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源自活动区11158的日冕物质抛射的偏折与旋转

Deflection and Rotation of CMEs from Active Region 11158.

作者信息

Kay Christina, Gopalswamy Nat, Xie Hong, Yashiro Seiji

机构信息

Solar Physics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA.

Department of Physics, The Catholic University of America, Washington, DC, USA.

出版信息

Sol Phys. 2017;292(6). doi: 10.1007/s11207-017-1098-z. Epub 2017 Jun 7.

Abstract

Between 13 and 16 February 2011, a series of coronal mass ejections (CMEs) erupted from multiple polarity inversion lines within active region 11158. For seven of these CMEs we employ the graduated cylindrical shell (GCS) flux rope model to determine the CME trajectory using both (STEREO) extreme ultraviolet (EUV) and coronagraph images. We then use the model called Forecasting a CME's Altered Trajectory (ForeCAT) for nonradial CME dynamics driven by magnetic forces to simulate the deflection and rotation of the seven CMEs. We find good agreement between ForeCAT results and reconstructed CME positions and orientations. The CME deflections range in magnitude between 10° and 30°. All CMEs are deflected to the north, but we find variations in the direction of the longitudinal deflection. The rotations range between 5° and 50° with both clockwise and counterclockwise rotations. Three of the CMEs begin with initial positions within 2° from one another. These three CMEs are all deflected primarily northward, with some minor eastward deflection, and rotate counterclockwise. Their final positions and orientations, however, differ by 20° and 30°, respectively. This variation in deflection and rotation results from differences in the CME expansion and radial propagation close to the Sun, as well as from the CME mass. Ultimately, only one of these seven CMEs yielded discernible signatures near Earth, although the active region faced toward Earth throughout the eruptions. We suggest that the differences in the deflection and rotation of the CMEs can explain whether each CME impacted or missed Earth.

摘要

2011年2月13日至16日期间,一系列日冕物质抛射(CME)从活动区11158内的多个极性反转线喷发出来。对于其中7次CME,我们采用渐变圆柱壳(GCS)通量绳模型,利用太阳日球层天文台(STEREO)的极紫外(EUV)和日冕仪图像来确定CME轨迹。然后,我们使用名为“预测CME改变后的轨迹”(ForeCAT)的模型,来模拟由磁力驱动的非径向CME动力学,以模拟这7次CME的偏转和旋转。我们发现ForeCAT结果与重建的CME位置和方向之间有很好的一致性。CME的偏转幅度在10°至30°之间。所有CME都向北偏转,但我们发现纵向偏转方向存在变化。旋转角度在5°至50°之间,既有顺时针旋转也有逆时针旋转。其中3次CME开始时彼此之间的初始位置在2°以内。这3次CME主要都向北偏转,有一些轻微的向东偏转,并逆时针旋转。然而,它们的最终位置和方向分别相差20°和30°。这种偏转和旋转的变化是由CME在靠近太阳处的膨胀和径向传播差异以及CME质量差异导致的。最终,尽管在整个喷发过程中活动区都朝向地球,但这7次CME中只有一次在地球附近产生了可辨别的特征。我们认为,CME偏转和旋转的差异可以解释每次CME是否撞击或错过地球。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7d73/7398417/5d28577b6ce6/nihms-938439-f0001.jpg

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