论文标题

较低太阳大气中的双极性扩散:黑子的MHD模拟

Ambipolar Diffusion in the Lower Solar Atmosphere: MHD Simulations of a Sunspot

论文作者

MacBride, Conor D., Jess, David B., Khomenko, Elena, Grant, Samuel D. T.

论文摘要

在血浆完全离子化的假设下,通常进行太阳气氛的磁水动力学(MHD)模拟。但是,在较低的太阳大气中,温度降低通常仅导致血浆的部分电离。这种部分电离等离子体的中性和离子化成分之间的相互作用会产生双极扩散。为了研究双极扩散在光球和色球层传播波特征中的作用,我们采用Mancha3D数值代码来模拟磁声波,这些磁声波在太阳斑点上方的蒙布上方的大气中传播。我们通过改变模拟来研究模拟,以在计算该过程的MHD方程中包括其他项,从而研究了数据驱动的磁平衡的非理想MHD方程。分析具有/没有双相扩散的模拟的能量光谱密度,我们发现证据表明,在弱离子化的低密度区域中,双极性扩散在波特征中起关键作用,因此最大化了局部歧义性歧义性扩散系数。结果,我们建议双极扩散是一种重要的机制,需要仔细考虑是否应包括在模拟中,以及是否应将其用于分析和解释较低太阳大气的特定观察结果。

Magnetohydrodynamic (MHD) simulations of the solar atmosphere are often performed under the assumption that the plasma is fully ionized. However, in the lower solar atmosphere a reduced temperature often results in only the partial ionization of the plasma. The interaction between the decoupled neutral and ionized components of such a partially ionized plasma produces ambipolar diffusion. To investigate the role of ambipolar diffusion in propagating wave characteristics in the photosphere and chromosphere, we employ the Mancha3D numerical code to model magnetoacoustic waves propagating through the atmosphere immediately above the umbra of a sunspot. We solve the non-ideal MHD equations for data-driven perturbations to the magnetostatic equilibrium and the effect of ambipolar diffusion is investigated by varying the simulation to include additional terms in the MHD equations that account for this process. Analyzing the energy spectral densities for simulations with/without ambipolar diffusion, we find evidence to suggest that ambipolar diffusion plays a pivotal role in wave characteristics in the weakly ionized low density regions, hence maximizing the local ambipolar diffusion coefficient. As a result, we propose that ambipolar diffusion is an important mechanism that requires careful consideration into whether it should be included in simulations, and whether it should be utilized in the analysis and interpretation of particular observations of the lower solar atmosphere.

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