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Stream Interactions and Interplanetary Coronal Mass Ejections at 5.3 AU near the Solar Ecliptic Plane

机译:在黄道面附近5.3 AU的流相互作用和行星际冠状物质抛射

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摘要

We have performed a survey of the characteristics of two types of large spatial-scale solar-wind structures, stream interaction regions (SIRs), and interplanetary coronal mass ejections (ICMEs), near 5.3 AU, using solar-wind observations from Ulysses. Our study is confined to the three aphelion passes of Ulysses, and also within ± 10° of the solar ecliptic plane, covering a part of 1992, 1997 – 1998, and 2003 – 2005, representing three slices of different phases of the solar activity cycle. Overall, there are 54 SIRs and 60 ICMEs in the survey. Many are merged in hybrid events, suggesting that they have undergone multiple interactions prior to reaching Jovian orbit. About 91% of SIRs occur with shocks, with 47% of such shocks being forward – reverse shock pairs. The solar-wind velocity sometimes stays constant or even decreases within the interaction region near 5.3 AU, in contrast with the gradual velocity increase during SIRs at 1 AU. Shocks are driven by 58% of ICMEs, with 94% of them being forward shocks. Some ICMEs seem to have multiple small flux ropes with different scales and properties. We quantitatively compare various properties of SIRs and ICMEs at 5.3 AU, and study their statistical distributions and variations with solar activity. The width, maximum dynamic pressure, and peak perpendicular pressure of SIRs all become larger than ICMEs. Dynamic pressure (P dyn) is expected to be important for Jovian magnetospheric activity. We have examined the distributions of P dyn of SIRs, ICMEs, and general solar wind, but these cannot explain the observed bimodal distribution of the location of the Jovian magnetopause. By comparing the properties of SIRs and ICMEs at 0.72, 1, and 5.3 AU, we find that the ICME expansion slows down significantly between 1 and 5.3 AU. Some transient and small streams in the inner heliosphere have merged into a single interaction region.
机译:我们使用尤利西斯(Ulysses)的太阳风观测资料对5.3 AU附近的两种大型空间尺度太阳风结构,流相互作用区域(SIR)和行星际冠状物质抛射(ICME)的特征进行了调查。我们的研究仅限于尤里西斯的三个顶峰,也位于太阳黄道平面的±10°范围内,涵盖了1992、1997 – 1998和2003 – 2005的一部分,代表了太阳活动周期不同阶段的三片。总体而言,调查中有54个SIR和60个ICME。许多被合并为混合事件,表明它们在到达木星轨道之前已经经历了多次相互作用。大约91%的SIR发生在电击中,其中47%是正向-反向电击对​​。在1 AU的SIR期间,太阳风的速度有时会在5.3 AU附近的相互作用区域内保持恒定甚至降低。 58%的ICME推动了冲击,其中94%为正向冲击。一些ICME似乎有多条不同尺度和性质的小通量绳。我们定量比较了5.3 AU下SIR和ICME的各种特性,并研究了它们的统计分布和随太阳活动的变化。 SIR的宽度,最大动压和峰值垂直压力都大于ICME。预计动压(P dyn )对木星的磁层活动很重要。我们已经检查了SIR,ICME和一般太阳风的P dyn 的分布,但是这些不能解释观察到的木卫五的位置的双峰分布。通过比较SIR和ICME在0.72、1和5.3 AU处的特性,我们发现ICME膨胀在1和5.3 AU之间显着减慢。内部日球层中的一些瞬态和小流已合并为一个相互作用区域。

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