日冕随时间变化的动力学特性

E. Mason, R. Lionello, Cooper Downs, Jon A. Linker, R. Caplan, M. DeRosa
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摘要

在这封信中,我们首次对传统的线系稳态磁流体动力学模型和一种新的、完全随时间变化的全球日冕热力学磁流体动力学模拟进行了全球比较。为了近似太阳极小期附近的地表磁场分布和强度,我们使用洛克希德不断演变的地表通量同化模型来获得包含整个太阳旋转期间通量出现和地表流动的输入图,包括微分旋转和经向流动。每个时间步都在新的磁场输入边界条件下演变等离子体的先前状态,模拟太阳上的光球驱动。我们发现,与稳态模型相比,这种方法产生的电晕在质量上有所不同。在时间依赖模型中,磁能水平更高,并且日冕洞比在稳态模型中更多地沿着以下边缘演化。日冕的变化,如前向模拟的排放图所示,在时间依赖的驱动下在更长的时间尺度上演化。我们讨论了活跃和安静太阳场景的影响,太阳风的形成,以及广泛使用的稳态假设,如势场源面计算。
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Time-dependent Dynamics of the Corona
We present in this Letter the first global comparison between traditional line-tied steady-state magnetohydrodynamic models and a new, fully time-dependent thermodynamic magnetohydrodynamic simulation of the global corona. To approximate surface magnetic field distributions and magnitudes around solar minimum, we use the Lockheed Evolving Surface-Flux Assimilation Model to obtain input maps that incorporate flux emergence and surface flows over a full solar rotation, including differential rotation and meridional flows. Each time step evolves the previous state of the plasma with a new magnetic field input boundary condition, mimicking photospheric driving on the Sun. We find that this method produces a qualitatively different corona compared to steady-state models. The magnetic energy levels are higher in the time-dependent model, and coronal holes evolve more along the following edge than they do in steady-state models. Coronal changes, as illustrated with forward-modeled emission maps, evolve on longer timescales with time-dependent driving. We discuss implications for active and quiet Sun scenarios, solar wind formation, and widely used steady-state assumptions like potential field source surface calculations.
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