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Observational Evidence of Shallow Origins for the Magnetic Fields of Solar Cycles

机译:太阳周期磁场的浅层起源的观测证据

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Observational evidence for the origin of active region magnetic fields has been sought from published information on extended solar cycles, statistical distributions of active regions and ephemeral regions, helioseismology results, positional relationships to supergranules, and fine-scale magnetic structure of active regions and their sunspots during their growth. Statistical distributions of areas of ephemeral and active regions blend together to reveal a single power law. The shape of the size distribution in latitude of all active regions is independent of time during the solar cycle, yielding further evidence that active regions of all sizes belong to the same population. Elementary bipoles, identified also by other names, appear to be the building blocks of active regions; sunspots form from elementary bipoles and are therefore deduced to develop from the photosphere downward, consistent with helioseismic detection of downflows to 3-4 Mm below sunspots as well as long-observed downflows from chromospheric/coronal arch filaments into sunspots from their earliest appearance. Time-distance helioseismology has been effective in revealing flows related to sunspots to depths of 20 Mm. Ring diagram analysis shows a statistically significant preference for upflows to precede major active region emergence and downflows after flux emergence but both are often observed together or sometimes not detected. From deep-focus helioseismic techniques for seeking magnetic flux below the photosphere prior major active regions, there is evidence of acoustic travel-time perturbation signatures rising in the limited range of depths of 42-75 Mm but these have not been verified or found at more shallow depths by helioseismic holographic techniques. The development of active regions from clusters of elementary bipoles appears to be the same irrespective of how much flux an active region eventually develops. This property would be consistent with the magnetic fields of large active regions being generated in the same way and close the same depth as small active regions in a shallow zone below the photosphere. All evidence considered together, understanding the origins of the magnetic fields of solar cycles boils down to learning how and where elementary bipoles are generated beneath the photosphere.
机译:从延长的太阳周期,活动区域和短暂区域的统计分布,日震学结果,与超颗粒的位置关系以及活动区域及其黑子的细尺度磁性结构等已发布的信息中寻找了活动区域磁场起源的观测证据。在他们成长的过程中。临时区域和活动区域的统计分布融合在一起,揭示了一个幂函数。在太阳活动周期中,所有活动区域的纬度大小分布形状与时间无关,进一步证明所有大小的活动区域都属于同一种群。基本偶极子,也用其他名称标识,似乎是活跃区域的基础。太阳黑子由基本的偶极子形成,因此推论是从光球向下发展的,这与对低至太阳黑子以下3-4 Mm的向下流以及从色球/冠状弓形细丝从最早出现到太阳黑子的长期观测到的顺流地震检测一致。时空流变学已经有效地揭示了与黑子有关的水流到20 Mm的深度。环形图分析显示,在主要活动区域出现之前先出现上升趋势,在通量出现之后出现下降趋势,这在统计上是很重要的,但通常同时观察或有时未发现两者。从用于寻找光球在主要活动区域之前的磁通量的深聚焦流变技术,可以发现声传播时间扰动特征在42-75 Mm的有限深度范围内上升,但尚未得到验证或发现。通过日射全息技术在较浅的深度进行拍摄。无论有源区域最终产生了多少通量,从基本双极子簇形成的有源区域似乎都是相同的。该性质与在光球以下的浅层区域中以与小有源区相同的方式产生并闭合相同深度的大有源区的磁场一致。综合考虑所有证据,了解太阳周期磁场的起源归结为了解光球下如何以及在何处生成基本双极子。

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