论文标题
来自双面模拟的毫米波长的冲击波特征表征
Characterisation of shock wave signatures at millimetre wavelengths from Bifrost simulations
论文作者
论文摘要
毫米波长的观测为研究太阳能球体中的小规模动力学提供了宝贵的工具。我们在存在繁殖的冲击波的情况下评估了大气的物理条件,并将其与MM波长辐射中可观察到的特征联系起来,从而为MM波长观测值提供了宝贵的见解。来自3D辐射磁水动力学(MHD)代码双果的现实数值模拟用于解释由冲击波传播引起的大气变化。亮度温度(T $ _ \ text {b} $)的高效率(1 s)时间序列是通过高级辐射传输(ART)代码计算的,其波长为$ 1.309 $毫米和$ 1.204 $毫米,代表光谱带的相对侧面,代表了Atacama大型毫米/sibbillimeter/sibbillimeter(Alma)的相对侧面。提出了冲击波传播的一个例子。亮度温度显示出强烈的冲击波签名,地层高度在$ \ sim0.7 $至$ 1.4 $毫米之间的变化很大。结果表明,毫米亮度温度有效地跟踪中染色体中的冲击波向上传播。此外,我们表明,Alma带$ 6 $之间波长之间亮度温度的梯度可能被用作诊断工具,以了解采样层处的小规模动力学。
Observations at millimetre wavelengths provide a valuable tool to study the small scale dynamics in the solar chromosphere. We evaluate the physical conditions of the atmosphere in the presence of a propagating shock wave and link that to the observable signatures in mm-wavelength radiation, providing valuable insights into the underlying physics of mm-wavelength observations. A realistic numerical simulation from the 3D radiative Magnetohydrodynamic (MHD) code Bifrost is used to interpret changes in the atmosphere caused by shock wave propagation. High-cadence (1 s) time series of brightness temperature (T$_\text{b}$) maps are calculated with the Advanced Radiative Transfer (ART) code at the wavelengths $1.309$ mm and $1.204$ mm, which represents opposite sides of spectral band~$6$ of the Atacama Large Millimeter/submillimeter Array (ALMA). An example of shock wave propagation is presented. The brightness temperatures show a strong shock wave signature with large variation in formation height between $\sim0.7$ to $1.4$ Mm. The results demonstrate that millimetre brightness temperatures efficiently track upwardly propagating shock waves in the middle chromosphere. In addition, we show that the gradient of the brightness temperature between wavelengths within ALMA band $6$ can potentially be utilised as a diagnostics tool in understanding the small-scale dynamics at the sampled layers.