The Heliospheric Current Sheet and Plasma Sheet During Parker Solar Probe’S First Orbit B
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Slow Solar Wind: Observations and Modeling
Noname manuscript No. (will be inserted by the editor) Slow solar wind: observations and modeling L. Abbo · L. Ofman · S.K. Antiochos · V.H. Hansteen · L. Harra · Y-K. Ko · G. Lapenta · B. Li · P. Riley · L. Strachan · R. von Steiger · Y.-M. Wang Received: date / Accepted: date L. Abbo Osservatorio Astrofisico di Torino Strada Osservatorio 20, 10025 Pino Torinese, Italy Tel.: +39-011-8101954 Fax: +39-011- 8101930 E-mail: [email protected] · L. Ofman∗ (corresponding author) Catholic University of America, NASA-Goddard Space Flight Center Code 671, Greenbelt, MD 20771, USA ∗ also Visiting, Department of Geosciences, Tel Aviv University E-mail: [email protected] · S.K. Antiochos NASA-Goddard Space Flight Center Greenbelt, MD 20771, USA · V. Hansteen Institute of Theoretical Astrophysics, University of Oslo PB 1029, Blindern, N-0315, Oslo, Norway · L. Harra UCL-Mullard Space Science Laboratory Holmbury St. Mary, Dorking, Surrey, RH5 6NT, UK · Y.-K. Ko, L. Strachan, Y.-M. Wang Space Science Division, Naval Research Laboratory Washington, DC 20375-5352, USA · G. Lapenta Centre for Plasma Astrophysics, K. U. Leuven Celestijnenlaan 200b- bus 2400, 3001 Leuven, Belgium · B. Li Institute of Space Sciences, Shandong University Weihai 180 West Wenhua Road, 264209 Weihai, China · P. Riley Predictive Science, Inc. 9990 Mesa Rim Road, Suite 170, San Diego, CA 92121, USA · Y.-M. Wang Code 7682W Space Science Division Naval Research Laboratory Washington, DC 20375-5352, USA · R. von Steiger Director, International Space Science Institute Hallerstrasse 6 3012, Bern, Switzerland 2 L. Abbo, L. Ofman et al. Abstract While it is certain that the fast solar wind originates from coronal holes, where and how the slow solar wind (SSW) is formed remains an outstand- ing question in solar physics even in the post-SOHO era. -
Observations of Solar Wind Penetration Into the Earth's Magnetosphere: the Plasma Mantle
ENNIO R. SANCHEZ, CHING-I. MENG, and PATRICK T. NEWELL OBSERVATIONS OF SOLAR WIND PENETRATION INTO THE EARTH'S MAGNETOSPHERE: THE PLASMA MANTLE The large database provided by the continuous coverage of the Defense Meteorological Satellite Pro gram polar orbiting satellites constitutes an important source of information on particle precipitation in the ionosphere. This information can be used to monitor and map the Earth's magnetosphere (the cavity around the Earth that forms as the stream of particles and magnetic field ejected from the Sun, known as the solar wind, encounters the Earth's magnetic field) and for a large variety of statistical studies of its morphology and dynamics. The boundary between the magnetosphere and the solar wind is pre sumably open in some places and at some times, thus allowing the direct entry of solar-wind plasma into the magnetosphere through a boundary layer known as the plasma mantle. The preliminary results of a statistical study of the plasma-mantle precipitation in the ionosphere are presented. The first quan titative mapping of the ionospheric region where the plasma-mantle particles precipitate is obtained. INTRODUCTION Polar orbiting satellites are very useful platforms for studying the properties of the environment surrounding the Earth at distances well above the ionosphere. This article focuses on a description of the enormous poten tial of those platforms, especially when they are com bined with other means of measurement, such as ground-based stations and other satellites. We describe in some detail the first results of the kind of study for which the polar orbiting satellites are ideal instruments. -
1 Solar Wind at 33 AU: Setting Bounds on the Pluto Interaction For
Solar Wind at 33 AU: Setting Bounds on the Pluto Interaction for New Horizons F. Bagenal1, P.A. Delamere2, H. A. Elliott3, M.E. Hill4, C.M. Lisse4, D.J. McComas3,7, R.L McNutt, Jr.4, J.D. Richardson5, C.W. Smith6, D.F. Strobel8 1 University of Colorado, Boulder CO 2 University of Alaska, Fairbanks AK 3 Southwest Research Institute, San Antonio TX 4 ApplieD Physics Laboratory, The Johns Hopkins University, Laurel MD 5 Massachusetts Institute of Technology, CambriDge MA 6 University of New Hampshire, Durham NH 7 University of Texas at San Antonio, San Antonio TX 8 The Johns Hopkins University, Baltimore MD CorresponDing author information: Fran Bagenal Professor of Astrophysical and Planetary Sciences Laboratory for Atmospheric anD Space Physics UCB 600 University of Colorado 3665 Discovery Drive Boulder CO 80303 Tel. 303 492 2598 [email protected] Abstract NASA’s New Horizons spacecraft flies past Pluto on July 14, 2015, carrying two instruments that Detect chargeD particles. Pluto has a tenuous, extenDeD atmosphere that is escaping the planet’s weak gravity. The interaction of the solar wind with Pluto’s escaping atmosphere depends on solar wind conditions as well as the vertical structure of Pluto’s atmosphere. We have analyzeD Voyager 2 particles anD fielDs measurements between 25 anD 39 AU anD present their statistical variations. We have adjusted these predictions to allow for the Sun’s declining activity and solar wind output. We summarize the range of SW conDitions that can be expecteD at 33 AU anD survey the range of scales of interaction that New Horizons might experience. -
Modelling the Initiation of Coronal Mass Ejections: Magnetic Flux Emergence Versus Shearing Motions
A&A 507, 441–452 (2009) Astronomy DOI: 10.1051/0004-6361/200912541 & c ESO 2009 Astrophysics Modelling the initiation of coronal mass ejections: magnetic flux emergence versus shearing motions F. P. Zuccarello1,2,C.Jacobs1,2,A.Soenen1,2, S. Poedts1,2,B.vanderHolst3, and F. Zuccarello4 1 Centre for Plasma-Astrophysics, K. U. Leuven, Celestijnenlaan 200B, 3001 Leuven, Belgium e-mail: [email protected] 2 Leuven Mathematical Modelling & Computational Science Research Centre (LMCC), Belgium 3 Center for Space Environment Modeling, University of Michigan, 2455 Hayward Street, Ann Arbor, MI 48109, USA 4 Dipartimento di Fisica e Astronomia – Universitá di Catania via S.Sofia 78, 95123 Catania, Italy Received 20 May 2009 / Accepted 14 July 2009 ABSTRACT Context. Coronal mass ejections (CMEs) are enormous expulsions of magnetic flux and plasma from the solar corona into the inter- planetary space. These phenomena release a huge amount of energy. It is generally accepted that both photospheric motions and the emergence of new magnetic flux from below the photosphere can put stress on the system and eventually cause a loss of equilibrium resulting in an eruption. Aims. By means of numerical simulations we investigate both emergence of magnetic flux and shearing motions along the magnetic inversion line as possible driver mechanisms for CMEs. The pre-eruptive region consists of three arcades with alternating magnetic flux polarity, favouring the breakout mechanism. Methods. The equations of ideal magnetohydrodynamics (MHD) were advanced in time by using a finite volume approach and solved in spherical geometry. The simulation domain covers a meridional plane and reaches from the lower solar corona up to 30 R.When we applied time-dependent boundary conditions at the inner boundary, the central arcade of the multiflux system expands, leading to the eventual eruption of the top of the helmet streamer. -
THEMIS Telescope Images Analysed for Space Weather Traces
EPSC Abstracts Vol. 14, EPSC2020-1022, 2020 https://doi.org/10.5194/epsc2020-1022 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. THEMIS telescope images analysed for space weather traces Melinda Dósa1, Valeria Mangano2, Zsofia Bebesi1, Stefano Massetti2, Anna Milillo2, and Anna Görgei3 1Wigner Research Centre for Physics, Space Physics and Space Technology, Budapest, Hungary ([email protected]) 2INAF/IAPS, Istituto Nazionale di Astrofisica, Roma, Italy 3Eötvös Loránd University, Institute of Physics The THEMIS solar telescope operating on Tenerife (Canary islands) has observed Mercury’s Na exosphere along several campaigns since 2007. A dataset of images taken between 2009 and 2013 are analysed here in relation with propagated solar wind data. A small subset of the images shows a low level of correlation between Na-emission and solar wind dynamic pressure. The amount of data at present is not sufficient to make a clear statement on whether the correlation is a coincidence or can be explained by other factors (position of Mercury and Earth, solar activity, etc.). Nevertheless, the authors present a comprehensive study taking into account all possible factors. Sodium plays a special role in Mercury’s exosphere: due to its strong resonance line it has been observed and monitored by Earth-based telescopes for decades. Different and highly variable patterns of Na-emission have been identified, the most common and recurrent being the high latitude double-peak pattern [1]. It is clear that the exosphere is linked to the surface and influenced by the interstellar medium and the solar wind deviated by the magnetosphere, but the role and weight of the single processes are still under discussion [2]. -
Ejecta Event Associated with a Two&Hyphen;Step Geomagnetic Storm
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, A11104, doi:10.1029/2006JA011893, 2006 A two-ejecta event associated with a two-step geomagnetic storm C. J. Farrugia,1 V. K. Jordanova,1,2 M. F. Thomsen,2 G. Lu,3 S. W. H. Cowley,4 and K. W. Ogilvie5 Received 2 June 2006; revised 1 September 2006; accepted 12 September 2006; published 16 November 2006. [1] A new view on how large disturbances in the magnetosphere may be prolonged and intensified further emerges from a recently discovered interplanetary process: the collision/merger of interplanetary (IP) coronal mass ejections (ICMEs; ejecta) within 1 AU. As shown in a recent pilot study, the merging process changes IP parameters dramatically with respect to values in isolated ejecta. The resulting geoeffects of the coalesced (‘‘complex’’) ejecta reflect a superposition of IP triggers which may result in, for example, two-step, major geomagnetic storms. In a case study, we isolate the effects on ring current enhancement when two coalescing ejecta reached Earth on 31 March 2001. The magnetosphere ‘‘senses’’ the presence of the two ejecta and responds with a reactivation of the ring current soon after it started to recover from the passage of the first ejection, giving rise to a double-dip (DD) great storm (each min Dst < À250 nT). A drift-loss global kinetic model of ring current buildup shows that in this case the major factor determining the intensity of the storm activity is the very high (up to 10 cmÀ3) plasma sheet density. The plasma sheet density, in turn, is found to correlate well with the very high solar wind density, suggesting the compression of the leading ejecta as the source of the hot, superdense plasma sheet in this case. -
Cmes, Solar Wind and Sun-Earth Connections: Unresolved Issues
CMEs, solar wind and Sun-Earth connections: unresolved issues Rainer Schwenn Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany [email protected] In recent years, an unprecedented amount of high-quality data from various spaceprobes (Yohkoh, WIND, SOHO, ACE, TRACE, Ulysses) has been piled up that exhibit the enormous variety of CME properties and their effects on the whole heliosphere. Journals and books abound with new findings on this most exciting subject. However, major problems could still not be solved. In this Reporter Talk I will try to describe these unresolved issues in context with our present knowledge. My very personal Catalog of ignorance, Updated version (see SW8) IAGA Scientific Assembly in Toulouse, 18-29 July 2005 MPRS seminar on January 18, 2006 The definition of a CME "We define a coronal mass ejection (CME) to be an observable change in coronal structure that occurs on a time scale of a few minutes and several hours and involves the appearance (and outward motion, RS) of a new, discrete, bright, white-light feature in the coronagraph field of view." (Hundhausen et al., 1984, similar to the definition of "mass ejection events" by Munro et al., 1979). CME: coronal -------- mass ejection, not: coronal mass -------- ejection! In particular, a CME is NOT an Ejección de Masa Coronal (EMC), Ejectie de Maså Coronalå, Eiezione di Massa Coronale Éjection de Masse Coronale The community has chosen to keep the name “CME”, although the more precise term “solar mass ejection” appears to be more appropriate. An ICME is the interplanetry counterpart of a CME 1 1. -
Mechanisms of Formation of Multiple Current Sheets in the Heliospheric Plasma Sheet
EGU2020-3945 https://doi.org/10.5194/egusphere-egu2020-3945 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Mechanisms of formation of multiple current sheets in the heliospheric plasma sheet Evgeniy Maiewski1, Helmi Malova2,3, Roman Kislov3,4, Victor Popov5, Anatoly Petrukovich3, and Lev Zelenyi3 1National Research University”Higher School of Economics”, Moscow, Russian Federation ([email protected]) 2Scobeltsyn Institute of Nuclear Physics, Lomonosov Moscow State University, Moscow, Russia ([email protected]) 3Space Research Institute of the Russian Academy of Science, Moscow, Russia 4Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation of the Russian Academy of Sciences (IZMIRAN), Moscow, Russia 5Faculty of Physics, Lomonosov Moscow State University, Moscow, Russia When spacecraft cross the heliospheric plasma sheet (HPS) that separates large-scale magnetic sectors of the opposite direction in the solar wind, multiple rapid fluctuations of a sign of the radial magnetic field component are observed very often, indicating the presence of multiple current sheets occurring within the HPS. Possible mechanisms of formation of these structures in the solar wind are proposed. Taking into accout that the streamer belt in the solar corona is believed to be the main source of the slow solar wind in the heliosphere, we suggest that the effect of the multi-layered HPS is determined by the extension of many streamer-belt-borne thin current sheets oriented along the neutral line of the interplanetary magnetic field. Within the framework of a proposed MHD model, self-consistent distributions of the key solar wind characteristics which depend on streamer propreties are investigated. -
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. -
THEMIS Observations of a Hot Flow Anomaly: Solar Wind, Magnetosheath, and Ground-Based Measurements J
THEMIS observations of a hot flow anomaly: Solar wind, magnetosheath, and ground-based measurements J. Eastwood, D. Sibeck, V. Angelopoulos, T. Phan, S. Bale, J. Mcfadden, C. Cully, S. Mende, D. Larson, S. Frey, et al. To cite this version: J. Eastwood, D. Sibeck, V. Angelopoulos, T. Phan, S. Bale, et al.. THEMIS observations of a hot flow anomaly: Solar wind, magnetosheath, and ground-based measurements. Geophysical Research Letters, American Geophysical Union, 2008, 35 (17), pp.L17S03. 10.1029/2008GL033475. hal- 03086705 HAL Id: hal-03086705 https://hal.archives-ouvertes.fr/hal-03086705 Submitted on 23 Dec 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L17S03, doi:10.1029/2008GL033475, 2008 THEMIS observations of a hot flow anomaly: Solar wind, magnetosheath, and ground-based measurements J. P. Eastwood,1 D. G. Sibeck,2 V. Angelopoulos,3 T. D. Phan,1 S. D. Bale,1,4 J. P. McFadden,1 C. M. Cully,5,6 S. B. Mende,1 D. Larson,1 S. Frey,1 C. W. Carlson,1 K.-H. Glassmeier,7 H. U. Auster,7 A. Roux,8 and O. -
Helmet Streamers with Triple Structures: Simulations of Resistive Dynamics
HELMET STREAMERS WITH TRIPLE STRUCTURES: SIMULATIONS OF RESISTIVE DYNAMICS THOMAS WIEGELMANN1, KARL SCHINDLER2 and THOMAS NEUKIRCH3 1Max Planck Institut für Aeronomie, Max Planck Straße 2, D-37191 Katlenburg-Lindau, Germany; 2 Institut für Theoretische Physik IV, Ruhr-Universität Bochum, D-44780 Bochum, Germany; 3School of Mathematical and Computational Sciences, University of St. Andrews, St. Andrews, Scotland (Received 20 April 1999; accepted 8 October 1999) Abstract. Recent observations of the solar corona with the LASCO coronagraph on board of the SOHO spacecraft have revealed the occurrence of triple helmet streamers even during solar mini- mum, which occasionally go unstable and give rise to large coronal mass ejections. There are also indications that the slow solar wind is either a combination of a quasi-stationary flow and a highly fluctuating component or may even be caused completely by many small eruptions or instabilities. As a first step we recently presented an analytical method to calculate simple two-dimensional stationary models of triple helmet streamer configurations. In the present contribution we use the equations of time-dependent resistive magnetohydrodynamics to investigate the stability and the dynamical behaviour of these configurations. We particularly focus on the possible differences between the dynamics of single isolated streamers and triple streamers and on the way in which magnetic recon- nection initiates both small scale and large scale dynamical behaviour of the streamers. Our results indicate that small eruptions at the helmet streamer cusp may incessantly accelerate small amounts of plasma without significant changes of the equilibrium configuration and might thus contribute to the non-stationary slow solar wind. -
Space Weather
ASTRONOMY AND ASTROPHYSICS LIBRARY Series Editors: G. Börner, Garching, Germany A. Burkert, München, Germany W. B. Burton, Charlottesville, VA, USA and Leiden, The Netherlands M. A. Dopita, Canberra, Australia A. Eckart, Köln, Germany T. Encrenaz, Meudon, France E. K. Grebel, Heidelberg, Germany B. Leibundgut, Garching, Germany J. Lequeux, Paris, France A. Maeder, Sauverny, Switzerland V.Trimble, College Park, MD, and Irvine, CA, USA Kenneth R. Lang The Sun from Space Second Edition 123 Kenneth R. Lang Department of Physics and Astronomy Tufts University Medford MA 02155 USA [email protected] Cover image: Solar cycle magnetic variations. These magnetograms portray the polarity and distribution of the magnetism in the solar photosphere. They were made with the Vacuum Tower Telescope of the National Solar Observatory at Kitt Peak from 8 January 1992, at a maximum in the sunspot cycle (lower left) to 25 July 1999, well into the next maximum (lower right). Each magnetogram shows opposite polarities as darker and brighter than average tint. When the Sun is most active, the number of sunspots is at a maximum, with large bipolar sunspots that are oriented in the east–west (left–right) direction within two parallel bands. At times of low activity (top middle), there are no large sunspots and tiny magnetic fields of different magnetic polarity can be observed all over the photosphere. The haze around the images is the inner solar corona. (Courtesy of Carolus J. Schrijver, NSO, NOAO and NSF.) ISBN: 978-3-540-76952-1 e-ISBN: 978-3-540-76953-8 Library of Congress Control Number: 2008933407 c Springer-Verlag Berlin Heidelberg 2009 This work is subject to copyright.