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An Update on the Centered and Eccentric Geomagnetic Dipoles and Their Poles for the Years 1980?¢????2015

机译:1980年的中心偏心地磁偶极子及其极点的更新

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This paper is an update and extension of an earlier study of the centered and eccentric dipole models of the Earth's magnetic field. We use the 1980?¢????2015 IGRF Gauss coefficients to recalculate the magnetic dipole moments and pole positions for both the centered and eccentric dipoles for an additional 35????years. The changes that have taken place are mostly extensions of the trends described earlier. Interestingly, the earlier weak suggestion of an accelerated decline in the magnetic moment over the interval 1975?¢????1985 persists in the more recent data; if the current decline for the years 2000?¢????2015 continues, the Earth's field is projected to decline to nothing around the year 3797????A.D. This projected decline to zero field will almost certainly not occur on this date, but it is of interest because the timescale for the decline is remarkably short compared with the timescales derived for past field reversals. The asymmetry of the Earth's field continues to increase quite rapidly, with the offset of the equivalent dipole from the Earth's center now close to 9% of the Earth's radius. Since we now know that all the planets in our solar system with global magnetic fields have asymmetric fields that can be modeled more accurately as eccentric dipole fields, and not as centered dipole fields, the eccentric dipole analysis reported here can now be viewed more generally as an approach to planetary magnetic fields and not just to the magnetic field of our own planet.
机译:本文是对地球磁场的中心和偏心偶极子模型的早期研究的更新和扩展。我们使用1980年到2015年的IGRF高斯系数来重新计算中心和偏心偶极子的磁偶极矩和磁极位置,历时35年。已经发生的变化主要是前面所述趋势的扩展。有趣的是,较早的关于在1975年至1985年间磁矩加速下降的较弱建议仍然存在于最新数据中。如果目前的2000年下降趋势持续到2015年,则预计到3797年左右地球磁场将下降至零。预计下降到零磁场的这一天几乎肯定不会在此日期发生,但它是令人感兴趣的,因为与过去的磁场反转得出的时间尺度相比,下降的时间尺度非常短。地球场的不对称性继续以相当快的速度增加,等效偶极子相对于地球中心的偏移现在接近地球半径的9%。由于我们现在知道太阳系中所有具有全局磁场的行星都具有非对称场,可以将其更精确地建模为偏心偶极场,而不是中心偶极场,因此这里报告的偏心偶极子分析现在可以更一般地视为一种解决行星磁场而不只是解决我们自己星球磁场的方法。

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