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首页> 外文期刊>Geophysical Research Letters >Variability in Saturn's bow shock and magnetopause from Pioneer and Voyager: Probabilistic predictions and initial observations by Cassini - art. no. L20S08
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Variability in Saturn's bow shock and magnetopause from Pioneer and Voyager: Probabilistic predictions and initial observations by Cassini - art. no. L20S08

机译:先锋和航海家的土星弓震动和磁更年期的变异性:卡西尼号的概率预测和初步观察-艺术。没有。 L20S08

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摘要

Probability distributions for the location of the Saturnian bow shock and magnetopause have been derived by extrapolating observations of dynamic solar wind pressures to the position of Saturn's orbit. These observations are those made by the Pioneer 11, Voyager 1 and 2 spacecraft near Saturn's orbit and by the Ulysses spacecraft near its aphelion. The magnetopause subsolar distance ( measured from Saturn's center) is obtained using pressure equilibrium. The bow shock standoff distance is determined using empirical relations between bow shock size and solar wind dynamic pressure. Simple 2-D geometric models of the magnetopause and bow shock surfaces have been used to determine their morphologies over a large range in local time. Three cases have been studied: ( 1) An Earth-type magnetosphere with low internal plasma pressure; ( 2) An intermediate case calibrated with Voyager 1 observations; and ( 3) A Jupiter-like inflated magnetosphere. The comparison of these models with initial observations from the initial sunward orbits of the Cassini spacecraft indicates a more inflated magnetosphere than postulated by the previous modelling of the Pioneer-Voyager encounters.
机译:通过将观测到的太阳动态风压推算到土星轨道位置,可以得出土星弓激波和磁更年期位置的概率分布。这些观测结果是由土星轨道附近的先驱者11号,旅行者1号和2号航天器以及靠近其顶峰的尤利西斯号航天器进行的。磁层顶太阳下距离(从土星中心测量)是使用压力平衡获得的。弓形冲击距离是根据弓形冲击大小与太阳风动压力之间的经验关系确定的。磁层顶和弓形冲击面的简单二维几何模型已用于确定当地时间范围内的形态。研究了三种情况:(1)内部等离子体压力低的地球型磁层; (2)用旅行者1观测值校准的中间案例; (3)类似木星的膨胀磁层。这些模型与卡西尼号航天器初始朝阳轨道的初始观测结果的比较表明,磁层膨胀程度比先驱者-旅行者号遭遇的先前模型所假定的要大。

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