木星の磁気圏の黄昏の側面である
W S Kurth1, D A Gurnett, G B Hospodarsky
1Department of Physics and Astronomy, University of Iowa, Iowa City, Iowa 52242, USA. william-kurth@uiowa.edu
Nature
|March 5, 2002
まとめ
木星の磁気圏は,地球の磁気圏と似て,太陽風の圧力によって縮小し,膨張する. この研究では,この行動を確認するために2点測定を用いて,木星の磁気断層内の境界層の証拠が見つかりました.
科学分野:
- 惑星科学は惑星科学である.
- 宇宙物理学 宇宙物理学
- 磁気圏物理学 磁気圏物理学
背景:
- 木星の磁気断絶の動態は,以前は限られた単一の宇宙船データから推測されていた.
- 地球の磁気断層の動きは,複数の宇宙船の観測を用いてよく研究されています.
研究 の 目的:
- 太陽風の圧力変動に対する木星の磁気停滞反応を調査するために.
- 地球の磁気圏と木星の磁気断層の行動を比較するために.
主な方法:
- 木星の磁気断絶のほぼ同時2点測定を用いた.
- マグネトパウズサイズが大きいから小さいへの移行中にデータを分析した.
主要な成果:
- 木星の磁気断層は,太陽風の圧力変化に反応して,地球の磁気断層と同じような内向/外向の動きを示しています.
- 木星に対する地球ベースの磁気圏物理学の妥当性を確認しました.
- マグネトパウスの内部で,よく発達した境界層の証拠を観測した.
結論:
- 木星の磁気断層が太陽風の圧力に与える反応は,地球の磁気断層と類似しています.
- マグネトパウズダイナミクスを支配する物理は,異なる惑星にわたって保存されています.
- 木星の磁気圏内には,明確な境界層が存在する.
関連する概念動画
Magnetic Fields
A moving charge or a current creates a magnetic field in the surrounding space, in addition to its electric field. The magnetic field exerts a force on any other moving charge or current that is present in the field. Like an electric field, the magnetic field is also a vector field. At any position, the direction of the magnetic field is defined as the direction in which the north pole of a compass needle points.
A magnetic field is defined by the force that a charged particle experiences...
A magnetic field is defined by the force that a charged particle experiences...
Magnetic Field Lines
The representation of magnetic fields by magnetic field lines is very useful in visualizing the strength and direction of the magnetic field. Each of the magnetic field lines forms a closed loop. The field lines emerge from the north pole (N), loop around to the south pole (S), and continue through the bar magnet back to the north pole.
Magnetic field lines follow several hard-and-fast rules:
Magnetic field lines follow several hard-and-fast rules:
Diamagnetism
Materials consisting of paired electrons have zero net magnetic moments. However, when these materials are placed under an external magnetic field, the moments opposite to the field are induced. Such materials are called diamagnets. Diamagnetism is the response of the diamagnets when placed in an external magnetic field.
Diamagnetism was discovered by Anton Brugmans in 1778 when he observed that bismuth gets repelled by magnetic fields, thus theorizing that diamagnets get repelled by magnets.
Diamagnetism was discovered by Anton Brugmans in 1778 when he observed that bismuth gets repelled by magnetic fields, thus theorizing that diamagnets get repelled by magnets.
Magnetostatic Boundary Conditions
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Magnetic Damping
Eddy currents can produce significant drag on motion, called magnetic damping. For instance, when a metallic pendulum bob swings between the poles of a strong magnet, significant drag acts on the bob as it enters and leaves the field, quickly damping the motion.
If, however, the bob is a slotted metal plate, the magnet produces a much smaller effect. When a slotted metal plate enters the field, an emf is induced by the change in flux; however, it is less effective because the slots limit the...
If, however, the bob is a slotted metal plate, the magnet produces a much smaller effect. When a slotted metal plate enters the field, an emf is induced by the change in flux; however, it is less effective because the slots limit the...
Magnetic Declination
Magnetic declination is the angle between true north, which aligns with the Earth's rotational axis, and magnetic north, which follows the direction of the Earth's magnetic field. This discrepancy exists because the magnetic poles do not coincide with the geographic poles. The value of magnetic declination depends on the observer's location on Earth and is subject to changes over time due to the dynamic nature of the Earth's magnetic field.The declination is called eastern when magnetic north...


