jamming magnetic field - traducción al ruso
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jamming magnetic field - traducción al ruso

SPATIAL DISTRIBUTION OF VECTORS ALLOWING THE CALCULATION OF THE MAGNETIC FORCE ON A TEST PARTICLE
Magnetic flux density; B-Field; B-field; Magnetic field density; Magnetic Field; Magnetic field strength; Magnetic force field; Nonlinear magnetic field; Magnetic fields; Magnetic Flux Density; H-field; Magnatic field; B-fields; Magnetic field lines; Magnetic field line; Magnetizing field; Auxiliary magnetic field; H field; Effective magnetic field; Potential magnetic field; Magnetic field intensity; Strong magnetic field; Magnetic field energy density; Magnetic Field Energy Density; Magnetic field vector; Magnetic lines of force; Amperes per meter; Amperes per metre; Applied magnetic field; Ampere per metre; Magnetic vector
  • [[Hans Christian Ørsted]], ''Der Geist in der Natur'', 1854
  • The shape of the magnetic field produced by a [[horseshoe magnet]] is revealed by the orientation of iron filings sprinkled on a piece of paper above the magnet.
  • A sketch of Earth's magnetic field representing the source of the field as a magnet. The south pole of the magnetic field is near the geographic north pole of the Earth.
  • A [[Solenoid]] with electric current running through it behaves like a magnet.
  • '''M'''}} inside and outside a cylindrical bar magnet.

jamming magnetic field      
маскирующее магнитное поле
geomagnetism         
  • Variations in virtual axial dipole moment since the last reversal.
  • archive-date=18 January 2015 }}</ref>
  • Estimated declination contours by year, 1590 to 1990 (click to see variation).
  • Relationship between Earth's poles. A1 and A2 are the geographic poles; B1 and B2 are the geomagnetic poles; C1 (south) and C2 (north) are the magnetic poles.
  • Strength of the axial dipole component of Earth's magnetic field from 1600 to 2020.
  • Geomagnetic polarity during the late [[Cenozoic Era]]. Dark areas denote periods where the polarity matches today's polarity, light areas denote periods where that polarity is reversed.
  • date=January 2022}}
  • access-date=13 October 2011}}</ref>
  • The movement of Earth's North Magnetic Pole across the Canadian arctic.
  • T]].
  • An artist's rendering of the structure of a magnetosphere. 1)&nbsp;Bow shock. 2)&nbsp;Magnetosheath. 3)&nbsp;Magnetopause. 4)&nbsp;Magnetosphere. 5)&nbsp;Northern tail lobe. 6)&nbsp;Southern tail lobe. 7)&nbsp;Plasmasphere.
  • ℓ-<var>m</var>}} circles of equal latitude. The function changes sign each ℓtime it crosses one of these lines.
  • Example of a quadrupole field. This can also be constructed by moving two dipoles together.
  • Common coordinate systems used for representing the Earth's magnetic field.
MAGNETIC FIELD THAT EXTENDS FROM THE EARTH'S INNER CORE TO WHERE IT MEETS THE SOLAR WIND
Geomagnetism; Geomagnetic; Earth Magnetism; Geomagnetic field; Terrestrial magnetism; Earths magnitism; Magnetic field of earth; Magnetic field of the earth; Geomagnetics; Earths Magnetic Field; Earth magnetic field; Geomagnetic Field; Geomagnetic maximum; Earths magnetic field; The earth's magnetic field; Surface magnetic field; Magnetologist; Magnetic field of the Earth; Magnetic Field of Earth; Earth's magnetism; Earth's magnetic poles

общая лексика

геомагнетизм

magnetologist         
  • Variations in virtual axial dipole moment since the last reversal.
  • archive-date=18 January 2015 }}</ref>
  • Estimated declination contours by year, 1590 to 1990 (click to see variation).
  • Relationship between Earth's poles. A1 and A2 are the geographic poles; B1 and B2 are the geomagnetic poles; C1 (south) and C2 (north) are the magnetic poles.
  • Strength of the axial dipole component of Earth's magnetic field from 1600 to 2020.
  • Geomagnetic polarity during the late [[Cenozoic Era]]. Dark areas denote periods where the polarity matches today's polarity, light areas denote periods where that polarity is reversed.
  • date=January 2022}}
  • access-date=13 October 2011}}</ref>
  • The movement of Earth's North Magnetic Pole across the Canadian arctic.
  • T]].
  • An artist's rendering of the structure of a magnetosphere. 1)&nbsp;Bow shock. 2)&nbsp;Magnetosheath. 3)&nbsp;Magnetopause. 4)&nbsp;Magnetosphere. 5)&nbsp;Northern tail lobe. 6)&nbsp;Southern tail lobe. 7)&nbsp;Plasmasphere.
  • ℓ-<var>m</var>}} circles of equal latitude. The function changes sign each ℓtime it crosses one of these lines.
  • Example of a quadrupole field. This can also be constructed by moving two dipoles together.
  • Common coordinate systems used for representing the Earth's magnetic field.
MAGNETIC FIELD THAT EXTENDS FROM THE EARTH'S INNER CORE TO WHERE IT MEETS THE SOLAR WIND
Geomagnetism; Geomagnetic; Earth Magnetism; Geomagnetic field; Terrestrial magnetism; Earths magnitism; Magnetic field of earth; Magnetic field of the earth; Geomagnetics; Earths Magnetic Field; Earth magnetic field; Geomagnetic Field; Geomagnetic maximum; Earths magnetic field; The earth's magnetic field; Surface magnetic field; Magnetologist; Magnetic field of the Earth; Magnetic Field of Earth; Earth's magnetism; Earth's magnetic poles

общая лексика

магнитолог

Definición

грип
ГРИП, ГРИПП, гриппа, ·муж. (·франц. grippe) (мед.). Инфекционная болезнь - катарральное воспаление дыхательных путей, сопровождаемое лихорадочным состоянием; то же, что инфлуэнца
.

Wikipedia

Magnetic field

A magnetic field is a vector field that describes the magnetic influence on moving electric charges, electric currents,: ch1  and magnetic materials. A moving charge in a magnetic field experiences a force perpendicular to its own velocity and to the magnetic field.: ch13 : 278  A permanent magnet's magnetic field pulls on ferromagnetic materials such as iron, and attracts or repels other magnets. In addition, a nonuniform magnetic field exerts minuscule forces on "nonmagnetic" materials by three other magnetic effects: paramagnetism, diamagnetism, and antiferromagnetism, although these forces are usually so small they can only be detected by laboratory equipment. Magnetic fields surround magnetized materials, and are created by electric currents such as those used in electromagnets, and by electric fields varying in time. Since both strength and direction of a magnetic field may vary with location, it is described mathematically by a function assigning a vector to each point of space, called a vector field.

In electromagnetics, the term "magnetic field" is used for two distinct but closely related vector fields denoted by the symbols B and H. In the International System of Units, the unit of H, magnetic field strength, is the ampere per meter (A/m).: 22  The unit of B, the magnetic flux density, is the tesla (in SI base units: kilogram per second2 per ampere),: 21  which is equivalent to newton per meter per ampere. H and B differ in how they account for magnetization. In vacuum, the two fields are related through the vacuum permeability, B / μ 0 = H {\displaystyle \mathbf {B} /\mu _{0}=\mathbf {H} } ; but in a magnetized material, the quantities on each side of this equation differ by the magnetization field of the material.

Magnetic fields are produced by moving electric charges and the intrinsic magnetic moments of elementary particles associated with a fundamental quantum property, their spin.: ch1  Magnetic fields and electric fields are interrelated and are both components of the electromagnetic force, one of the four fundamental forces of nature.

Magnetic fields are used throughout modern technology, particularly in electrical engineering and electromechanics. Rotating magnetic fields are used in both electric motors and generators. The interaction of magnetic fields in electric devices such as transformers is conceptualized and investigated as magnetic circuits. Magnetic forces give information about the charge carriers in a material through the Hall effect. The Earth produces its own magnetic field, which shields the Earth's ozone layer from the solar wind and is important in navigation using a compass.

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