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首页> 外文期刊>The Astrophysical journal >LATITUDE DISTRIBUTION OF POLAR MAGNETIC FLUX IN THE CHROMOSPHERE NEAR SOLAR MINIMUM
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LATITUDE DISTRIBUTION OF POLAR MAGNETIC FLUX IN THE CHROMOSPHERE NEAR SOLAR MINIMUM

机译:接近最小最小值的染色体上极性磁通量的纬度分布

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The distribution of magnetic flux elements as a function of latitude in the polar solar caps at a time close to solar cycle minimum is explored. High-sensitivity line-of-sight magnetograms acquired by the Synoptic Optical Long-term Investigations of the Sun (SOLIS) vector spectromagnetograph (VSM) in the chromospheric line Ca n 854.2 nm are utilized. The area density distribution of the magnetic flux averaged over months is found to decrease close to the solar poles. This trend is more pronounced when considering only flux elements with relatively large size (larger than ≈5″ × 5″). The flux density of the latter is relatively flat from the edge of the polar cap up to latitudes of 75°-80° and decreases by more than 50% up to the solar pole. The density of smaller flux features is more uniformly distributed. Although the density decrease is still present, it is less pronounced. Hence, we believe there are two populations of flux elements in the polar caps. The small flux elements are probably produced uniformly across the polar area, in contrast to the large flux elements that are the product of magnetic fields of decaying active regions. The latter are concentrated by solar convection and carried up to high latitudes by differential rotation and meridional circulation. This result is important in studying meridional flows that transport the magnetic flux from lower to higher solar latitudes resulting, in particular, to the solar-cycle-related polar reversal. It is also of importance in studying polar structures contributing to the fast solar wind, such as polar plumes.
机译:在接近太阳周期最小值的时间,探索了磁通量元素在极地太阳帽中作为纬度的函数的分布。利用了在色球层Ca n 854.2 nm处通过太阳的天气光学长期研究(SOLIS)矢量分磁仪(VSM)获得的高灵敏度视线磁图。发现在数月内平均的磁通量的密度分布在靠近太阳极的地方减小。仅考虑较大尺寸(大于≈5“×5”)的通量元素时,这种趋势更为明显。从极帽的边缘到纬度为75°-80°,后者的通量密度相对平坦,到太阳极为止,其通量密度下降50%以上。较小的磁通量特征的密度分布更均匀。尽管密度降低仍然存在,但程度不明显。因此,我们认为极性帽中有两个磁通元素。与由衰减有源区的磁场产生的大通量元素相反,小通量元素可能在整个极性区域均匀产生。后者通过太阳对流而集中,并通过差速旋转和子午环流上升到高纬度。该结果对于研究子午流非常重要,子午流将磁通量从较低的纬度传递到较高的太阳纬度,尤其是导致了与太阳周期有关的极地反转。在研究有助于快速太阳风的极地结构(例如极地羽流)方面也很重要。

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