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首页> 外文期刊>Space Science Reviews >Corotating Interaction Regions at High Latitudes
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Corotating Interaction Regions at High Latitudes

机译:高纬度的同向交互区域

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摘要

Ulysses observed a stable strong CIR from early 1992 through 1994 during its first journey into the southern hemisphere. After the rapid latitude scan in early 1995, Ulysses observed a weaker CIR from early 1996 to mid-1997 in the northern hemisphere as it traveled back to the ecliptic at the orbit of Jupiter. These two CIRs are the observation basis of the investigation into the latitudinal structure of CIRs. The first CIR was caused by an extension of the northern coronal hole into the southern hemisphere during declining solar activity, whereas the second CIR near solar minimum activity was caused by small warps in the streamer belt. The latitudinal structure is described through the presentation of three 26-day periods during the southern CIR. The first at approx 24 deg S shows the full plasma interaction region including fast and slow wind streams, the compressed shocked flows with embedded stream interface and heliospheric current sheet (HCS), and the forward and reverse shocks with associated accelerated ions and electrons. The second at 40 deg S exhibits only the reverse shock, accelerated particles, and the 26-day modulation of cosmic rays. The possible mechanisms for the access of the accelerated particles and the CIR-modulated cosmic rays to high latitudes above the plasma interaction region are presented. They include direct magnetic field connection across latitude due to stochastic field line weaving or to systematic weaving caused by solar differential rotation combined with non-radial expansion of the fast wind. Another possible mechanism is particle diffusion across the average magnetic field, which includes stochastic field line weaving. A constraint on connection to a distant portion of the CIR is energy loss in the solar wind, which is substantial for the relatively slow-moving accelerated ions. Finally, the weaker northern CIR is compared with the southern CIR. It is weak because the inclination of the streamer belt and HCS decreased as Ulysses traveled to lower latitudes so that the spacecraft remained at about the maximum latitudinal extent of the HCS.
机译:从1992年初到1994年,尤利西斯(Ulysses)在首次进入南半球期间观察到了稳定的CIR。在1995年初进行了快速的纬度扫描后,尤利西斯在1996年初至1997年中旬观测到北半球的CIR减弱,因为它返回了木星轨道的黄道。这两个CIR是研究CIR纬度结构的观察基础。第一个CIR是由于太阳活动下降期间北冠​​状孔向南半球的延伸而引起的,而第二个CIR接近太阳最小活动是由拖缆带中的小翘曲引起的。通过在南部CIR期间的三个26天周期的描述来描述纬度结构。第一个大约在24度S处显示了完整的等离子体相互作用区域,包括快速和缓慢的风流,带有嵌入式流界面和日球层电流薄层(HCS)的压缩激波流以及带有相关的加速离子和电子的正激和反向激波。在40度S处的第二个仅显示出反向冲击,加速的粒子以及对宇宙射线的26天调制。提出了加速粒子和CIR调制宇宙射线进入等离子相互作用区域上方高纬度的可能机制。其中包括由于随机磁场线编织或由于太阳差速旋转以及快速风的非径向膨胀所引起的系统编织而在整个纬度上形成的直接磁场连接。另一个可能的机制是粒子在平均磁场中的扩散,这包括随机场线编织。连接到CIR较远部分的限制是太阳风中的能量损失,这对于运动相对较慢的加速离子而言是相当大的。最后,将较弱的北部CIR与南部CIR进行比较。它之所以微弱,是因为尤利西斯(Ulysses)向更低的纬度移动时,拖缆带和HCS的倾斜度降低了,因此航天器保持在HCS的最大纬度范围内。

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