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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 -
Doc.10100.Space Weather Manual FINAL DRAFT Version
Doc 10100 Manual on Space Weather Information in Support of International Air Navigation Approved by the Secretary General and published under his authority First Edition – 2018 International Civil Aviation Organization TABLE OF CONTENTS Page Chapter 1. Introduction ..................................................................................................................................... 1-1 1.1 General ............................................................................................................................................... 1-1 1.2 Space weather indicators .................................................................................................................... 1-1 1.3 The hazards ........................................................................................................................................ 1-2 1.4 Space weather mitigation aspects ....................................................................................................... 1-3 1.5 Coordinating the response to a space weather event ......................................................................... 1-3 Chapter 2. Space Weather Phenomena and Aviation Operations ................................................................. 2-1 2.1 General ............................................................................................................................................... 2-1 2.2 Geomagnetic storms .......................................................................................................................... -
Analysis of Geomagnetic Storms in South Atlantic Magnetic Anomaly (SAMA)
Analysis of geomagnetic storms in South Atlantic Magnetic Anomaly (SAMA) Júlia Maria Soja Sampaio, Elder Yokoyama, Luciana Figueiredo Prado Copyright 2019, SBGf - Sociedade Brasileira de Geofísica Moreover, Dst and AE indices may vary according to the This paper was prepared for presentation during the 16th International Congress of the geomagnetic field geometry, such as polar to intermediate Brazilian Geophysical Society held in Rio de Janeiro, Brazil, 19-22 August 2019. latitudinal field variations. In this framework, fluctuations Contents of this paper were reviewed by the Technical Committee of the 16th in the geomagnetic field can occur under the influence of International Congress of the Brazilian Geophysical Society and do not necessarily represent any position of the SBGf, its officers or members. Electronic reproduction or the South Atlantic Magnetic Anomaly (SAMA). The SAMA storage of any part of this paper for commercial purposes without the written consent is a region of minimum geomagnetic field intensity values of the Brazilian Geophysical Society is prohibited. ____________________________________________________________________ at the Earth’s surface (Figure 1), and its dipole intensity is decreasing along the past 1000 years (Terra-Nova et. al., Abstract 2017). Geomagnetic storm is a major disturbance of Earth’s In this study we will compare the behavior of the types of magnetosphere resulted from the interaction of solar wind geomagnetic storms basis on AE and Dst indices. and the Earth’s magnetic field. This disturbance depends of the Earth magnetic field geometry, and varies in terms of intensity from the Poles to the Equator. This disturbance is quantified through geomagnetic indices, such as the Dst and the AE indices. -
Space UK Earth’S Surface Water
Issue #49 IN THIS ISSUE: Staring at the Sun MYSTERIOUS Helpline from Space Weightless in the Clouds MERCURY Contents News Cornwall Calling Space Weather Watcher Mapping the Route to Mars Honour for UK Astronaut New Satellite Tracks Pollution UK-France Space Deal In Pictures The Sun Features Mysterious Mercury Zero-G Science Helpline from Space Education Resources UK Space History Skylark Made in the UK Earth-i Info News Cornwall Calling The first Moon landing Cornwall Calling Credit: NASA Cornwall could soon be Antennas at Goonhilly beamed communicating with the Moon and images of the 1969 Moon landing Mars, following the announcement and, shortly after it was built in that the world’s first commercial deep 1985, the 32-metre Goonhilly-6 space communication base will be at antenna carried the historic Live Aid the Goonhilly Earth Station. concert broadcast to TV viewers An £8.4 million investment will see a around the world. two-year upgrade of the Goonhilly-6 A Space Industry Bill, announced antenna so it can communicate as part of the Queen’s speech in One of the large dishes at Goonhilly with future robotic and crewed 2017, will introduce new powers missions to the Moon and Mars. The to allow rocket and spaceplane Credit: Goonhilly Cornwall and Isles of Scilly Local launches from UK soil. Goonhilly is Enterprise Partnership’s Growth Deal also offering spacecraft tracking and the European Space Agency and communications facilities as (ESA) – which the UK Space Agency part of the Spaceport Cornwall contributes to – funded the contract, funding bid. which will allow Goonhilly to support “We see huge opportunities for ESA’s worldwide network of spacecraft the developing space sector in monitoring ground stations. -
A Future Mars Environment for Science and Exploration
Planetary Science Vision 2050 Workshop 2017 (LPI Contrib. No. 1989) 8250.pdf A FUTURE MARS ENVIRONMENT FOR SCIENCE AND EXPLORATION. J. L. Green1, J. Hol- lingsworth2, D. Brain3, V. Airapetian4, A. Glocer4, A. Pulkkinen4, C. Dong5 and R. Bamford6 (1NASA HQ, 2ARC, 3U of Colorado, 4GSFC, 5Princeton University, 6Rutherford Appleton Laboratory) Introduction: Today, Mars is an arid and cold world of existing simulation tools that reproduce the physics with a very thin atmosphere that has significant frozen of the processes that model today’s Martian climate. A and underground water resources. The thin atmosphere series of simulations can be used to assess how best to both prevents liquid water from residing permanently largely stop the solar wind stripping of the Martian on its surface and makes it difficult to land missions atmosphere and allow the atmosphere to come to a new since it is not thick enough to completely facilitate a equilibrium. soft landing. In its past, under the influence of a signif- Models hosted at the Coordinated Community icant greenhouse effect, Mars may have had a signifi- Modeling Center (CCMC) are used to simulate a mag- cant water ocean covering perhaps 30% of the northern netic shield, and an artificial magnetosphere, for Mars hemisphere. When Mars lost its protective magneto- by generating a magnetic dipole field at the Mars L1 sphere, three or more billion years ago, the solar wind Lagrange point within an average solar wind environ- was allowed to directly ravish its atmosphere.[1] The ment. The magnetic field will be increased until the lack of a magnetic field, its relatively small mass, and resulting magnetotail of the artificial magnetosphere its atmospheric photochemistry, all would have con- encompasses the entire planet as shown in Figure 1. -
And Ground-Based Observations of Pulsating Aurora
University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Spring 2010 Space- and ground-based observations of pulsating aurora Sarah Jones University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation Jones, Sarah, "Space- and ground-based observations of pulsating aurora" (2010). Doctoral Dissertations. 597. https://scholars.unh.edu/dissertation/597 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. SPACE- AND GROUND-BASED OBSERVATIONS OF PULSATING AURORA BY SARAH JONES B.A. in Physics, Dartmouth College 2004 DISSERTATION Submitted to the University of New Hampshire in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Physics May, 2010 UMI Number: 3470104 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT Dissertation Publishing UMI 3470104 Copyright 2010 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 This dissertation has been examined and approved. -
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. -
Jets Downstream of Collisionless Shocks
Space Sci Rev (2018) 214:81 https://doi.org/10.1007/s11214-018-0516-3 Jets Downstream of Collisionless Shocks Ferdinand Plaschke1,2 · Heli Hietala3 · Martin Archer4 · Xóchitl Blanco-Cano5 · Primož Kajdicˇ5 · Tomas Karlsson6 · Sun Hee Lee7 · Nojan Omidi8 · Minna Palmroth9,10 · Vadim Roytershteyn11 · Daniel Schmid12 · Victor Sergeev13 · David Sibeck7 Received: 19 December 2017 / Accepted: 2 June 2018 / Published online: 21 June 2018 © The Author(s) 2018 Abstract The magnetosheath flow may take the form of large amplitude, yet spatially local- ized, transient increases in dynamic pressure, known as “magnetosheath jets” or “plasmoids” among other denominations. Here, we describe the present state of knowledge with respect to such jets, which are a very common phenomenon downstream of the quasi-parallel bow shock. We discuss their properties as determined by satellite observations (based on both case and statistical studies), their occurrence, their relation to solar wind and foreshock con- ditions, and their interaction with and impact on the magnetosphere. As carriers of plasma and corresponding momentum, energy, and magnetic flux, jets bear some similarities to bursty bulk flows, which they are compared to. Based on our knowledge of jets in the near Earth environment, we discuss the expectations for jets occurring in other planetary and B F. Plaschke [email protected] 1 Space Research Institute, Austrian Academy of Sciences, Graz, Austria 2 Present address: Institute of Physics, University of Graz, Graz, Austria 3 Department of -
On Magnetic Storms and Substorms
ILWS WORKSHOP 2006, GOA, FEBRUARY 19-24, 2006 On magnetic storms and substorms G. S. Lakhina, S. Alex, S. Mukherjee and G. Vichare Indian Institute of Geomagnetism, New Panvel (W), Navi Mumbai-410218, India Abstract. Magnetospheric substorms and storms are indicators of geomagnetic activity. Whereas the geomagnetic index AE (auroral electrojet) is used to study substorms, it is common to characterize the magnetic storms by the Dst (disturbance storm time) index of geomagnetic activity. This talk discusses briefly the storm-substorms relationship, and highlights some of the characteristics of intense magnetic storms, including the events of 29-31 October and 20-21 November 2003. The adverse effects of these intense geomagnetic storms on telecommunication, navigation, and on spacecraft functioning will be discussed. Index Terms. Geomagnetic activity, geomagnetic storms, space weather, substorms. _____________________________________________________________________________________________________ 1. Introduction latitude magnetic fields are significantly depressed over a Magnetospheric storms and substorms are indicators of time span of one to a few hours followed by its recovery geomagnetic activity. Where as the magnetic storms are which may extend over several days (Rostoker, 1997). driven directly by solar drivers like Coronal mass ejections, solar flares, fast streams etc., the substorms, in simplest terms, are the disturbances occurring within the magnetosphere that are ultimately caused by the solar wind. The magnetic storms are characterized by the Dst (disturbance storm time) index of geomagnetic activity. The substorms, on the other hand, are characterized by geomagnetic AE (auroral electrojet) index. Magnetic reconnection plays an important role in energy transfer from solar wind to the magnetosphere. Magnetic reconnection is very effective when the interplanetary magnetic field is directed southwards leading to strong plasma injection from the tail towards the inner magnetosphere causing intense auroras at high-latitude nightside regions. -
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. -
Solar Wind Magnetosphere Coupling
Solar Wind Magnetosphere Coupling F. Toffoletto, Rice University Figure courtesy T. W. Hill with thanks to R. A. Wolf and T. W. Hill, Rice U. Outline • Introduction • Properties of the Solar Wind Near Earth • The Magnetosheath • The Magnetopause • Basic Physical Processes that control Solar Wind Magnetosphere Coupling – Open and Closed Magnetosphere Processes – Electrodynamic coupling – Mass, Momentum and Energy coupling – The role of the ionosphere • Current Status and Summary QuickTime™ and a YUV420 codec decompressor are needed to see this picture. Introduction • By virtue of our proximity, the Earth’s magnetosphere is the most studied and perhaps best understood magnetosphere – The system is rather complex in its structure and behavior and there are still some basic unresolved questions – Today’s lecture will focus on describing the coupling to the major driver of the magnetosphere - the solar wind, and the ionosphere – Monday’s lecture will look more at the more dynamic (and controversial) aspect of magnetospheric dynamics: storms and substorms The Solar Wind Near the Earth Solar-Wind Properties Observed Near Earth • Solar wind parameters observed by many spacecraft over period 1963-86. From Hapgood et al. (Planet. Space Sci., 39, 410, 1991). Solar Wind Observed Near Earth Values of Solar-Wind Parameters Parameter Minimum Most Maximum Probable Velocity v (km/s) 250 370 2000× Number density n (cm-3) 683 Ram pressure rv2 (nPa)* 328 Magnetic field strength B 0 6 85 (nanoteslas) IMF Bz (nanoteslas) -31 0¤ 27 * 1 nPa = 1 nanoPascal = 10-9 Newtons/m2. Indicates at least one interval with B < 0.1 nT. ¤ Mean value was 0.014 nT, with a standard deviation of 3.3 nT.