Theory Observation
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Magnetosphere
Earth, like planets, Sun and even galaxies is surrounded by a large magnetic field. For Earth, this is the so-called magnetosphere. Magnetosphere is a vast comet-tail shaped area beginning at Earth Sun side and extending beyond Earth. It is the space manifestation of Earth's magnetic field, the one which acts upon compass' needle. Earth's magnetic field is a gigantic dipole magnet axis of which is slightly different from Earth's axis; this difference yields magnetic poles being located at different places than geographical ones. Earth magnetic lines extend into surrounding space
It is the solar wind which is shaping Earth's magnetosphere: sunwards the solar wind compresses Earth's magnetic field; on the opposite side it shapes it comet-tail. Solar wind is a ions plasma emanating from Sun and carrying with it the latter's magnetic field. Sunwards, solar wind hits magnetosphere at the bow shock. It is the place where Earth's magnetic field abruptly deflects solar particles and magnetic field. This compressed part of the magnetosphere extends to about 6-10 Earth radii from Earth. The encounter between the solar wind and Earth's magnetic field is generating sonic booms! Two polar cusps along magnetosphere axis allow solar wind to reach upper part of the atmosphere. Magnetosphere's comet-tail side extends up to 1,000 Earth radii. Some solar particles which somehow managed to reach there form the "plasma sheet". The so-called neutral sheet stays at the middle of it. It is where northern and southern part of the Earth's magnetic field cancel. Plasma sheet is too a coating of sort for magnetosphere's tail. Each side of plasma sheet are found tail lobes. Boundary between magnetosphere and interplanetary medium is called the magnetopause
Related to Earth protective shield are too an Earth atmosphere's part and the famous Van Allen belts. Ionosphere is Earth's atmospheric layer populated by charged particles. A part of these particles leaks into the plasmasphere which is a spherical zone more directly part of magnetosphere. In plasmasphere are found Van Allen belts. Van Allen belts are tori of charged particles: inner belt is made of high-energy protons resulting from upper atmosphere being knocked by cosmic rays as outer belt is high-energy electrons yielded by cosmic rays and magnetosphere acceleration Strong Events Inside the Van Allen Belts Magnetosphere is a dynamic medium in connection with solar wind especially with solar eruptions. These may lead to magnetosphere's outer part being punctured magnetotail side, solar wind and magnetic lines enter there and break Earth magnetic lines. Ensuing mixed solar-Earth magnetic lines flow into tail, compressing plasmasheet from both sides. Earth parts of magnetic lines eventually reconnect. Earthside lines violently snap back Earth (this is a so-called "reconnection" process); they carry solar wind particles with them; these funnel into polar cusps down to upper atmosphere and yield the famous auroras or Northern Lights through an 'auroral oval'. Sudden, powerful brightening, and increased dynamism of Northern Lights are called 'substorms', as their mechanism is still ill-known. In any case, they originate into the magnetosphere's tail, from where an increase in the solar particles snaps back into the northern regions of Earth. On magnetosphere's tail side a solar plasma bubble is expelled from magnetosphere. Solar events and auroras may work too directly from magnetosphere Sun's side: solar and terrestrial lines connect yielding so-called "cracks" which are punctures in Earth magnetic shield. Solar wind enters puncture and follows magnetic lines to polar cusps there too yielding Northern Lights. Recent findings showed that cracks may last up to 9 hours Ion Plumes in the Ionosphere, a By-Product of Geo-Magnetic Storms As far as the origins of the Earth's magnetic field are concerned, they are thought to be due to the interaction between the two varieties of Earth's core: a liquid core exists around a solid inner core and both acts like a dynamo. Earth's magnetic field is a living system. Its axis e.g. is varying and as a result magnetic poles are drifting: north magnetic pole is drifting from Canada to Siberia. Another major change the magnetic field endures is reversals: it flips, north pole becoming south and vice versa. These reversals occur about each 300,000 years. Last occurred 780,000 years ago. Reversals do not occur suddenly but they take a few thousand years to complete. During this evolving phase, the magnetic field does not show its dipole bar magnet classical aspect anymore: its it tangled and complicated instead, magnetic poles may be located anywhere on Earth's surface, and there may be more of them than the usual two. Reversals modify magnetosphere but do not make it disappear however and it still protects Earth. Earth's magnetic field has been monitored to have weakened by 10 per cent since the 19th century. This decline has to be put in perspective however as the field today is about twice as strong as normal. It is thought too that this decline would better be the sign that the magnetic field is at the onset of a so-called "excursion" which sees the field swiftly reverse and back over a period of about 400 years Themis sees More About the Geomagnetic Substorms and Auroras The Plasmasphere, the Major Contributor to the Magnetosphere During Superstorms!
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