论文标题
在太阳能周期23和24期间快速冠状质量弹出的聚类以及对CME-CME相互作用的影响
Clustering of fast Coronal Mass Ejections during the solar cycles 23 and 24 and implications for CME-CME interactions
论文作者
论文摘要
我们研究了在太阳能周期23和24期间发生的快速冠状质量弹出(CME)的聚类特性。我们采用两种方法:最大频谱方法可以检测主要的群集,并提供了簇阈值阈值时间方法,提供了有关典型集群特性和时间尺度的详细信息。我们的分析表明,在太阳能循环23和24的不同阶段中,具有速度$ \ geq 1000 \ km/s $的CME优先以孤立的事件和平均两个成员的群集。但是,具有更多成员的簇尤其是在太阳周期的最大阶段中出现的。在整个期间,在太阳能周期23和24的最大阶段中,约有50%是孤立的事件,有18%(12%)出现在具有2(3)构件的群集中,而在较大的群集中又有20%的$ \ geq 4 $,而在太阳能中,最小的快速CME往往会更频繁地作为孤立的事件发生(62%)。在不同的太阳周期阶段,无论在太阳能最小值和最大值期间,CME的出现频率截然不同。这些发现表明,极端事件的$τ_c$可能反映出大型耀斑和CME积极活性ARS的特征能量积累时间。从统计学上讲,快速CME的聚类特性与地球的干扰风暴指数DST表明,簇中发生的快速CME往往会产生比孤立的快速CME的更大的地磁风暴。这可能与CME-CME相互作用有关,从而与地球磁层产生更复杂和更强的相互作用。
We study the clustering properties of fast Coronal Mass Ejections (CMEs) that occurred during solar cycles 23 and 24. We apply two methods: the Max spectrum method can detect the predominant clusters and the de-clustering threshold time method provides details on the typical clustering properties and time scales. Our analysis shows that during the different phases of solar cycles 23 and 24, CMEs with speed $\geq 1000\ km/s$ preferentially occur as isolated events and in clusters with on average two members. However, clusters with more members appear particularly during the maximum phases of the solar cycles. Over the total period and in the maximum phases of solar cycles 23 and 24, about 50% are isolated events, 18% (12%) occur in clusters with 2 (3) members, and another 20% in larger clusters $\geq 4$, whereas in solar minimum fast CMEs tend to occur more frequently as isolated events (62%). During different solar cycle phases, the typical de-clustering time scales of fast CMEs are $τ_c=28-32\ hrs$, irrespective of the very different occurrence frequencies of CMEs during solar minimum and maximum. These findings suggest that $τ_c$ for extreme events may reflect the characteristic energy build-up time for large flare and CME-prolific active ARs. Associating statistically the clustering properties of fast CMEs with the Disturbance storm index Dst at Earth suggests that fast CMEs occuring in clusters tend to produce larger geomagnetic storms than isolated fast CMEs. This may be related to CME-CME interaction producing a more complex and stronger interaction with the Earth magnetosphere.