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Self-Consistent Evolution Models for Slow CMEs up to 1 AU

机译:用于慢速CMES的自我一致的演化模型高达1 AU

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Our 2.5D (axi-symmetric) self-consistent numerical magneto-hydrodynamics (MHD) models for the onset of CMEs under solar minimum conditions and for their interaction with coronal streamers and subsequent evolution up to 1 AU, are presented and discussed. The CMEs are initiated by magnetic flux emergence/cancellation and/or by shearing the magnetic foot points of a magnetic arcade which is positioned above or below the equatorial plane and embedded in a larger helmet streamer. The overlying magnetic streamer field then deflects the CMEs towards the equator, and the deflection path is dependent on the driving velocity. The core of the CME, created during the onset process, contains a magnetic flux rope and the synthetic white light images often show the typical three-part CME structure. The resulting CMEs propagate only slightly faster than the background solar wind, but this small excess speed is high enough to create a fast MHD shock wave from a distance of 0.25 AU onwards. At 1 AU, the plasma shows the typical characteristics of a magnetic cloud, and the simulated data are in good agreement with the (ACE) observations.
机译:我们的2.5D(AXI-COMMETRIC)自我一致的数值磁力 - 流体动力学(MHD)用于太阳能最小条件下的CMES发作的模型,并讨论了与冠状飘带的相互作用以及高达1 AU的随后的进化,并讨论。通过磁通量出现/取消启动CME和/或通过将位于赤道平面上方或下方的磁拱形的磁脚点剪切并嵌入较大的头盔拖车。然后覆盖的磁拖场偏转向赤道的CME偏转,并且偏转路径取决于驱动速度。在起始过程中产生的CME的核心包含磁通磁绳和合成白光图像通常显示典型的三部分CME结构。得到的CME仅比背景太阳能略微快速地传播,但这种小的超速速度足够高,以从0.25 Au向后从0.25 Au开始产生快速MHD冲击波。在1 AU处,等离子体显示磁云的典型特性,并且模拟数据与(ACE)观察结果良好。

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