首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Solar winds driven by nonlinear low-frequency Alfvén waves from the photosphere: Parametric study for fast/slow winds and disappearance of solar winds
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Solar winds driven by nonlinear low-frequency Alfvén waves from the photosphere: Parametric study for fast/slow winds and disappearance of solar winds

机译:来自光球的非线性低频Alfvén波驱动的太阳风:关于快/慢风和太阳风消失的参数研究

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We investigate how properties of the corona and solar wind in open coronal holes depend on properties of magnetic fields and their footpoint motions at the surface. We perform one-dimensional magnetohydrodynamical (MHD) simulations for the heating and the acceleration in coronal holes by low-frequency Alfvén waves from the photosphere to 0.3 or 0.1 AU. We impose low-frequency (0.05 Hz) transverse fluctuations of the field lines at the photosphere with various amplitude, spectrum, and polarization in the open flux tubes with different photospheric field strength, B r,0, and superradial expansion of the cross section, f max. We find that transonic solar winds are universal consequences. The atmosphere is also stably heated up to 106 K by the dissipation of the Alfvén waves through compressive-wave generation and wave reflection in the cases of the sufficient wave input with photospheric amplitude, dv ,0 0.7 km s~-1. The density, and accordingly the mass flux, of solar winds show a quite sensitive dependence on dv ,0 because of an unstable aspect of the heating by the nonlinear Alfvén waves. A case with < dv ⊥0> = 0.4 km s~-1 gives 50 times smaller mass flux than the fiducial case for the fast wind with < dv ⊥0 >= 0.7 km s~-1; solar wind virtually disappears only if dv ,0 becomes 1/2. We also find that the solar wind speed has a positive correlation with B r,0/f max, which is consist ent with recent observations by Kojima et al. On the basis of these findings, we show that both fast and slow solar winds can be explained by the single process, the dissipation of the low-frequency Alfvén waves, with different sets of dv ,0 and B r,0/f max. Our simulations naturally explain the observed (1) anticorrelation of the solar wind speed and the coronal temperature and (2) larger amplitude of Alfvénic fluctuations in the fast wind. In Appendix A, we also explain our implementation of the outgoing boundary condition of the MHD waves with some numerical tests.
机译:我们研究日冕孔中日冕和太阳风的性质如何取决于磁场的性质及其在表面的脚点运动。我们执行一维磁流体动力学(MHD)模拟,对从光球到0.3或0.1 AU的低频Alfvén波对日冕孔进行加热和加速。我们在具有不同光球场强,B r,0和横截面的超径向膨胀的开放通量管中,在光球上施加具有各种幅度,光谱和极化的光场的低频(0.05 Hz)横向波动, f最大我们发现跨音速太阳风是普遍的后果。在光波振幅为dv,0 0.7 km s〜-1的足够波输入的情况下,通过压缩波的产生和波的反射,Alfvén波的消散也将大气稳定加热至106K。由于非线性Alfvén波加热的不稳定方面,太阳风的密度以及相应的质量通量显示出对dv,0的非常敏感的依赖性。 = 0.4 km s〜-1的情况下产生的质量通量是基准风速小于dv⊥0> = 0.7 km s〜-1的情况下质量通量的50倍;仅当dv,0变为1/2时,太阳风才真正消失。我们还发现,太阳风速与B r,0 / f max正相关,这与Kojima等人最近的观测结果一致。基于这些发现,我们表明,快速和慢速太阳风都可以通过单个过程,低频Alfvén波的耗散以及dv,0和B r,0 / f max的不同集合来解释。我们的模拟自然地解释了观察到的(1)太阳风速与日冕温度的反相关性,以及(2)快速风中Alfvénic波动的幅度更大。在附录A中,我们还通过一些数值测试解释了MHD波输出边界条件的实现。

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