论文标题
在太阳光球上方的逃生声波中测得的相移及其对局部气旋学的可能影响
Phase Shifts Measured in Evanescent Acoustic Waves above the Solar Photosphere and Their Possible Impacts to Local Helioseismology
论文作者
论文摘要
使用安装在Dunn太阳能望远镜上的干涉量学双维光谱仪(IBIS)获得了一组464分钟的高分辨率高积累观测值。十组多普勒格(Dopplergram)源自光谱线的一分子,该频谱线的分配器大约对应于不同的大气高度,并且使用MDI样算法和重中心方法得出了两组多普勒格拉姆。然后对这些数据进行过滤以保持声学模式,并在不同大气高度的多普勒速度之间计算出相移作为声频率的函数。对频率和高度依赖性相位偏移的分析表明,对于逃生的声波,较高大气中的振荡导致较低大气中的人在频率低于3.0 MHz的频率下方1秒钟,而当频率频率高于3.0 MHz时,则落后约1 s。在具有系统的向上或向下流动的区域中也发现了不可忽略的相移。所有这些频率依赖性相位移动无法通过垂直流或对流的蓝光来解释,但可能是由于复杂的流体动力学和光电球中非绝热大气中的辐射转移所致。这些相位波的这些相移对某些局部热溶测量的解释构成了巨大的挑战,这些测量涉及在不同的大气高度或具有系统垂直流的区域中获取的数据。需要对这些相移的更定量表征,以便可以在测量过程中将它们删除,也可以在Helioseisic倒置中解释。
A set of 464-min high-resolution high-cadence observations were acquired for a region near the Sun's disk center using the Interferometric BI-dimensional Spectrometer (IBIS) installed at the Dunn Solar Telescope. Ten sets of Dopplergrams are derived from the bisector of the spectral line corresponding approximately to different atmospheric heights, and two sets of Dopplergrams are derived using MDI-like algorithm and center-of-gravity method. These data are then filtered to keep only acoustic modes, and phase shifts are calculated between Doppler velocities of different atmospheric heights as a function of acoustic frequency. The analysis of the frequency- and height-dependent phase shifts shows that for evanescent acoustic waves, oscillations in the higher atmosphere lead those in the lower atmosphere by an order of 1 s when their frequencies are below about 3.0 mHz, and lags behind by about 1 s when their frequencies are above 3.0 mHz. Non-negligible phase shifts are also found in areas with systematic upward or downward flows. All these frequency-dependent phase shifts cannot be explained by vertical flows or convective blueshifts, but are likely due to complicated hydrodynamics and radiative transfer in the non-adiabatic atmosphere in and above the photosphere. These phase shifts in the evanescent waves pose great challenges to the interpretation of some local helioseismic measurements that involve data acquired at different atmospheric heights or in regions with systematic vertical flows. More quantitative characterization of these phase shifts is needed so that they can either be removed during measuring processes or be accounted for in helioseismic inversions.