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A north-south difference in the rotation rate of auroral hiss at Saturn: Comparison to Saturn's kilometric radio emission

机译:土星极光嘶嘶自转速率的南北差异:与土星公里无线电发射的比较

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Broadband whistler-mode emissions, commonly observed by the Cassini spacecraft at high latitudes in Saturn's magnetosphere at frequencies below about 100 Hz, have characteristics very similar to auroral hiss observed at high latitudes in Earth's magnetosphere. In contrast to terrestrial auroral hiss, which shows no obvious rotational modulation, Saturnian auroral hiss shows a very pronounced rotational modulation. We show that the rotation period of the auroral hiss is different in the northern and southem hemispheres, with a period of about 10.6 hours in the northern hemisphere and about 10.8 hours in the southem hemisphere. To within experimentalerror the rotation periods in the two hemispheres match the rotation periods of Satum Kilometric Radiation, an intense radio emission generated along the auroral field lines at frequencies from about 20 to 500 kHz. These north-south asymmetries have potentially important implications on how angular momentum is transferred from the planet to the magnetospheric plasma.
机译:卡西尼号航天器通常在土星磁层的高纬度以低于100 Hz的频率观察到宽带吹口哨模式发射,其特性与地球磁层高纬度的极光嘶嘶声非常相似。与地面极光嘶嘶声没有明显的旋转调制相反,土星极光嘶嘶声显示了非常明显的旋转调制。我们显示,极光嘶嘶声的旋转周期在北半球和南半球是不同的,在北半球大约为10.6小时,在南半球大约为10.8小时。为了在实验误差范围内,两个半球的旋转周期与Satum公里辐射的旋转周期相匹配,后者是沿极光场线以大约20至500 kHz的频率产生的强烈无线电发射。这些南北不对称对角动量如何从行星传递到磁层等离子体具有潜在的重要意义。

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