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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Polarization and phase of planetary-period magnetic field oscillations on high-latitude field lines in Saturn's magnetosphere
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Polarization and phase of planetary-period magnetic field oscillations on high-latitude field lines in Saturn's magnetosphere

机译:土星磁层高纬度磁力线上行星周期磁场振荡的极化和相位

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We examine magnetic field data obtained by the Cassini spacecraft on a sequence of high-latitude orbits in Saturn's magnetosphere spanning October 2006 to May 2007 to determine whether planetary-period oscillations are present on polar open field lines, such as have been found previously in near-equatorial magnetic field data. Such oscillations are found generally to be present with amplitudes ~0.5–1 nT, somewhat smaller than the few nT amplitudes typical of the quasi-dipolar equatorial region. The polarization characteristics in the northern and southern polar regions are determined and found to differ significantly from those in the equatorial region. The phases of the oscillations in the northern and southern hemispheres are also determined relative to the equatorial oscillations, and hence relative to each other, requiring extension of the equatorial oscillation phase model to the end of 2007, spanning the interval of high-latitude orbits. The results show that the overall pattern of field oscillations is not consistent with a rotating external current system that mimics a rotating transverse dipole in the outer regions. Rather, we suggest that the overall field perturbations are associated with a rotating partial ring current and its field-aligned closure currents, the latter favoring the southern ionosphere during the southern summer conditions examined. A physical picture is presented that links together observed planetary-period modulations in the middle and outer magnetospheric field, plasma, and radio emissions that may be subject to further test and makes predictions as to how these phenomena will evolve during future Saturn equinox and northern summer conditions.
机译:我们检查了卡西尼号航天器在2006年10月至2007年5月期间在土星磁层上的一系列高纬度轨道上获得的磁场数据,以确定是否在极地开放磁场线上出现了行星周期振荡,例如先前在附近发现的-赤道磁场数据。人们发现这种振荡通常以〜0.5-1 nT的幅度出现,比准偶极赤道区域的典型nT幅度要小一些。确定了北极和南部极地地区的极化特征,发现它们与赤道地区的极化特征有显着差异。北半球和南半球的振荡相位也是相对于赤道振荡确定的,因此也是相对于彼此确定的,需要将赤道振荡相位模型扩展到2007年底,跨越高纬度轨道的间隔。结果表明,场振荡的总体模式与在外部区域模拟旋转横向偶极子的旋转外部电流系统不一致。相反,我们建议总的场扰动与旋转的部分环流及其场对准的闭合电流有关,后者在研究的夏季南部条件下有利于南部电离层。呈现了一张物理图片,将中外磁层磁场,等离子体和无线电发射中观测到的行星周期调制联系在一起,这些调制可能需要进一步测试,并预测这些现象在未来土星春分和北部夏季将如何演变条件。

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