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Three-dimensional hydrodynamical CO5BOLD model atmospheres of red giant stars - VI. First chromosphere model of a late-type giant

机译:红色巨型恒星的三维流体动力学CO5BOLD模型大气-VI。晚型巨人的第一个色球层模型

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Aims. Although observational data unequivocally point to the presence of chromospheres in red giant stars, no attempts have been made so far to model them using 3D hydrodynamical model atmospheres. We therefore compute an exploratory 3D hydrodynamical model atmosphere for a cool red giant in order to study the dynamical and thermodynamic properties of its chromosphere, as well as the influence of the chromosphere on its observable properties. Methods. Three-dimensional radiation hydrodynamics simulations are carried out with the CO ~(5) BOLD model atmosphere code for a star with the atmospheric parameters ( T _(eff) ≈ 4010 ?K, log? g = 1.5 , [ M / H ] = 0.0 ), which are similar to those of the K-type giant star Aldebaran ( α Tau). The computational domain extends from the upper convection zone into the chromosphere ( 7.4 ≥ log? τ _(Ross) ≥ ? 12.8 ) and covers several granules in each horizontal direction. Using this model atmosphere, we compute the emergent continuum intensity maps at different wavelengths, spectral line profiles of Ca? ii K, the Ca? ii infrared triplet line at 854.2?nm, and H α , as well as the spectral energy distribution (SED) of the emergent radiative flux. Results. The initial model quickly develops a dynamical chromosphere that is characterised by propagating and interacting shock waves. The peak temperatures in the chromospheric shock fronts reach values of up to 5000?K, although the shock fronts remain quite narrow. Similar to the Sun, the gas temperature distribution in the upper layers of red giant stars is composed of a cool component due to adiabatic cooling in the expanding post-shock regions and a hot component due to shock waves. For this red giant model, the hot component is a rather flat high-temperature tail, which nevertheless affects the resulting average temperatures significantly. Conclusions. The simulations show that the atmospheres of red giant stars are dynamic and intermittent. Consequently, many observable properties cannot be reproduced with static 1D models, but require advanced 3D hydrodynamical modelling. Furthermore, including a chromosphere in the models might produce significant contributions to the emergent UV flux.
机译:目的尽管观测数据明确地指出了红色巨星中存在色球,但到目前为止,还没有尝试使用3D水动力模型大气对它们进行建模。因此,我们计算了一个凉爽的红色巨人的探索性3D水动力模型气氛,以研究其色球层的动力学和热力学性质,以及色球层对其可观测性质的影响。方法。使用CO〜(5)BOLD模型大气代码对大气参数为T((eff)≈4010?K,log?g = 1.5,[M / H] =的恒星进行三维辐射流体动力学模拟0.0),与K型巨星Aldebaran(αTau)的相似。计算域从上层对流区延伸到色球层(7.4≥log?τ_(Ross)≥12.8),并在每个水平方向上覆盖了几个颗粒。使用这种模型大气,我们可以计算出在不同波长下Ca 2+的谱线轮廓的涌现连续谱强度图。 ii K,Ca? ii在854.2?nm处的红外三重态谱线和Hα,以及出射辐射通量的光谱能量分布(SED)。结果。初始模型迅速发展出一个动态色球层,其特征是传播和相互作用的冲击波。色球震荡波峰的峰值温度达到5000?K,尽管震荡波峰仍然很窄。与太阳相似,红色巨星上层的气体温度分布由激波后区域绝热冷却引起的冷成分和激波引起的热成分组成。对于此红色巨人模型,高温组件是相当平坦的高温尾巴,但它会显着影响最终的平均温度。结论。模拟表明,红色巨星的大气是动态的和断断续续的。因此,许多可观察的特性无法用静态1D模型重现,但需要高级3D流体动力学建模。此外,在模型中包含色球层可能会对出现的紫外线通量产生重大贡献。

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