The Economic Impact of Critical National Infrastructure Failure Due to Space Weather
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UC Irvine UC Irvine Previously Published Works
UC Irvine UC Irvine Previously Published Works Title Astrophysics in 2006 Permalink https://escholarship.org/uc/item/5760h9v8 Journal Space Science Reviews, 132(1) ISSN 0038-6308 Authors Trimble, V Aschwanden, MJ Hansen, CJ Publication Date 2007-09-01 DOI 10.1007/s11214-007-9224-0 License https://creativecommons.org/licenses/by/4.0/ 4.0 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Space Sci Rev (2007) 132: 1–182 DOI 10.1007/s11214-007-9224-0 Astrophysics in 2006 Virginia Trimble · Markus J. Aschwanden · Carl J. Hansen Received: 11 May 2007 / Accepted: 24 May 2007 / Published online: 23 October 2007 © Springer Science+Business Media B.V. 2007 Abstract The fastest pulsar and the slowest nova; the oldest galaxies and the youngest stars; the weirdest life forms and the commonest dwarfs; the highest energy particles and the lowest energy photons. These were some of the extremes of Astrophysics 2006. We attempt also to bring you updates on things of which there is currently only one (habitable planets, the Sun, and the Universe) and others of which there are always many, like meteors and molecules, black holes and binaries. Keywords Cosmology: general · Galaxies: general · ISM: general · Stars: general · Sun: general · Planets and satellites: general · Astrobiology · Star clusters · Binary stars · Clusters of galaxies · Gamma-ray bursts · Milky Way · Earth · Active galaxies · Supernovae 1 Introduction Astrophysics in 2006 modifies a long tradition by moving to a new journal, which you hold in your (real or virtual) hands. The fifteen previous articles in the series are referenced oc- casionally as Ap91 to Ap05 below and appeared in volumes 104–118 of Publications of V. -
Progress in Space Weather Modeling in an Operational Environment
J. Space Weather Space Clim. 3 (2013) A17 DOI: 10.1051/swsc/2013037 Ó I. Tsagouri et al., Published by EDP Sciences 2013 RESEARCH ARTICLE OPEN ACCESS Progress in space weather modeling in an operational environment Ioanna Tsagouri1,*, Anna Belehaki1, Nicolas Bergeot2,3, Consuelo Cid4,Ve´ronique Delouille2,3, Tatiana Egorova5, Norbert Jakowski6, Ivan Kutiev7, Andrei Mikhailov8, Marlon Nu´n˜ez9, Marco Pietrella10, Alexander Potapov11, Rami Qahwaji12, Yurdanur Tulunay13, Peter Velinov7, and Ari Viljanen14 1 National Observatory of Athens, P. Penteli, Greece *Corresponding author: e-mail: [email protected] 2 Solar-Terrestrial Centre of Excellence, Brussels, Belgium 3 Royal Observatory of Belgium, Brussels, Belgium 4 Universidad de Alcala´, Alcala´ de Henares, Spain 5 Physikalisch-Meteorologisches Observatorium Davos and World Radiation Center (PMOD/WRC), Davos, Switzerland 6 German Aerospace Center, Institute of Communications and Navigation, Neustrelitz, Germany 7 Bulgarian Academy of Sciences, Sofia, Bulgaria 8 Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation (IZMIRAN), Troitsk, Moscow Region, Russia 9 Universidad de Ma´laga, Ma´laga, Spain 10 Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy 11 Institute of Solar-Terrestrial Physics SB RAS, Irkutsk, Russia 12 University of Bradford, Bradford, UK 13 Middle East Technical University, Ankara, Turkey 14 Finnish Meteorological Institute, Helsinki, Finland Received 19 June 2012 / Accepted 10 March 2013 ABSTRACT This paper aims at providing an overview of latest advances in space weather modeling in an operational environment in Europe, including both the introduction of new models and improvements to existing codes and algorithms that address the broad range of space weather’s prediction requirements from the Sun to the Earth. -
1859 Carrington Event
Sun – Part 28 - 1859 Carrington event Sunspots recorded by Richard Carrington, 1859 Aurora On 1 September 1859, English astronomer Richard Carrington continued the daytime heliographic measurements of sunspots from his observatory in Surrey, which he had begun in 1857. Sunspot number had been very high ever since 28 August, but, on this particular day, he became one of the first two people to independently make the first observation of a solar flare. The other observer was Richard Hodgson, an amateur astronomer with an observatory in Essex. What they saw, with the naked eye on a projection of the Sun through a telescope onto a screen, was a 'white light flare' in the Sun's photosphere. When Carrington learned that the nearby Kew Observatory magnetometer had concurrently recorded a crochet, an instantaneous perturbation of Earth's ionosphere, he connected the two, identifying that the flare he had observed was associated with the numerous sunspots he had observed during previous days and the terrestrial effects which had been experienced on Earth. The flare was associated with a massive coronal mass ejection (CME) which had begun the 150 million km journey from the Sun 18 hours earlier (normally it takes 3-4 days for a CME to reach Earth). It was proposed that this great speed was facilitated by an earlier CME which had 'cleared the way' a few days earlier. The CME which produced the flare on 1 September 1859 was part of the largest geomagnetic storm ever recorded by ground-based magnetometers. During the 1-2 September storm, aurorae were visible around the world, those in the Northern Hemisphere observed as far south as the Caribbean and sub-Saharan Africa. -
The Grand Aurorae Borealis Seen in Colombia in 1859
The Grand Aurorae Borealis Seen in Colombia in 1859 Freddy Moreno C´ardenasa, Sergio Cristancho S´ancheza, Santiago Vargas Dom´ınguezb aCentro de Estudios Astrof´ısicos, Gimnasio Campestre, Bogot´a, Colombia bUniversidad Nacional de Colombia - Sede Bogot´a- Facultad de Ciencias - Observatorio Astron´omico - Carrera 45 # 26-85, Bogot´a- Colombia Abstract On Thursday, September 1, 1859, the British astronomer Richard Car- rington, for the first time ever, observes a spectacular gleam of visible light on the surface of the solar disk, the photosphere. The Carrington Event, as it is nowadays known by scientists, occurred because of the high solar activity that had visible consequences on Earth, in particular reports of outstanding aurorae activity that amazed thousands of people in the western hemisphere during the dawn of September 2. The geomagnetic storm, generated by the solar-terrestrial event, had such a magnitude that the auroral oval expanded towards the equator, allowing low latitudes, like Panama's 9◦N, to catch a sight of the aurorae. An expedition was carried out to review several his- torical reports and books from the northern cities of Colombia allowed the identification of a narrative from Monter´ıa,Colombia (8◦ 45' N), that de- scribes phenomena resembling those of an aurorae borealis, such as fire-like lights, blazing and dazzling glares, and the appearance of an immense S-like shape in the sky. The very low latitude of the geomagnetic north pole in 1859, the lowest value in over half a millennia, is proposed to have allowed the observations of auroral events at locations closer to the equator, and supports the historical description found in Colombia. -
An Opposite Response of the Low-Latitude Ionosphere at Asian
Originally published as: Xiong, C., Lühr, H., Yamazaki, Y. (2019): An Opposite Response of the Low‐Latitude Ionosphere at Asian and American Sectors During Storm Recovery Phases: Drivers From Below or Above. - Journal of Geophysical Research, 124, 7, pp. 6266—6280. DOI: http://doi.org/10.1029/2019JA026917 RESEARCH ARTICLE An Opposite Response of the Low‐Latitude Ionosphere at 10.1029/2019JA026917 Asian and American Sectors During Storm Recovery Key Points: • The dayside low‐latitude ionosphere Phases: Drivers From Below or Above – on 9 11 September 2017 exhibits Chao Xiong1 , Hermann Lühr1 , and Yosuke Yamazaki1 prominent positive/negative responses at the Asian/American 1GFZ German Research Centre for Geosciences, Potsdam, Germany sectors • The global distribution of thermospheric O/N2 ratio measured by GUVI cannot well explain such Abstract In this study, we focus on the recovery phase of a geomagnetic storm that happened on 6–11 longitudinal opposite response of September 2017. The ground‐based total electron content data, as well as the F region in situ electron ionosphere density, measured by the Swarm satellites show an interesting feature, revealing at low and equatorial • We suggest lower atmospheric forcing the main contributor to the latitudes on the dayside ionosphere prominent positive and negative responses at the Asian and American longitudinal opposite response of longitudinal sectors, respectively. The global distribution of thermospheric O/N2 ratio measured by global – ionosphere on 9 11 September 2017 ultraviolet imager on board the Thermosphere, Ionosphere, Mesosphere Energetics and Dynamics satellite cannot well explain such longitudinally opposite response of the ionosphere. Comparison between the equatorial electrojet variations from stations at Huancayo in Peru and Davao in the Philippines suggests that Correspondence to: the longitudinally opposite ionospheric response should be closely associated with the interplay of E C. -
Solar Flare: the "Carrington Event" of 1859
Chas' Compilation: Solar Flare: The "Carrington Event" of 1859 Chas' Compilation A compilation of information and links regarding assorted subjects: politics, religion, science, computers, health, movies, music... essentially whatever I'm reading about, working on or experiencing in life. Saturday, August 08, 2009 About Me Solar Flare: The "Carrington Event" of 1859 Name: Chas Sprague Location: State of In a post I did a few days ago, about sunspot activity, the famous solar storm of 1859, Jefferson, United States often referred to as the "Carrington Event", was frequently mentioned. I've been I was born and raised in reading up on that, and here is some of the information I found: Connecticut, went to college in Boston, dropped out, moved A Super Solar Flare west to San Francisco where I lived for 23 years. I now live in rural Oregon, At 11:18 AM on the cloudless morning of Thursday, September 1, 1859, enjoying a lifestyle I've longed for. 33-year-old Richard Carrington—widely acknowledged to be one of England's foremost solar astronomers—was in his well-appointed private View my complete profile observatory. Just as usual on every sunny day, his telescope was projecting an 11-inch-wide image of the sun on a screen, and Carrington Previous Posts skillfully drew the sunspots he saw. ● True Health Care Reform: Reduce On that morning, he was capturing the likeness of an enormous group of the "Wedge" sunspots. Suddenly, before his eyes, two brilliant beads of blinding white ● Obama Supporters Can't Take a light appeared over the sunspots, intensified rapidly, and became kidney- Joke shaped. -
Midlatitude Ionospheric F2-Layer Response to Eruptive Solar Events
Midlatitude ionospheric F2-layer response to eruptive solar events-caused geomagnetic disturbances over Hungary during the maximum of the solar cycle 24: a case study K. A. Berényi *,1,2, V. Barta 2, Á. Kis 2 1 Eötvös Loránd University, Budapest, Hungary 2 Research Centre for Astronomy and Earth Sciences, GGI, Hungarian Academy of Sciences, Sopron, Hungary Published in Advances in Space Research Abstract In our study we analyze and compare the response and behavior of the ionospheric F2 and of the sporadic E-layer during three strong (i.e., Dst <-100nT) individual geomagnetic storms from years 2012, 2013 and 2015, winter time period. The data was provided by the state-of the art digital ionosonde of the Széchenyi István Geophysical Observatory located at midlatitude, Nagycenk, Hungary (IAGA code: NCK, geomagnetic lat.: 46,17° geomagnetic long.: 98,85°). The local time of the sudden commencement (SC) was used to characterize the type of the ionospheric storm (after Mendillo and Narvaez, 2010). This way two regular positive phase (RPP) ionospheric storms and one no-positive phase (NPP) storm have been analyzed. In all three cases a significant increase in electron density of the foF2 layer can be observed at dawn/early morning (around 6:00 UT, 07:00 LT). Also we can observe the fade-out of the ionospheric layers at night during the geomagnetically disturbed time periods. Our results suggest that the fade-out effect is not connected to the occurrence of the sporadic E-layers. Keywords: ionospheric storm, geomagnetic disturbance, space weather, midlatitude F2-layer, sporadic E-layer *Corresponding author. -
Extreme Solar Eruptions and Their Space Weather Consequences Nat
Extreme Solar Eruptions and their Space Weather Consequences Nat Gopalswamy NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA Abstract: Solar eruptions generally refer to coronal mass ejections (CMEs) and flares. Both are important sources of space weather. Solar flares cause sudden change in the ionization level in the ionosphere. CMEs cause solar energetic particle (SEP) events and geomagnetic storms. A flare with unusually high intensity and/or a CME with extremely high energy can be thought of examples of extreme events on the Sun. These events can also lead to extreme SEP events and/or geomagnetic storms. Ultimately, the energy that powers CMEs and flares are stored in magnetic regions on the Sun, known as active regions. Active regions with extraordinary size and magnetic field have the potential to produce extreme events. Based on current data sets, we estimate the sizes of one-in-hundred and one-in-thousand year events as an indicator of the extremeness of the events. We consider both the extremeness in the source of eruptions and in the consequences. We then compare the estimated 100-year and 1000-year sizes with the sizes of historical extreme events measured or inferred. 1. Introduction Human society experienced the impact of extreme solar eruptions that occurred on October 28 and 29 in 2003, known as the Halloween 2003 storms. Soon after the occurrence of the associated solar flares and coronal mass ejections (CMEs) at the Sun, people were expecting severe impact on Earth’s space environment and took appropriate actions to safeguard technological systems in space and on the ground. -
Geomagnetic Storms and the US Power Grid
Geomagnetic Storms and the US Power Grid 1 Effects of Space Weather on the US Power Grid • Look at how space weather can affect the electric power grid. • Discuss how the Geomagnetically Induced Currents are introduced into the grid. • Look at how these currents affect the grid – Particularly the effect on large power transformers • Go over a few documented cases • Briefly look at the grid structure and how its design contributes to the problem • Review the results of the simulation a severe solar storm 2 US Electric Grid Interconnections (what is the Electric Grid) • The US Grid Consists of Three Independent AC Systems (Interconnects) – Eastern Interconnection – Western Interconnection – Texas Interconnection • Linked by High Voltage DC Ties – Transmission Network – Distribution Systems – Generating Facilities • T&D dividing line ~100 kV • Distribution systems are regulated by the states • Most Transmission and Generation facilities are fall under the Regulatory Authority of FERC 3 United States Electric Grid Makeup of the Grid •The Distribution System (local utility) delivers the power. •The Transmission system transports power in bulk quantities across the network. •Generation system provides the facilities that make the power. •The majority of Transmission and Generation facilities are part of Bulk Power System •The Bulk Power System is a highly a interconnected system with thousands of 4 pathways and interconnections United States Transmission Grid Transmission System consists of over: 180,000 miles of HV Transmission Lines - 80,000 -
Global Ionospheric Storms
Global Ionospheric Storms Anthony J. Mannucci Jet Propulsion Laboratory, California Institute Of Technology THEME: Atmosphere-Ionosphere-Magnetosphere Interactions EXECUTIVE SUMMARY We discuss Global Ionospheric Storms as an important sub-field of study within solar and space physics. Significant science questions are discussed as well as methods to address them. Progress requires a robust observational approach that includes thermosphere/ionosphere imaging combined with in-situ measurements from space and ground-based measurements from globally distributed instruments. Because of the large-scale changes that occur over time scales of minutes, instruments operating continuously are needed to form the core observations. Small satellite constellations are also well suited to the study of GIS to characterize local time dependence of the ionospheric response. 1. Scientific Challenge Understanding the storm-time ionosphere is fundamental to solar and space physics. Significant scientific attention and resources have been devoted to this topic over the last few decades, yet it remains fresh. Knowledge has been gained over the years, certainly a triumph for our field, yet this knowledge remains insufficient to predict how the ionosphere will behave during the next storm with a high level of confidence. We consider here “ionospheric behavior” in its broadest sense: behavior that spans time scales from minutes to days, and spatial scales from hundreds of meters to thousands of kilometers. The concerted effort of the past decades has provided an appreciation of the various physical phenomena that play a role in the ionospheric response to storms, yet we cannot pin down with confidence what will happen in any given event. The remaining gaps in our understanding are due to limited observations that are not up to the task of constraining the scientific hypotheses. -
Top-Side Ionosphere Response to Extreme Solar Events
Ann. Geophys., 24, 1469–1477, 2006 www.ann-geophys.net/24/1469/2006/ Annales © European Geosciences Union 2006 Geophysicae Top-side ionosphere response to extreme solar events A. V. Dmitriev1,2, H.-C. Yeh1, J.-K. Chao1, I. S. Veselovsky2,3, S.-Y. Su1, and C. C. Fu1 1Institute of Space Science, National Central University, Chung-Li, Taiwan 2Skobeltsyn Institute of Nuclear Physics Moscow State University, Moscow, Russia 3Space Research Institute (IKI) Russian Academy of Sciences, Moscow, Russia Received: 17 August 2005 – Revised: 27 January 2006 – Accepted: 14 Febraury 2006 – Published: 3 July 2006 Part of Special Issue “The 11th International Symposium on Equatorial Aeronomy (ISEA-11), Taipei, May 2005” Abstract. Strong X-flares and solar energetic particle (SEP) particles (SEP), with energies up to hundreds and thousands fluxes are considered as sources of topside ionospheric dis- of MeV. The solar radiation impacts the Earth’s ionosphere turbances observed by the ROCSAT-1/IPEI instrument dur- almost immediately. The impact depends on the spectrum ing the Bastille Day event on 14 July 2000 and the Halloween and contents of the radiation (e.g. Mitra, 1974). event on 28 October–4 November 2003. It was found that The present study regards two outstanding events which within a prestorm period in the dayside ionosphere at alti- occurred in the 23 solar cycle: Bastille Day on 14 July tudes of ∼600 km the ion density increased up to ∼80% in 2000 and the Halloween event on 28 October–4 Novem- response to flare-associated enhancements of the solar X-ray ber 2003. The Bastille Day solar flare on 14 July had a emission. -
Download of RINEX files for All the GNSS Stations for the Previous 3 Days; 2
remote sensing Article IONORING: Real-Time Monitoring of the Total Electron Content over Italy Claudio Cesaroni 1,* , Luca Spogli 1,2 and Giorgiana De Franceschi 1 1 Istituto Nazionale di Geofisica e Vulcanologia, 00143 Rome, Italy; [email protected] (L.S.); [email protected] (G.D.F.) 2 SpacEarth Technology, 00143 Rome, Italy * Correspondence: [email protected] Abstract: IONORING (IONOspheric RING) is a tool capable to provide the real-time monitoring and modeling of the ionospheric Total Electron Content (TEC) over Italy, in the latitudinal and longitudinal ranges of 35◦N–48◦N and 5◦E–20◦E, respectively. IONORING exploits the Global Navigation Satellite System (GNSS) data acquired by the RING (Rete Integrata Nazionale GNSS) network, managed by the Istituto Nazionale di Geofisica e Vulcanologia (INGV). The system provides TEC real-time maps with a very fine spatial resolution (0.1◦ latitude x 0.1◦ longitude), with a refresh time of 10 min and a typical latency below the minute. The TEC estimated at the ionospheric piercing points from about 40 RING stations, equally distributed over the Italian territory, are interpolated using locally (weighted) regression scatter plot smoothing (LOWESS). The validation is performed by comparing the IONORING TEC maps (in real-time) with independent products: (i) the Global Ionospheric Maps (GIM) - final product- provided by the International GNSS Service (IGS), and (ii) the European TEC maps from the Royal Observatory of Belgium. The validation results are satisfactory in terms of Root Mean Square Error (RMSE) between 2 and 3 TECu for both comparisons. The potential of IONORING in depicting the TEC daily and seasonal variations is analyzed over 3 years, from May 2017 to April 2020, as well as its capability to account for the effect of the disturbed Citation: Cesaroni, C.; Spogli, L.; De Franceschi, G.