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An update of Leighton’s solar dynamo model

机译:Leighton的太阳能发电机模型的更新

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摘要

In 1969, Leighton developed a quasi-1D mathematical model of the solar dynamo, building upon the phenomenological scenario of Babcock published in 1961. Here we present a modification and extension of Leighton’s model. Using the axisymmetric component (longitudinal average) of the magnetic field, we consider the radial field component at the solar surface and the radially integrated toroidal magnetic flux in the convection zone, both as functions of latitude. No assumptions are made with regard to the radial location of the toroidal flux. The model includes the effects of (i) turbulent diffusion at the surface and in the convection zone; (ii) poleward meridional flow at the surface and an equatorward return flow affecting the toroidal flux; (iii) latitudinal differential rotation and the near-surface layer of radial rotational shear; (iv) downward convective pumping of magnetic flux in the shear layer; and (v) flux emergence in the form of tilted bipolar magnetic regions treated as a source term for the radial surface field. While the parameters relevant for the transport of the surface field are taken from observations, the model condenses the unknown properties of magnetic field and flow in the convection zone into a few free parameters (turbulent diffusivity, effective return flow, amplitude of the source term, and a parameter describing the effective radial shear). Comparison with the results of 2D flux transport dynamo codes shows that the model captures the essential features of these simulations. We make use of the computational efficiency of the model to carry out an extended parameter study. We cover an extended domain of the 4D parameter space and identify the parameter ranges that provide solar-like solutions. Dipole parity is always preferred and solutions with periods around 22 yr and a correct phase difference between flux emergence in low latitudes and the strength of the polar fields are found for a return flow speed around 2 m?s ~(-1) , turbulent diffusivity below about 80 km ~(2) s ~(-1) , and dynamo excitation not too far above the threshold (linear growth rate less than 0.1 yr ~(-1) ).
机译:1969年,Leighton于1961年发布的Babcock现象学情景,开发了一个太阳能发电机的拟1D数学模型。在这里,我们提出了Leighton模型的修改和延伸。使用磁场的轴对称分量(纵向平均值),我们考虑太阳面的径向场分量和对流区域中的径向集成环形磁通量,无论是纬度的函数。关于环形通量的径向位置没有假设。该模型包括(i)表面和对流区的湍流扩散的影响; (ii)地表的极向子午线流动和影响环形通量的赤道返回流程; (iii)纬度差动旋转和径向旋转剪切的近表面层; (iv)向下对流泵送剪切层中的磁通量; (v)倾斜双极区域形式的通量出现作为径向表面场的源术语。虽然从观察中取出了对表面场传输的参数,但模型将磁场的未知特性和对流区域流入几种自由参数(湍流扩散,有效返回流程,源术语的幅度,和描述有效径向剪切的参数。与2D磁通传输发电机码结果的比较表明,该模型捕获了这些模拟的基本特征。我们利用模型的计算效率来执行扩展参数研究。我们介绍了4D参数空间的扩展域,并识别提供太阳能溶液的参数范围。偶极奇偶校验总是优选的,并且在低纬度的低纬度和低纬度的磁共振出现之间的溶液和极差异的正确相位差和极性场的强度差异为返回流量速度,湍流速度约为2mΩ·(-1),湍流扩散率低于约80 km〜(2)s〜(-1),电动刺激远远超过阈值(线性生长率小于0.1yr〜(-1))。

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