On the self-consistent algorithm for numerical simulation of the global geomagnetic disturbances and associated electric current spreading to low latitudes

L. Alperorich, B. Fidel
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Abstract

We present a finite elements algorithm (FEA) for study of the global current systems produced by extra low frequency electromagnetic disturbances like hydromagnetic waves, solar-quite daily variations, and so on. All these problems can be reduced to Laplace's equation on a thin nonhomogeneous anisotropic shell. Our approach is based on satisfying this law within each elementary cell of the numerical grid. The main strength of the proposed algorithm is in the widely used finite difference method (FDM). It was found that the FDM accumulates numerical errors caused by numerical 'diffusion'. This artificial diffusion is a sequence of the finite difference representation of the differential operators of the original Laplace equation in a nonhomogeneous case.
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全球地磁扰动及相关低纬度电流扩散数值模拟的自洽算法
我们提出了一种有限元算法(FEA),用于研究由特低频电磁干扰(如水电磁波、太阳日变化等)产生的全球电流系统。所有这些问题都可以归结为非均匀各向异性薄壳上的拉普拉斯方程。我们的方法是基于在数值网格的每个基本单元内满足这一定律。该算法的主要优点在于广泛使用的有限差分法(FDM)。结果表明,FDM会累积由数值“扩散”引起的数值误差。这种人工扩散是原始拉普拉斯方程的微分算子在非齐次情况下的有限差分表示的序列。
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