geomagnetic dipole
美 [ˌdʒioʊmægˈnɛtɪk ˈdaɪpoʊl]英 [ˌdʒi(ː)əʊmægˈnɛtɪk(əl) ˈdaɪpəʊl]
- 地磁偶极子
geomagnetic dipole
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Secular variation of the geomagnetic dipole over the past 2000 years
过去2000年以来地磁偶极子的长期变化
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The geomagnetic dipole field in the 20th century
二十世纪的地球偶极子磁场
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The results indicate that the geomagnetic dipole moment is not always kept decreasing over the past 2000 years , but increasing during nearly 400 years .
结果表明:过去2000年中,地磁场的偶极子磁矩并非一直减小,有近400年的时间是持续增长的。
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With geomagnetic field model records , several kinds of secular variation of geomagnetic dipole moment and the position of the geomagnetic north pole during the year 0 ~ 2000 A. D are calculated and analyzed .
利用地磁场模型资料,计算和分析了公元0~2000年的地磁场偶极子磁矩和地磁北极位置的长期变化。