首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >North-south asymmetry in global distribution of the solar wind speed during 1985–2013
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North-south asymmetry in global distribution of the solar wind speed during 1985–2013

机译:在全球分布南北不对称太阳风速度在1985 - 2013

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Interplanetary scintillation (IPS) observations made between 1985 and 2013 are used to investigate the north-south (N-S) asymmetry in global distribution of the solar wind speed. The IPS observations clearly demonstrate that the global distribution of the solar wind speed systematically changes with the solar activity. This change is found to closely correlate with that in polar magnetic fields of the Sun, while fast wind data at solar minima systematically deviate from this correlation. The IPS observations show that notable N-S asymmetry of polar solar winds occurs at the solar maxima, and small but significant N-S asymmetry exists at the solar minima. The observed asymmetry at the solar maxima is consistent with the time lag in the reversal of polar magnetic fields between north and south hemispheres. We also find that significant N-S asymmetry of the polar fast wind lasts for the period between Cycles 23 and 24 solar maxima, starting from predominance of the fast wind over the north pole and ending with that over the south pole. The N-S asymmetry revealed from IPS observations is found to be generally consistent with Ulysses observations. We compare IPS observations with magnetic field data of the Sun and find that the ratio of the quadrupole to dipole coefficients exhibits a similar time variation to that of the N-S asymmetry revealed from IPS observations. This suggests that higher-order multipole moments play an important role in determining the N-S asymmetry of the solar wind when the dipole moment weakens.
机译:行星际闪烁(IPS)观察在1985年和2013年之间用于调查南北(n)的不对称全球分销的太阳风速度。IPS观察清楚地证明全球分销的太阳风速度系统的变化与太阳活动。发现这种变化密切相关在太阳的磁场极性,快速系统在太阳能风能数据最小值偏离这一相关性。观测表明,显著的计算不对称极地太阳风发生在太阳极大值,小但重要的计算不对称的存在太阳能最小值。最大值的时间间隔是一致的北之间的磁场极性逆转南北半球。重要的计算不对称极快的风持续周期23和24之间的时期太阳能极大值,从优势的快风在北极和结束在南极。显示从IPS的观察发现通常与尤利西斯的观察一致。我们比较IPS观测磁场太阳和发现的数据的比例四极偶极子系数展品类似的时间变化的计算从IPS观察不对称了。表明高阶多极的时刻一个重要的角色在决定计算当偶极子不对称的太阳风削弱了。

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