首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Interplanetary magnetic field during the past 9300 yearsinferred from cosmogenic radionuclides
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Interplanetary magnetic field during the past 9300 yearsinferred from cosmogenic radionuclides

机译:行星际磁场在过去的9300年yearsinferred从宇宙发生的放射性核素

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[1] We have reconstructed the interplanetary magnetic field (IMF), its radial component,and the open solar magnetic flux using the solar modulation potential derived fromcosmogenic ~(10)Be radionuclide data for a period covering the past 9300 years.Reconstructions using the assumption of both constant and variable solar wind speedsyielded closely similar results. During the Maunder Minimum, the strength of the IMF wasapproximately 2 nT compared to a mean value of 6.6 nT for the past 40 years,corresponding to an increase of the open solar magnetic flux of about 350%. We examinefour cycles of the Hallstatt periodicity in the IMF with a mean period of —2250 yearsand an amplitude of0.75 nT. Grand solar minima have largely occurred in clustersduring the Hallstatt cycle minima around the years —5300, —3400, —1100, and +1500 A.D.The last cluster includes the Dalton, Maunder, and Sporer minima. We predict that thenext such cluster will occur in about 1500 years. The long-term IMF has variedbetweennT and —8 nT and does not confirm a proposed floor (lower limit). There is aslowly changing long-term trend of amplitude 1.5 nT, with a minimum around the year—4600 and a maximum around 0 A.D. that may be of solar origin but which also may bedue to unknown long-term changes in the atmospheric effects or geomagnetic fieldintensity.
机译:[1]我们已经重建了星际磁场(IMF),其径向分量,开放使用太阳能太阳能磁通量调制潜在派生fromcosmogenic~(10)被放射性核素数据在一段时间内覆盖过去的9300年。假设太阳常数和变量风speedsyielded密切相似的结果。在蒙德极小期的强度国际货币基金组织(IMF) 2种nT相比的意思值6.6元在过去40年,相应的增加了太阳磁通的约350%。国际货币基金组织的哈尔斯塔特周期性的周期平均-2250 yearsand振幅of0.75 nT。大太阳能最小值在很大程度上发生在clustersduring初期铁器时代的周期最小值在-5300年,-3400年,-1100年,+ 1500不知道去年集群包括道尔顿,胡扯,斯波勒最小值。还是这样的集群将发生在约1500年。8元,不确认提议的地板上(下限)。长期趋势的振幅1.5元,最低的一年- 4600和最大0公元太阳能起源的可能但也bedue未知的长期变化吗大气效应或地磁fieldintensity。

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