Solar Activity and Variation of Geomagnetic Disturbance
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摘要: 以每年中地磁指数C9≥L事件的次数表示地磁扰动程度.研究下列六种情况:L=3、4和5,其中每一种又再分成重现的和一般的两类.用曲线分段拟合法求出地磁扰动年次数Ck与黑子相对数Rk之间的经验的平均关系f(R);计算出△k=Ck-fk,其中fk≡f(Rk).计算结果表明:1.用黑子相对数极小年之前四年作太阳活动周的起算点.对这种“活动周”求△k=Ck-fk的平均,得到各个△.各“活动周”的△的符号依次正负交替.2.由90年地磁扰动观测资料得来的符号交替规律出现在C9≥3、4和5时的各种情况.这很可能是由于太阳极区磁场符号依次交替变化造成的.进一步地划分时段后,各个“活动周”中△k对于△的弥散程度σ不同.σ序列显现出约70年的长周期.Abstract: The events of which geomagnetic indices C9s are all larger than L (L is a constant) are noticed. The number of times of the events in a year is taken to express the level of geomagnetic disturbance of the year. Six cases are studied:L=3, 4 and 5; each of them is subdivided into two subcases: recurrent events and general events.The method of the curve fitting with piecewise polynomials is used to derive an averaged experimental relationship f(R) between the number of times in a year Ck and the sunspot relative number Rk (k is the order of the years from 1980 to 1979). Then, △k = Ck - fk (fk = f(Rk)) are calculated. The result shows that: 1, for the 'solar cycles', each of which begins at he year four years before the minimum of the cor responding solar cycle, the signs of the average values of △k alternate, ('sign alternating' fule +,-,+,-,......); 2. the 'sign alternating' rule oceurs in all the six subcases. It is mostly likely that the rule is caused by thereversal of the solar polar fields. After a further dividing of the 'cycles', every cycle has own dispersity (o) about its averaged △, △. The sequence of a shows a long term period of about 70 years.
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