The Magnetic Field of Jupiter: A Comparison of Radio Astronomy and Spacecraft Observations
The Magnetic Field of Jupiter: A Comparison of Radio Astronomy and Spacecraft Observations
复制标题
木星的磁场:射电天文学和航天器观测的比较
DOI:
10.1146/annurev.ea.07.050179.002125
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发表时间:
1979
影响因子:
14.9
通讯作者:
S. Gulkis
中科院分区:
文献类型:
--
作者:
E. Smith;S. Gulkis
The planet Jupiter is known to possess a strong magnetic field. First revealed to radio astronomers in the mid-1950s through its polarized radio emissions at decametric and decimetric wavelengths, the magnetic field was later ( 1973 and 1974) sampled directly by magnetometers on board the Pioneer 10 and Pioneer 1 1 spacecraft which passed within 2.84 and 1 .59 jovian radii (rJ) respectively of Jupiter. Within about 10rJ of the center of Jupiter, a region we call the inner magnetosphere, the magnetic field is in the first approximation a dipole field associated with currents interior to the planet. Outside of this region, the planetary magnetic field is affected by currents external to the planet and the field departs significantly from a dipole. Recent review articles of the in situ magnetic field measurements and of the radio astronomical measurements can be found in the book Jupiter edited by T. Gehrels (1976). The radio astronomical measurements of the decimetric radiation and the in situ measurements give information on the magnetic field in the overlapping spatial domain from about 1.6rJ to 4rJ. The continuous decimetric emissions, which were successfully interpreted in the early 1960s as synchrotron radiation from relativistic electrons trapped in a planetary magnetic field, have allowed well-founded inferences to be drawn regarding the properties of the field and the trapped particles. In the range of overlap, good agreement has been obtained with the in situ measurements of Jupiter's vector dipole magnetic moment. The dipole moment is �4.2 gauss rJ, is tilted � 10° with respect to Jupiter's