Solar Wind, Energetic Particles & Dust
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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. -
New Horizons: Reconnaissance of the Pluto-Charon System and The
C.T. Russell Editor New Horizons Reconnaissance of the Pluto-Charon System and the Kuiper Belt Previously published in Space Science Reviews Volume 140, Issues 1–4, 2008 C.T. Russell Institute of Geophysics & Planetary Physics University of California Los Angeles, CA, USA Cover illustration: NASA’s New Horizons spacecraft was launched on 2006 January 19, received a grav- ity assist during a close approach to Jupiter on 2007 February 28, and is now headed for a flyby with closest approach 12,500 km from the center of Pluto on 2015 July 14. This artist’s depiction shows the spacecraft shortly after passing above Pluto’s highly variegated surface, which may have black-streaked surface deposits produced from cryogenic geyser activity, and just before passing into Pluto’s shadow when solar and earth occultation experiments will probe Pluto’s tenuous, and possibly hazy, atmosphere. Sunlit crescents of Pluto’s moons Charon, Nix, and Hydra are visible in the background. After flying through the Pluto system, the New Horizons spacecraft could be re-targeted towards other Kuiper Belt Objects in an extended mission phase. This image is based on an original painting by Dan Durda. © Dan Durda 2001 All rights reserved. Back cover illustration: The New Horizons spacecraft was launched aboard an Atlas 551 rocket from the NASA Kennedy Space Center on 2008 January 19 at 19:00 UT. Library of Congress Control Number: 2008944238 DOI: 10.1007/978-0-387-89518-5 ISBN-978-0-387-89517-8 e-ISBN-978-0-387-89518-5 Printed on acid-free paper. -
Measurements of the Interplanetary Dust Population by the Venetia Burney Student Dust Counter on the New Horizons Mission Andrew R
41st Lunar and Planetary Science Conference (2010) 1219.pdf Measurements of the Interplanetary Dust Population by the Venetia Burney Student Dust Counter on the New Horizons Mission Andrew R. Poppe1,2, David James1, Brian Jacobsmeyer1,2, and Mihaly Hor´anyi1,2, 1Laboratory for Atmospheric and Space Physics, Boulder, CO, and 2Department of Physics, University of Colorado, Boulder, CO, ([email protected]) Introduction: The Venetia Burney Student Dust Counter (SDC) on the New Horizons mission is an in- strument designed to measure the spatial density of in- terplanetary dust particles with mass, m > 10−12 g, on a radial profile throughout the solar system [1]. The instrument consists of fourteen permanently-polarized polyvinylidene fluoride (PVDF) detectors that register a charge when impacted by a hypervelocity(v> 1 km/sec) dust particle. PVDF-style dust detectors have previously flown on the Vega 1 and 2 [2] and Cassini spacecraft [3]. The instrument has a total surface area of 0.11 m2, a one- second time resolution and a factor of two in mass reso- lution. When impacted by a hypervelocity dust particle, the instrument records the time, charge, threshold and detector number. SDC is part of the Education and Pub- lic Outreach program of New Horizons, and as such, was designed, tested, integrated and is now operated solely by students. New Horizons was launched on January 19, 2006 and encountered Jupiter on February 28, 2007. Prior to the Jupiter encounter, SDC took measurements in two main Figure 1: The New Horizons flight path up to January 1, 2010. periods of the inner solar system: 2.66-3.55 A.U. -
Episode 2: Bodies in Orbit
Episode 2: Bodies in Orbit This transcript is based on the second episode of Moonstruck, a podcast about humans in space, produced by Dra!House Media and featuring analysis from the Center for Strategic and International Studies’ Aerospace Security Project. Listen to the full episode on iTunes, Spotify, or on our website. BY Thomas González Roberts // PUBLISHED April 4, 2018 AS A DOCENT at the Smithsonian National Air & Space But before humans could use the bathroom in space, a Museum I get a lot of questions from visitors about the lot of questions needed to be answered. Understanding grittiest details of spaceflight. While part of me wants to how human bodies respond to the environment of outer believe that everyone is looking for a thoughtful Kennedy space took years of research. It was a dark, controversial quote to drive home an analysis of the complicated period in the history of spaceflight. This is Moonstruck, a relationship between nationalism and space travel, some podcast about humans in space. I’m Thomas González people are less interested in my stories and more Roberts. interested in other, equally scholarly topics: In the late 1940s, American scientists began to focus on Kids: I have a question. What if you need to go to the two important challenges of spaceflight: solar radiation bathroom while you're in a spacesuit? Is there a special and weightlessness.1 diaper? Aren't you like still wearing the diaper when you are wearing a spacesuit? Let'sThomas start González with radiation. Roberts is the host and executive producer of Moonstruck, and a space policy Alright, alright, I get it. -
+ New Horizons
Media Contacts NASA Headquarters Policy/Program Management Dwayne Brown New Horizons Nuclear Safety (202) 358-1726 [email protected] The Johns Hopkins University Mission Management Applied Physics Laboratory Spacecraft Operations Michael Buckley (240) 228-7536 or (443) 778-7536 [email protected] Southwest Research Institute Principal Investigator Institution Maria Martinez (210) 522-3305 [email protected] NASA Kennedy Space Center Launch Operations George Diller (321) 867-2468 [email protected] Lockheed Martin Space Systems Launch Vehicle Julie Andrews (321) 853-1567 [email protected] International Launch Services Launch Vehicle Fran Slimmer (571) 633-7462 [email protected] NEW HORIZONS Table of Contents Media Services Information ................................................................................................ 2 Quick Facts .............................................................................................................................. 3 Pluto at a Glance ...................................................................................................................... 5 Why Pluto and the Kuiper Belt? The Science of New Horizons ............................... 7 NASA’s New Frontiers Program ........................................................................................14 The Spacecraft ........................................................................................................................15 Science Payload ...............................................................................................................16 -
1 the Atmosphere of Pluto As Observed by New Horizons G
The Atmosphere of Pluto as Observed by New Horizons G. Randall Gladstone,1,2* S. Alan Stern,3 Kimberly Ennico,4 Catherine B. Olkin,3 Harold A. Weaver,5 Leslie A. Young,3 Michael E. Summers,6 Darrell F. Strobel,7 David P. Hinson,8 Joshua A. Kammer,3 Alex H. Parker,3 Andrew J. Steffl,3 Ivan R. Linscott,9 Joel Wm. Parker,3 Andrew F. Cheng,5 David C. Slater,1† Maarten H. Versteeg,1 Thomas K. Greathouse,1 Kurt D. Retherford,1,2 Henry Throop,7 Nathaniel J. Cunningham,10 William W. Woods,9 Kelsi N. Singer,3 Constantine C. C. Tsang,3 Rebecca Schindhelm,3 Carey M. Lisse,5 Michael L. Wong,11 Yuk L. Yung,11 Xun Zhu,5 Werner Curdt,12 Panayotis Lavvas,13 Eliot F. Young,3 G. Leonard Tyler,9 and the New Horizons Science Team 1Southwest Research Institute, San Antonio, TX 78238, USA 2University of Texas at San Antonio, San Antonio, TX 78249, USA 3Southwest Research Institute, Boulder, CO 80302, USA 4National Aeronautics and Space Administration, Ames Research Center, Space Science Division, Moffett Field, CA 94035, USA 5The Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA 6George Mason University, Fairfax, VA 22030, USA 7The Johns Hopkins University, Baltimore, MD 21218, USA 8Search for Extraterrestrial Intelligence Institute, Mountain View, CA 94043, USA 9Stanford University, Stanford, CA 94305, USA 10Nebraska Wesleyan University, Lincoln, NE 68504 11California Institute of Technology, Pasadena, CA 91125, USA 12Max-Planck-Institut für Sonnensystemforschung, 37191 Katlenburg-Lindau, Germany 13Groupe de Spectroscopie Moléculaire et Atmosphérique, Université Reims Champagne-Ardenne, 51687 Reims, France *To whom correspondence should be addressed. -
Anticipated Scientific Investigations at the Pluto System
Space Sci Rev (2008) 140: 93–127 DOI 10.1007/s11214-008-9462-9 New Horizons: Anticipated Scientific Investigations at the Pluto System Leslie A. Young · S. Alan Stern · Harold A. Weaver · Fran Bagenal · Richard P. Binzel · Bonnie Buratti · Andrew F. Cheng · Dale Cruikshank · G. Randall Gladstone · William M. Grundy · David P. Hinson · Mihaly Horanyi · Donald E. Jennings · Ivan R. Linscott · David J. McComas · William B. McKinnon · Ralph McNutt · Jeffery M. Moore · Scott Murchie · Catherine B. Olkin · Carolyn C. Porco · Harold Reitsema · Dennis C. Reuter · John R. Spencer · David C. Slater · Darrell Strobel · Michael E. Summers · G. Leonard Tyler Received: 5 January 2007 / Accepted: 28 October 2008 / Published online: 3 December 2008 © Springer Science+Business Media B.V. 2008 L.A. Young () · S.A. Stern · C.B. Olkin · J.R. Spencer Southwest Research Institute, Boulder, CO, USA e-mail: [email protected] H.A. Weaver · A.F. Cheng · R. McNutt · S. Murchie Johns Hopkins University Applied Physics Lab., Laurel, MD, USA F. Bagenal · M. Horanyi University of Colorado, Boulder, CO, USA R.P. Binzel Massachusetts Institute of Technology, Cambridge, MA, USA B. Buratti Jet Propulsion Laboratory, Pasadena, CA, USA D. Cruikshank · J.M. Moore NASA Ames Research Center, Moffett Field, CA, USA G.R. Gladstone · D.J. McComas · D.C. Slater Southwest Research Institute, San Antonio, TX, USA W.M. Grundy Lowell Observatory, Flagstaff, AZ, USA D.P. Hinson · I.R. Linscott · G.L. Tyler Stanford University, Stanford, CA, USA D.E. Jennings · D.C. Reuter NASA Goddard Space Flight Center, Greenbelt, MD, USA 94 L.A. Young et al. -
Giant Planet / Kuiper Belt Flyby
Giant Planet / Kuiper Belt Flyby Amanda Zangari (SwRI) Tiffany Finley (SwRI) with Cecilia Leung (LPL/SwRI) Simon Porter (SwRI) OPAG: February 23, 2017 Take Away • New Horizons provided scientifically valuable exploration of the Kuiper Belt in the New Frontiers cost cap. • The Kuiper Belt is full of objects with a diverse range of stories that go beyond what we learned from Pluto. • Giant Planet flybys add scientific value to a Kuiper Belt mission • Found preliminary trajectory examples for high interest KBOs-- Haumea, Varuna, 2015 RR245 can be reached via Jupiter AND Saturn, Uranus or Neptune flyby in the 2030s. • To be a candidate New Frontiers mission, a 2 Giant planet+KBO mission must be endorsed by a decadal survey according to current rules. New Horizons Heritage NH Jupiter Encounter planned around Pluto flyby timing, which was dominated by achieving quadruple occultations, “interesting” side up. New Horizons Heritage Pluto flyby took advantage of Ecliptic crossing, enabling access to the cold classical belt (where 2014 MU69 is located). New Horizons Heritage 2014 MU69 discovered while in flight. Targeting was from spacecraft propulsion and took advantage of cold classical population density. Object is small, reddish ~40 km diameter. Saturn’s moons show incredible diversity NASA/JPL As do Uranus and Neptune Some Kuiper Belt Geography Where do we want to go? Getting there- JGA “anytime” New Horizons model: Fast Launch, Jupiter Flyby, Launch window every 11 years McGranaghan et al 2011 Can we go to more than just Jupiter? If so, where, what? New Horizons 2 • 2008 launch using New Horizons flight spares • Proposed Jupiter flyby, equinox flyby of Uranus, and flyby of (47171) 1999 TC36 (now know to be trinary). -
DOE Could Improve Planning and Communication Related to Plutonium-238 And
United States Government Accountability Office Report to Congressional Requesters September 2017 SPACE EXPLORATION DOE Could Improve Planning and Communication Related to Plutonium- 238 and Radioisotope Power Systems Production Challenges Accessible Version GAO-17-673 September 2017 SPACE EXPLORATION DOE Could Improve Planning and Communication Related to Plutonium-238 and Radioisotope Power Systems Production Challenges Highlights of GAO-17-673, a report to congressional requesters Why GAO Did This Study What GAO Found NASA uses RPS to generate electrical The National Aeronautics and Space Administration (NASA) selects radioisotope power in missions in which solar power systems (RPS) for missions primarily based on the agency’s scientific panels or batteries would be objectives and mission destinations. Prior to the establishment of the Department ineffective. RPS convert heat of Energy’s (DOE) Supply Project in fiscal year 2011 to produce new plutonium- generated by the radioactive decay of 238 (Pu-238), NASA officials said that Pu-238 supply was a limiting factor in Pu-238 into electricity. DOE maintains selecting RPS-powered missions. After the initiation of the Supply Project, a capability to produce RPS for NASA however, NASA officials GAO interviewed said that missions are selected missions, as well as a limited and independently of decisions on how to power them. Once a mission is selected, aging supply of Pu-238 that will be NASA considers power sources early in its mission review process. Multiple depleted in the 2020s, according to NASA and DOE officials and factors could affect NASA’s demand for RPS and Pu-238. For example, high documentation. With NASA funding, costs associated with RPS and missions can affect the demand for RPS DOE initiated the Pu-238 Supply because, according to officials, NASA’s budget can only support one RPS Project in 2011, with a goal of mission about every 4 years. -
Space Biology Research and Biosensor Technologies: Past, Present, and Future †
biosensors Perspective Space Biology Research and Biosensor Technologies: Past, Present, and Future † Ada Kanapskyte 1,2, Elizabeth M. Hawkins 1,3,4, Lauren C. Liddell 5,6, Shilpa R. Bhardwaj 5,7, Diana Gentry 5 and Sergio R. Santa Maria 5,8,* 1 Space Life Sciences Training Program, NASA Ames Research Center, Moffett Field, CA 94035, USA; [email protected] (A.K.); [email protected] (E.M.H.) 2 Biomedical Engineering Department, The Ohio State University, Columbus, OH 43210, USA 3 KBR Wyle, Moffett Field, CA 94035, USA 4 Mammoth Biosciences, Inc., South San Francisco, CA 94080, USA 5 NASA Ames Research Center, Moffett Field, CA 94035, USA; [email protected] (L.C.L.); [email protected] (S.R.B.); [email protected] (D.G.) 6 Logyx, LLC, Mountain View, CA 94043, USA 7 The Bionetics Corporation, Yorktown, VA 23693, USA 8 COSMIAC Research Institute, University of New Mexico, Albuquerque, NM 87131, USA * Correspondence: [email protected]; Tel.: +1-650-604-1411 † Presented at the 1st International Electronic Conference on Biosensors, 2–17 November 2020; Available online: https://iecb2020.sciforum.net/. Abstract: In light of future missions beyond low Earth orbit (LEO) and the potential establishment of bases on the Moon and Mars, the effects of the deep space environment on biology need to be examined in order to develop protective countermeasures. Although many biological experiments have been performed in space since the 1960s, most have occurred in LEO and for only short periods of time. These LEO missions have studied many biological phenomena in a variety of model organisms, and have utilized a broad range of technologies. -
The Mars Thermosphere-Ionosphere: Predictions for the Arrival of Planet-B
Earth Planets Space, 50, 247–257, 1998 The Mars thermosphere-ionosphere: Predictions for the arrival of Planet-B S. W. Bougher1 and H. Shinagawa2 1Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, U.S.A. 2Solar Terrestrial Environment Laboratory, Nagoya University, Japan (Received July 28, 1997; Revised January 6, 1998; Accepted February 12, 1998) The primary science objective of the Planet-B mission to Mars is to study the Martian upper atmosphere-ionosphere system and its interaction with the solar wind. An improved knowledge of the Martian magnetic field (whether it is induced or intrinsic) is needed, and will be provided by Planet-B. In addition, a proper characterization of the neutral thermosphere structure is essential to place the various plasma observations in context. The Neutral Mass Spectrometer (NMS) onboard Planet-B will provide the required neutral density information over the altitude range of 150–500 km. Much can be learned in advance of Planet-B data taking as multi-dimensional thermosphere-ionosphere and MHD models are exercised to predict the Mars near-space environment that might be expected during the solar maximum conditions of Cycle 23 (1999–2001). Global model simulations of the Mars thermosphere-ionosphere system are presented and analyzed in this paper. These Mars predictions pertain to the time of Planet-B arrival in October 1999 (F10.7∼200; Ls∼220). In particular, the National Center for Atmospheric Research (NCAR) Mars Thermosphere General Circulation Model (MTGCM) is exercised to calculate thermospheric neutral densities (CO2, + + + CO, N2,O,Ar,O2), photochemical ions (CO2 ,O2 ,O below 200 km), neutral temperatures, and 3-components winds over 70–300 km. -
The Deep Space Network - a Technology Case Study and What Improvements to the Deep Space Network Are Needed to Support Crewed Missions to Mars?
The Deep Space Network - A Technology Case Study and What Improvements to the Deep Space Network are Needed to Support Crewed Missions to Mars? A Master’s Thesis Presented to Department of Telecommunications State University of New York Polytechnic Institute Utica, New York In Partial Fulfillment of the Requirements for the Master of Science Degree By Prasad Falke May 2017 Abstract The purpose of this thesis research is to find out what experts and interested people think about Deep Space Network (DSN) technology for the crewed Mars mission in the future. The research document also addresses possible limitations which need to be fix before any critical missions. The paper discusses issues such as: data rate, hardware upgrade and new install requirement and a budget required for that, propagation delay, need of dedicated antenna support for the mission and security constraints. The Technology Case Study (TCS) and focused discussion help to know the possible solutions and what everyone things about the DSN technology. The public platforms like Quora, Reddit, StackExchange, and Facebook Mars Society group assisted in gathering technical answers from the experts and individuals interested in this research. iv Acknowledgements As the thesis research was challenging and based on the output of the experts and interested people in this field, I would like to express my gratitude and appreciation to all the participants. A special thanks go to Dr. Larry Hash for his guidance, encouragement, and support during the whole time. Additionally, I also want to thank my mother, Mrs. Mangala Falke for inspiring me always. Last but not the least, I appreciate the support from Maricopa County Emergency Communications Group (MCECG) and Arizona Near Space Research (ANSR) Organization for helping me to find the experts in space and communications field.