Geomagnetic Storms and the US Power Grid
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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. -
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. -
Planetary Magnetospheres
CLBE001-ESS2E November 9, 2006 17:4 100-C 25-C 50-C 75-C C+M 50-C+M C+Y 50-C+Y M+Y 50-M+Y 100-M 25-M 50-M 75-M 100-Y 25-Y 50-Y 75-Y 100-K 25-K 25-19-19 50-K 50-40-40 75-K 75-64-64 Planetary Magnetospheres Margaret Galland Kivelson University of California Los Angeles, California Fran Bagenal University of Colorado, Boulder Boulder, Colorado CHAPTER 28 1. What is a Magnetosphere? 5. Dynamics 2. Types of Magnetospheres 6. Interaction with Moons 3. Planetary Magnetic Fields 7. Conclusions 4. Magnetospheric Plasmas 1. What is a Magnetosphere? planet’s magnetic field. Moreover, unmagnetized planets in the flowing solar wind carve out cavities whose properties The term magnetosphere was coined by T. Gold in 1959 are sufficiently similar to those of true magnetospheres to al- to describe the region above the ionosphere in which the low us to include them in this discussion. Moons embedded magnetic field of the Earth controls the motions of charged in the flowing plasma of a planetary magnetosphere create particles. The magnetic field traps low-energy plasma and interaction regions resembling those that surround unmag- forms the Van Allen belts, torus-shaped regions in which netized planets. If a moon is sufficiently strongly magne- high-energy ions and electrons (tens of keV and higher) tized, it may carve out a true magnetosphere completely drift around the Earth. The control of charged particles by contained within the magnetosphere of the planet. -
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. -
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. -