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arXiv 1402.2293astro-ph.SR
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来自高分辨率观测和三维模拟的太阳对流的功率谱

The power spectrum of solar convection flows from high-resolution observations and 3D simulations

L. Yelles Chaouche, F. Moreno-Insertis, J. A. Bonet

摘要:

我们比较傅立叶光谱的光球速度场从非常高的分辨率IMaX观测到最近的三维数值磁对流模型。我们进行了一个适当的比较,通过合成谱线的数值模型,然后向他们施加足够的剩余仪器退化,影响观测数据。此外,通常的观测代理的有效性进行了测试,从数值箱获得合成观测和比较的速度代理的实际速度值从数值网格。对于观测,使用了空间分辨率约为120公里的日出/IMaX仪器的数据,从而使观测傅立叶光谱的计算能够很好地进入亚颗粒范围。对于模拟,我们使用四个系列的运行获得的STAGGER代码和合成的IMaX谱线(FeI 5250.2 A)从他们。通过多普勒(垂直分量)和局部相关跟踪(水平分量)获得速度场的代理。观测和模拟傅立叶功率谱之间的一个很好的匹配,获得的垂直速度数据的尺度在200公里和6毫米。相反,一个明确的垂直移动时,合成观测不退化。由于LCT程序的不准确性,水平速度数据的匹配不那么令人印象深刻。关于数值箱的直接速度值与合成观测的直接速度值的内部比较,当在数值箱中使用log($tau_{500}$)= -1表面上的速度值时,获得了垂直分量的高相关性(0.96)。相应的傅立叶谱彼此接近。由于LCT程序的粗糙度,水平速度达到较低的最大相关性(0.5)(在$tau_{500}$ = 1时)。

英文摘要:

We compare Fourier spectra of photospheric velocity fields from very high resolution IMaX observations to those from recent 3D numerical magnetoconvection models. We carry out a proper comparison by synthesizing spectral lines from the numerical models and then applying to them the adequate residual instrumental degradation that affects the observational data. Also, the validity of the usual observational proxies is tested by obtaining synthetic observations from the numerical boxes and comparing the velocity proxies to the actual velocity values from the numerical grid. For the observations, data from the SUNRISE/IMaX instrument with about 120 km spatial resolution are used, thus allowing the calculation of observational Fourier spectra well into the subgranular range. For the simulations, we use four series of runs obtained with the STAGGER code and synthesize the IMaX spectral line (FeI 5250.2 A) from them. Proxies for the velocity field are obtained via Dopplergrams (vertical component) and local correlation tracking (horizontal component). A very good match between observational and simulated Fourier power spectra is obtained for the vertical velocity data for scales between 200 km and 6 Mm. Instead, a clear vertical shift is obtained when the synthetic observations are not degraded. The match for the horizontal velocity data is much less impressive because of the inaccuracies of the LCT procedure. Concerning the internal comparison of the direct velocity values of the numerical boxes with those from the synthetic observations, a high correlation (0.96) is obtained for the vertical component when using the velocity values on the log($tau_{500}$) = -1 surface in the box. The corresponding Fourier spectra are near each other. A lower maximum correlation (0.5) is reached (at $tau_{500}$ = 1) for the horizontal velocities as a result of the coarseness of the LCT procedure.

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