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Cusp observation at Saturn's high-latitude magnetosphere by the Cassini spacecraft

机译:卡西尼号太空船对土星高纬度磁层的尖锐观测

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摘要

We report on the first analysis of magnetospheric cusp observations at Saturn by multiple in situ instruments onboard the Cassini spacecraft. Using this we infer the process of reconnection was occurring at Saturn's magnetopause. This agrees with remote observations that showed the associated auroral signatures of reconnection. Cassini crossed the northern cusp around noon local time along a poleward trajectory. The spacecraft observed ion energy-latitude dispersions-a characteristic signature of the terrestrial cusp. This ion dispersion is "stepped," which shows that the reconnection is pulsed. The ion energy-pitch angle dispersions suggest that the field-aligned distance from the cusp to the reconnection site varies between ~27 and 51 R_S. An intensification of lower frequencies of the Saturn kilometric radiation emissions suggests the prior arrival of a solar wind shock front, compressing the magnetosphere and providing more favorable conditions for magnetopause reconnection.
机译:我们报告了卡西尼号飞船上多个原位仪器在土星对磁层尖端观测的首次分析。使用此方法,我们推断重新连接的过程发生在土星的磁层顶。这与远程观测一致,后者显示了重新连接的相关极光特征。卡西尼号在当地时间中午前后沿着极点轨迹越过了北部尖峰。航天器观测到了离子能量-纬度色散-地面尖端的特征信号。该离子分散是“阶梯式”的,这表明重新连接是脉冲式的。离子能量-节距角的色散表明,从尖端到再连接部位的场对准距离在〜27和51 R_S之间变化。土星公里辐射发射频率的降低表明太阳风冲击锋面先到,压缩了磁层,为磁层顶重新连接提供了更有利的条件。

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