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Cusp observation at Saturns 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 RS. 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.Key Points class="unordered" style="list-style-type:disc">We observe evidence for reconnection in the cusp plasma at SaturnWe present evidence that the reconnection process can be pulsed at SaturnSaturn's cusp shows similar characteristics to the terrestrial cusp
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,这是地球尖端的特征。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 RS与51 RS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。要点 class =“ unordered” style =“ list-style- type:disc“> <!-list-behavior =无序前缀-word = mark-type = disc max-label-size = 0-> 我们观察到土星尖尖血浆重新连接的证据 我们提供了证据,表明重新连接过程可以在土星上发生脉冲 土星的尖瓣显示出与陆地尖瓣相似的特征

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