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2.4 Jupiter's Geomagnetism

-Jupiter's geomagnetic effects cannot be explained by considering the magnetic field lines first.-

2.4.1 Characteristics of charged particles of Jupiter

 Jupiter rotates counterclockwise wise like the Earth, but Jupiter's geomagnetism is opposite to the Earth's geomagnetic field. Furthermore, as shown in Fig. 2.4.1, auroras sometimes appear only at the north pole area of Jupiter. Considering magnetic field lines, the magnetic field lines do not differ between north pole area and south. The explanation that charged particles wrap around magnetic field lines and move along magnetic field lines is differed from the facts. The magnetic field lines considered as the basis of the explanation have no reaction and indicate the direction of magnetic action. A substantial moving charged particle exerts a magnetic effect on other moving charged particles. Between charged particles running in parallel, the energy is magnetically low. This chain of magnetic couplings explains Jupiter's magnetism by considering moving charged particles first.


   Fig. 2.4.1 Air currents orbiting Jupiter and auroras at the North Pole
  Origin of this CG::28257_jovian_aurora.jpg (640×640) (astroarts.co.jp) 

2.4.2 Formation of Jupiter's magnetics

As shown in Fig. 2.4.2, there are charged particles in a thick liquid metallic state inside the star. It has been thought that Jupiter's geomagnetic field is generated by the motion of the group of charged particles. If the geomagnetism of the Earth is mainly generated by the motion of charged particles in the upper sky, the direction of the Earth's geomagnetic field is opposite to that of Jupiter. Therefore, Jupiter's geomagnetic field is explained by the charged particles on move inside of the Jupiter as shown in Fig. 2.4.3.  

   
    Fig. 2.4.2 Internal structure of Jupiter         Fig. 2.4.3 Geomagnetic of Jupiter

2.4.3 Plasma torus of Io's of Jupiter

 The northern lights of Jupiter, shown in Fig. 2.4.1, have bright spots corresponding to the Galilean moons. The bright spots of the auroras are located at high to low latitudes, corresponding to the distant order of Io, Europa, and Ganymede. The atmosphere of Jupiter's Galilean moons is rarefied. All Galilean satellites have the same revolution and rotation periods, and their own rotation is slow, so there is no geomagnetism.
Fig. 2.4.5 shows how the rotation of the Io-plasma torus through the rotation of the magnetosphere due to Jupiter's rotation provides a high-speed tailwind for ionization of Io's atmosphere and the generation of plasma flow. Jupiter's geomagnetic field rotates in the same period as Jupiter's rotation in 10 hour(0.4135 days). Io orbits Jupiter in a radius of 4.217x105 km iat period of 1.77 days. Therefore, the kinetic energy of the collision betwee charged particle H+ and ions are shown in Table 2.4.1. The magnitude of the kinetic energy of this H+ is sufficient to ionize paticles


 Table 2.4.1 Physical power of collision by H +’s those are magnetic coupling with rotating Jupiter

  Orbital radius   Orbital period   Orbital speed   Difference of speed   Energy of Collision  
Revolution of Io   4.217x105 km  1.77days   17.3 km/sec   
 Jupiter's geomagnetic   Location of Io   0.4135days   74.1 km/sec  56.8 km/sec   16.8eV 

Tsuchiya, et al., using the Hisaki, space telescope for planetary observation, showed that the extreme ultraviolet emission of sulfide ions in Io's plasma torus becomes stronger downstream of Io as shown as shown in Fig. 2.4.4.


Fig.2.4.4 Io's plasma torus [1]

[1]:[Journal of Geophysical Research Space Physics: Local electron heating in the Io plasma torus associated with Io from HISAKI satellite observation https://doi.org/10.1002/2015JA021420 ]https://www.astroarts.co.jp/article/assets/2016/05/4302_illustration.jpg

2.4.4 Jupiter's geomagnetism sweeps Galilean satellites to produce plasma

Jupiter's outer charged particle swarm chained by magnetic coupling with the charged particle group inside Jupiter, which rotates at high speed, sputters the Galilean moons and generates ions. The ion groups are distributed in a doughnut shape, as shown in Fig. 2.4.5.
Since the speed of the orbiting ions slows down in the regions of the North and South Poles, they fall to Jupiter by gravity and generate aurora. Therefore, auroras change slowly because ions fall due to gravity. (last modified April 21, 2023)


Fig. 2.4.5 Doughnut-shaped charged particles associated with Jupiter's Galilean moons

 
  Index                 -2.4-