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Towards an algebraic method of solar cycle prediction

机译:朝着太阳循环预测的代数方法

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We discuss the potential use of an algebraic method to compute the value of the solar axial dipole moment at solar minimum, widely considered to be the most reliable precursor of the activity level in the next solar cycle. The method consists of summing up the ultimate contributions of individual active regions to the solar axial dipole moment at the end of the cycle. A potential limitation of the approach is its dependence on the underlying surface flux transport (SFT) model details. We demonstrate by both analytical and numerical methods that the factor relating the initial and ultimate dipole moment contributions of an active region displays a Gaussian dependence on latitude with parameters that only depend on details of the SFT model through the parameter η /Δ_( u )where η is supergranular diffusivity and Δ_( u )is the divergence of the meridional flow on the equator. In a comparison with cycles simulated in the 2 × 2D dynamo model we further demonstrate that the inaccuracies associated with the algebraic method are minor and the method may be able to reproduce the dipole moment values in a large majority of cycles.
机译:我们讨论了代数方法的潜在用途来计算太阳能最小值的太阳轴向偶极力矩的值,被广泛认为是下一个太阳循环中活动水平最可靠的前体。该方法包括将个体有源区的最终贡献总结到循环结束时的太阳轴向偶极力矩。该方法的潜在限制是其对底层表面磁通传输(SFT)模型细节的依赖性。我们通过分析和数值方法证明了有源区域的初始和最终偶极矩贡献的因子和最终偶极矩贡献的因素显示了对纬度的高斯依赖,其中参数通过参数η/Δ_(u)在其中仅取决于SFT模型的细节η是超级扩散性,Δ_(U)是赤道上的子午线流动的分歧。在与2×2D发电机模型中模拟的循环的比较中,我们进一步证明与代数方法相关的不准确性是轻微的,并且该方法可以能够在大多数循环中再现偶极力矩值。

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