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The science behind our Sun and its interaction with Earth The
The science behind our Sun and its interaction with Earth The

Magnetic Force on a Current-Carrying Wire - Easy Peasy All-in
Magnetic Force on a Current-Carrying Wire - Easy Peasy All-in

... 100 loops or turns, and contains a current of 0.045 A. The coil is placed in a uniform magnetic field of magnitude 0.15 T. (a) Determine the magnetic moment of the coil. (b) Find the maximum torque that the magnetic field can exert on the coil. ...
Origin of the Solar System
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... generations of stars within our galaxy. ! •  This gas consisted of 98% hydrogen and helium and 2% heavy elements (by mass).! ...
Magnetic Field Variations - West Virginia University
Magnetic Field Variations - West Virginia University

Magnetic field produced by a moving point charge
Magnetic field produced by a moving point charge

Magnetic Materials Background: 12. Other Materials
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... and Fe. Terfenol is used for position and field sensors, as well as mechanical actuators and speakers. Magnetostrictive position / load sensors work by the fact that when a magnetostrictive material experiences a strain then the magnetisation of the material will change. Terfenol actuators usually h ...
INFORMATION ON ELECTRIC AND MAGNETIC FIELDS Willoughby
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... with the current. In combination, these fields cause energy to be transferred along electric wires. With both electric and magnetic fields, the strength of the field is strongest when close to its source and diminishes rapidly with distance from the source. Many common materials, such as brickwork o ...
A multi-instrument analysis of sunspot umbrae
A multi-instrument analysis of sunspot umbrae

... The recent solar minimum and rise phase of solar cycle 24 have been unlike any period since the early 1900s. We examine some properties of sunspot umbrae over the last 17 years with three different instruments on the ground and in space: MDI, HMI and BABO. The distribution of magnetic fields and the ...
FGT3_ConcepTestsch28 quiz
FGT3_ConcepTestsch28 quiz

Changing Magnetic Fields and Electrical Current
Changing Magnetic Fields and Electrical Current

... Introduction: For a very long time, electricity and magnetism were seen as two separate phenomena. The first hints that they were related came when in April of 1820 Hans Christian Ørsted discovered that electrical currents can produce magnetic fields when during one of his lectures while demonstrati ...
GY305 Lecture3 Geomagnetics
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Solar Abundance of the Elements

... World War despite Harkins’ earlier warning about using atmospheric abundances and Russell’s comment [4] that "The calculated abundance of hydrogen in the sun’s atmosphere is almost incredibly great" (p. 70). Most modern estimates for the abundance of H, He and other light, volatile elements are base ...
Introduction to Geomagnetism - Center for Science Education
Introduction to Geomagnetism - Center for Science Education

... Substantial work on magnetism, particularly terrestrial magnetism, was described in 1600 by Dr. William Gilbert. In an introduction to his book De Magnete, Gilbert debunks many of the older ideas of the causes and properties of magnetism. He attacked alchemists for their obscure language, and put ma ...
questions with answers on electromagnetism
questions with answers on electromagnetism

... The strength of the magnetic field is proportional to the current in the wire. If you double the current, the magnetic force is doubled. Since Voltage = Current x Resistance (V = I*R), you can double the current in a wire by doubling the voltage of the source of electricity. Turns of coil If you wra ...
MAGNETISM Time Allowed : 3 hours Maximum Marks : 70 (a) All
MAGNETISM Time Allowed : 3 hours Maximum Marks : 70 (a) All

... clockwise direction. The coil is placed in a uniform magnetic field of 10T. Find the torque that will act on the coil when the direction of magnetic field is a.> Parallel to the plane of the coil b.> Perpendicular to the plane of the coil. Also find the net force acting on the coil in both cases. Q. ...
Global coupling at 660 km is proposed to explain plate tectonics and
Global coupling at 660 km is proposed to explain plate tectonics and

... The experimentally determined solidus of the anhydrous peridotite KLB-1 (Herzberg, 2000; Zhang and Herzberg, 1994) relevant for such a mantle, is hundreds of degrees higher than the expected temperatures of an average mantle. In contrast, the presence of partial melt in the low velocity zone (Gutenb ...
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the sun part 2

... amount of energy (this is called MAGNETIC RECONNECTION). This magnetic energy released into the solar atmosphere heats up the chromospheres and the corona. Since the bases of the magnetic field lines are the sunspots, the most active parts of the chromosphere and corona are above the sunspots. The g ...
Basic Magnetism
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... Pluto's compact moon system [9], Haumea's collisional family [10], several binary or single satellite systems (e.g, 1999 TC36, Eris, Quaoar and several Centaur objects) [11] and even ring systems around Centaurs, which may have embedded tiny moons [12, 13]. Despite multiple dynamical perturbations a ...
Name - H-W Science Website
Name - H-W Science Website

... direction which is horizontal, or parallel to the surface of the earth. However, at the north magnetic pole a compass would dip straight down vertically. Most compasses are not able to move vertically, so a dip needle can be used to illustrate the vertical movement. The angle formed by the dip needl ...
Chapter 36 – Magnetism
Chapter 36 – Magnetism

Lecture 12 - UConn Physics
Lecture 12 - UConn Physics

... through a wire which is wrapped n turns per unit length on a cylinder of radius a and length L. • If a << L, the B field is to first order contained within the solenoid, in the axial direction, and of constant magnitude. In this limit, we can calculate the field using Ampere's Law. ...
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Geomagnetic storm



A geomagnetic storm is a temporary disturbance of the Earth's magnetosphere caused by a solar wind shock wave and/or cloud of magnetic field that interacts with the Earth's magnetic field. The increase in the solar wind pressure initially compresses the magnetosphere. The solar wind's magnetic field interacts with the Earth’s magnetic field and transfers an increased energy into the magnetosphere. Both interactions cause an increase in plasma movement through the magnetosphere (driven by increased electric fields inside the magnetosphere) and an increase in electric current in the magnetosphere and ionosphere.During the main phase of a geomagnetic storm, electric current in the magnetosphere creates a magnetic force that pushes out the boundary between the magnetosphere and the solar wind. The disturbance in the interplanetary medium that drives the storm may be due to a solar coronal mass ejection (CME) or a high speed stream (co-rotating interaction region or CIR) of the solar wind originating from a region of weak magnetic field on the Sun’s surface. The frequency of geomagnetic storms increases and decreases with the sunspot cycle. CME driven storms are more common during the maximum of the solar cycle, while CIR driven storms are more common during the minimum of the solar cycle.Several space weather phenomena tend to be associated with or are caused by a geomagnetic storm. These include: solar energetic Particle (SEP) events, geomagnetically induced currents (GIC), ionospheric disturbances that cause radio and radar scintillation, disruption of navigation by magnetic compass and auroral displays at much lower latitudes than normal. In 1989, a geomagnetic storm energized ground induced currents that disrupted electric power distribution throughout most of the province of Quebec and caused aurorae as far south as Texas.
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