combined Category and Title: “FASTSAT a Mini-Satellite Mission…..A Way Ahead” Authors: Mark E. Boudreaux, Joseph Casas, Timothy A. Smith The Fast Affordable Science and Technology Spacecraft (FASTSAT) is a mini-satellite weighing less than 150 kg. FASTSAT was developed as government-industry collaborative research and development flight project targeting rapid access to space to provide an alternative, low cost platform for a variety of scientific, research, and technology payloads. The initial spacecraft was designed to carry six instruments and launch as a secondary “rideshare” payload. This design approach greatly reduced overall mission costs while maximizing the on-board payload accommodations. FASTSAT was designed from the ground up to meet a challenging short schedule using modular components with a flexible, configurable layout to enable a broad range of payloads at a lower cost and shorter timeline than scaling down a more complex spacecraft. The integrated spacecraft along with its payloads were readied for launch 15 months from authority to proceed. As an ESPA-class spacecraft, FASTSAT is compatible with many different launch vehicles, including Minotaur I, Minotaur IV, Delta IV, Atlas V, Pegasus, Falcon 1/1e, and Falcon 9. These vehicles offer an array of options for launch sites and provide for a variety of rideshare possibilities. FASTSAT a Mini Satellite Mission …..A Way Ahead 15th Annual Space & Missile Defense Conference Session Track 1.2 : Operations for Small, Tactical Satellites Mark Boudreaux/NASA -
Thermosphere? Why Is It So Hot? Atmosphere Model and Thermosphere 5
UNIT 6, LESSON 1: EARTH LAYERS & ATMOSPHERE LET’S BUILD OUR EARTH AND THE ATMOSPHERE 1 & 2 Where is earth’s crust? What is the difference between the 1. Read/annotate the oceanic and continental crust? paragraph(s) Crust and Mantle Where is the earth’s mantle? What is a plate? What part of the 2. Answer the questions mantle is below the plates? that go with the 3 Where is the earth’s core? How is the core similar to the mantle? paragraph(s) Core 4 & 5 Where is the troposphere? What are you likely to find there? Name at least 3 things. 3. Show Mrs. Stoddard Troposphere and Stratosphere your answers Where is the stratosphere? Why would the air be warm in the 4. If you get it correct, get stratosphere? Where is the mesosphere? Why do meteors burn in this layer? a piece of your 6 & 7 Mesosphere Where is the thermosphere? Why is it so hot? atmosphere model And Thermosphere 5. Repeat until your 8 Where is the exosphere? Why do some experts ignore the exosphere and think the thermosphere is the outermost layer of Exosphere model is finished! the earth’s atmosphere? CHECK YOUR MODEL! Exosphere Thermosphere Mesosphere Stratosphere Troposphere Core Name Class Period Mantle Crust HOW DID WE DO ON THE ATMOSPHERE MODEL? LET’S SET UP OUR JOURNALS! Earth’s Layers and Atmosphere 1:301:291:281:271:261:251:241:231:221:211:201:191:181:171:161:151:141:131:121:111:101:091:081:071:061:051:041:031:021:011:000:590:580:570:560:550:540:530:520:510:500:490:480:470:460:450:440:430:420:410:400:390:380:370:360:350:340:330:320:310:300:290:280:270:260:250:240:230:220:210:200:190:180:170:160:150:140:130:120:110:100:090:080:070:060:050:040:030:020:01End -
Highlights in Space 2010
International Astronautical Federation Committee on Space Research International Institute of Space Law 94 bis, Avenue de Suffren c/o CNES 94 bis, Avenue de Suffren UNITED NATIONS 75015 Paris, France 2 place Maurice Quentin 75015 Paris, France Tel: +33 1 45 67 42 60 Fax: +33 1 42 73 21 20 Tel. + 33 1 44 76 75 10 E-mail: : [email protected] E-mail: [email protected] Fax. + 33 1 44 76 74 37 URL: www.iislweb.com OFFICE FOR OUTER SPACE AFFAIRS URL: www.iafastro.com E-mail: [email protected] URL : http://cosparhq.cnes.fr Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law The United Nations Office for Outer Space Affairs is responsible for promoting international cooperation in the peaceful uses of outer space and assisting developing countries in using space science and technology. United Nations Office for Outer Space Affairs P. O. Box 500, 1400 Vienna, Austria Tel: (+43-1) 26060-4950 Fax: (+43-1) 26060-5830 E-mail: [email protected] URL: www.unoosa.org United Nations publication Printed in Austria USD 15 Sales No. E.11.I.3 ISBN 978-92-1-101236-1 ST/SPACE/57 *1180239* V.11-80239—January 2011—775 UNITED NATIONS OFFICE FOR OUTER SPACE AFFAIRS UNITED NATIONS OFFICE AT VIENNA Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law Progress in space science, technology and applications, international cooperation and space law UNITED NATIONS New York, 2011 UniTEd NationS PUblication Sales no. -
The O/OREOS Mission—Astrobiology in Low Earth Orbit
Acta Astronautica 93 (2014) 501–508 Contents lists available at ScienceDirect Acta Astronautica journal homepage: www.elsevier.com/locate/actaastro The O/OREOS mission—Astrobiology in low Earth orbit P. Ehrenfreund a,n, A.J. Ricco b, D. Squires b, C. Kitts c, E. Agasid b, N. Bramall b, K. Bryson d, J. Chittenden b, C. Conley e, A. Cook b, R. Mancinelli d, A. Mattioda b, W. Nicholson f, R. Quinn g, O. Santos b,G.Tahue,M.Voyteke, C. Beasley b,L.Bicac, M. Diaz-Aguado b, C. Friedericks b,M.Henschkeb,D.Landish, E. Luzzi b,D.Lyb, N. Mai b, G. Minelli b,M.McIntyreb,M.Neumannc, M. Parra b, M. Piccini b, R. Rasay c,R.Ricksb, A. Schooley b, E. Stackpole b, L. Timucin b,B.Yostb, A. Young c a Space Policy Institute, Washington DC, USA b NASA Ames Research Center, Moffett Field, CA, USA c Robotic Systems Laboratory, Santa Clara University, Santa Clara, CA, USA d Bay Area Environmental Research Institute, Sonoma, CA, USA e NASA Headquarters, Washington DC, USA f University of Florida, Gainesville, FL, USA g SETI Institute, Mountain View, CA, USA h Draper Laboratory, Cambridge, MA, USA article info abstract Article history: The O/OREOS (Organism/Organic Exposure to Orbital Stresses) nanosatellite is the first Received 19 December 2011 science demonstration spacecraft and flight mission of the NASA Astrobiology Small- Received in revised form Payloads Program (ASP). O/OREOS was launched successfully on November 19, 2010, to 22 June 2012 a high-inclination (721), 650-km Earth orbit aboard a US Air Force Minotaur IV rocket Accepted 18 September 2012 from Kodiak, Alaska. -
Diffuse Electron Precipitation in Magnetosphere-Ionosphere- Thermosphere Coupling
EGU21-6342 https://doi.org/10.5194/egusphere-egu21-6342 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Diffuse electron precipitation in magnetosphere-ionosphere- thermosphere coupling Dong Lin1, Wenbin Wang1, Viacheslav Merkin2, Kevin Pham1, Shanshan Bao3, Kareem Sorathia2, Frank Toffoletto3, Xueling Shi1,4, Oppenheim Meers5, George Khazanov6, Adam Michael2, John Lyon7, Jeffrey Garretson2, and Brian Anderson2 1High Altitude Observatory, National Center for Atmospheric Research, Boulder CO, United States of America 2Applied Physics Laboratory, Johns Hopkins University, Laurel MD, USA 3Department of Physics and Astronomy, Rice University, Houston TX, USA 4Bradley Department of Electrical and Computer Engineering, Virginia Tech, Blacksburg VA, USA 5Astronomy Department, Boston University, Boston MA, USA 6Goddard Space Flight Center, NASA, Greenbelt MD, USA 7Department of Physics and Astronomy, Dartmouth College, Hanover NH, USA Auroral precipitation plays an important role in magnetosphere-ionosphere-thermosphere (MIT) coupling by enhancing ionospheric ionization and conductivity at high latitudes. Diffuse electron precipitation refers to scattered electrons from the plasma sheet that are lost in the ionosphere. Diffuse precipitation makes the largest contribution to the total precipitation energy flux and is expected to have substantial impacts on the ionospheric conductance and affect the electrodynamic coupling between the magnetosphere and ionosphere-thermosphere. -
120 Application of Nanosatellites in the Near
SES 2013 Ninth Scientific Conference with International Participation SPACE, ECOLOGY, SAFETY 20 – 22 November 2013, Sofia, Bulgaria APPLICATION OF NANOSATELLITES IN THE NEAR-EARTH SPACE INVESTIGATION Daniela Boneva1, Lachezar Filipov1, Krasimira Yankova1, Deyan Gotchev1, Zhivko Zhelezov2, Georgi Chamov2, Mariya Bivolarska2, Spaska Yaneva2 1Space Research and Technology Institute – Bulgarian Academy of Sciences 2Space Research Ltd e-mail: [email protected], [email protected], [email protected], [email protected] [email protected], [email protected] Keywords: Nanosatellites; Near-Earth Space; Zodiacal Light; Abstract: We present based characteristics of the nanosatellites’ equipment and we point to the advantages of their usage. The purpose of this paper is to survey the applications of nanosatellites as a new and advanced technology. It is reviewed the most employable of them in space science and technology. We present the conception of our new project that will investigate the polarimetry of the Zodiacal light on a Sun-synchronous low Earth orbit. ПРИЛОЖЕНИЕ НА НАНОСАТЕЛИТИ В ИЗСЛЕДВАНЕТО НА БЛИЗКИЯ КОСМОС Даниела Бонева1, Лъчезар Филипов1, Красимира Янкова1, Деян Гочев1, Живко Железов2, Георги Чамов2, Мария Биволарска2, Спаска Янева2 1Институт за космически изследвания и технологии – Българска академия на науките 2Спейс рисърч ООД e-mail: [email protected], [email protected], [email protected], [email protected] [email protected], [email protected] Ключови думи: Наносателити;Близък космос;Зодиакална светлина; Резюме: Представени са основни характеристики на наносателитите и са посочени предимствата на използването им. Целта на тази статия е да се проучат приложенията на наносателитите като нова и напреднала технология. Разгледани са най-пригодни за заетост от тях в областта на космическите науки и технологии. -
A Breath of Fresh Air: Air-Scooping Electric Propulsion in Very Low Earth Orbit
A BREATH OF FRESH AIR: AIR-SCOOPING ELECTRIC PROPULSION IN VERY LOW EARTH ORBIT Rostislav Spektor and Karen L. Jones Air-scooping electric propulsion (ASEP) is a game-changing concept that extends the lifetime of very low Earth orbit (VLEO) satellites by providing periodic reboosting to maintain orbital altitudes. The ASEP concept consists of a solar array-powered space vehicle augmented with electric propulsion (EP) while utilizing ambient air as a propellant. First proposed in the 1960s, ASEP has attracted increased interest and research funding during the past decade. ASEP technology is designed to maintain lower orbital altitudes, which could reduce latency for a communication satellite or increase resolution for a remote sensing satellite. Furthermore, an ASEP space vehicle that stores excess gas in its fuel tank can serve as a reusable space tug, reducing the need for high-power chemical boosters that directly insert satellites into their final orbit. Air-breathing propulsion can only work within a narrow range of operational altitudes, where air molecules exist in sufficient abundance to provide propellant for the thruster but where the density of these molecules does not cause excessive drag on the vehicle. Technical hurdles remain, such as how to optimize the air-scoop design and electric propulsion system. Also, the corrosive VLEO atmosphere poses unique challenges for material durability. Despite these difficulties, both commercial and government researchers are making progress. Although ASEP technology is still immature, it is on the cusp of transitioning between research and development and demonstration phases. This paper describes the technical challenges, innovation leaders, and potential market evolution as satellite operators seek ways to improve performance and endurance. -
Small Satellite Doldrums
25 Years of Small Satellites AC4/5 MISSION Siegfried Janson The Aerospace Corporation Presented August 9, 2011 © The Aerospace© The Aerospace Corporation Corporation 2010 2011 Microsatellite Launch History: Last 25 years Microsatellite launch rates rose rapidly in the early 1960’s, and peaked in 1965. Non-Strela microsatellite launch rates hit bottom from 1977 to 1987; the “Small 2 Satellite Doldrums”. They’ve recovered over the past 25 years. Nanosatellite Launch History: About 3 nanosatellites were launched per year during the first decade of space exploration. Launch rates hit zero between 1972 to 1989, but stabilized at ~2 per year 3 through 2002. The CubeSat paradigm has enabled a rapid rise in launch rates. Picosatellite Launch History: Only two active picosatellites were flown before 2000. The Stanford Orbiting Picosatellite Automated Launcher (OPAL) ejected 6 picosatellites into orbit, kicking- st 4 off a 21 century return of picosatellites and the CubeSat Era. Small Satellite Launch History: The First 30 years • The 1960’s: Boom and Bust - Small satellite launch rates rapidly increase in early 1960’s as the Space Age unfolds - Small satellite launch rates decrease in latter half of decade as launch vehicle throw weight capability increases and satellites get bigger (on average). • The 1970’s: Soviet Microsatellites Dominate - Strela-1M constellation deployed; it eventually requires over 300 spacecraft - Western small satellite launch rates continue to decline as satellites grow in size • The 1980’s: Small Satellite Doldrums (1977-1987) - No nanosatellites or picosatellites launched - Less than 5 Western microsatellites launched per year - DARPA initiates LightSat program; holds workshop in 1987 - First AIAA/USU Small Satellite Conference in 1987 - “Doldrums” end in 1987 By 1986, the Soviet Union was actively launching military communications microsatellites, but the rest of the world was experiencing a dearth of new small 5 satellites. -
The Marshall Engineering Thermosphere (MET) Model Volume H Technical Description
NASA / CR--1998-207946 The Marshall Engineering Thermosphere (MET) Model Volume h Technical Description R.E. Smith Physitron, Inc., Huntsville, Alabama Prepared for Marshall Space Flight Center under Contract NAS8-38333 National Aeronautics and Space Administration Marshall Space Flight Center May 1998 EXECUTIVE SUMMARY Volume I of this report presents a technical description of the Marshall Engineering Thermosphere (MET) model atmosphere and a summary of its historical development. Vari- ous programs developed to augment the original capability of the model are discussed in de- tail. The report also describes each of the individual subroutines developed to enhance the model. Computer codes for these subroutines are contained in four appendices. Volume II contains a copy of each of the reference documents. If you have questions or comments or need to request additional information, contact the Chief, Electromagnetics and Aerospace Environments Branch, Systems Analysis and Inte- gration Laboratory, MSFC, AL 35812. iii TABLE OF CONTENTS Section Title I INTRODUCTION ......................................................................................................... 1 II SCOPE ........................................................................................................................... 1 HI DESCRIPTION OF THE NEUTRAL THERMOSPHERE .......................................... 1 A. Variations ............................................................................................................ 1 B. Solar Activity Parameters -
The Dynamics and Control of the Cubesail Mission — a Solar Sailing
© 2010 Andrzej Pukniel. THE DYNAMICS AND CONTROL OF THE CUBESAIL MISSION—A SOLAR SAILING DEMONSTRATION BY ANDRZEJ PUKNIEL DISSERTATION Submitted in partial fulfillment of the requirements for the degree of Doctor in Philosophy in Aerospace Engineering in the Graduate College of the University of Illinois at Urbana-Champaign, 2010 Urbana, Illinois Doctoral Committee: Professor Victoria Coverstone, Chair Professor John Prussing Professor Rodney Burton Professor Gary Swenson ABSTRACT The proposed study addresses two issues related to the slow emergence of solar sailing as a viable space propulsion method. The low technology readiness level and complications related to stowage, deployment, and support of the sail structure are both addressed by combining the CU Aerospace and University of Illinois-developed UltraSail and CubeSat expertise to design a small-scale solar sail deployment and propulsion experiment in low Earth orbit. The study analyzes multiple aspects of the problem from initial sizing and packaging of the solar sail film into two CubeSat-class spacecraft, through on-orbit deployment dynamics, attitude control of large and flexible space structure, and predictions of performance and orbital maneuvering capability. ii ACKNOWLEDGEMENTS The following work would have not been possible without the continuous support and encouragement of my advisor, Professor Coverstone. Her patience, scientific insight, and enthusiasm are a rare combination that fosters a unique research environment. It allows the students to develop both as highly competent engineers as well as young individuals. Few advisors sincerely care for their students’ personal development as much as Professor Coverstone and I consider myself privileged to be part of her research group. I would also like to thank Professors Rod Burton and Gary Swenson as well as Dr.