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arXiv 2002.10379astro-ph.SRastro-ph.EP
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内重力波对亚恒星大气云演化的影响

The effect of internal gravity waves on cloud evolution in sub-stellar atmospheres

Amy Parent, Ruth E. Falconer, Elspeth K. H. Lee, Karen A. Meyer, Craig R. Stark

摘要:

亚恒星物体表现出光度变化,这被认为是由一些过程引起的,如磁驱动的斑点或不均匀的云层覆盖。最近的模型表明,湍流和波,包括内部重力波,可能在云的演变中起重要作用。本文的目的是研究IGW对尘埃成核和尘埃生长的影响,以及由此产生的云结构的观测是否可以用来恢复大气密度信息。对于二维简化大气,数值求解控制流体方程,模拟了IGW通过对尘埃成核和地幔生长的影响。此外,我们推导出一个表达式,将波致云结构的属性与可观测参数联系起来,以推断大气密度。数值模拟表明,$ρ, p, T$变化所造成的重力波导致的成核率的增加高达20倍,和地幔生长率的增加高达1.6倍,相比其平衡值。更广泛的参数空间的探索表明,在绝对值方面,由于IGW的成核增加是较强的冷却器(T矮星)和富TiO 2亚恒星大气。然而,相对增加,是更大的温暖(L矮)和TiO 2-穷人的气氛中,由于条件不太适合有效的成核平衡。这些变化导致了带状区域,其中尘埃的形成更加明显,类似于在地球上观察到的云结构。我们表明,IGW在亚恒星物体的大气中可以产生类似于在地球上观察到的带状云结构。我们提出了一种方法,其中潜在的带状云的观测可以用来估计亚恒星物体的大气密度。

英文摘要:

Sub-stellar objects exhibit photometric variability, which is believed to be caused by a number of processes, such as magnetically-driven spots or inhomogeneous cloud coverage. Recent models have shown that turbulent flows and waves, including internal gravity waves, may play an important role in cloud evolution. The aim of this paper is to investigate the effect of IGW on dust nucleation and dust growth, and whether observations of the resulting cloud structures could be used to recover atmospheric density information. For a simplified atmosphere in two dimensions, we numerically solved the governing fluid equations to simulate the effect on dust nucleation and mantle growth as a result of the passage of an IGW. Furthermore, we derived an expression that relates the properties of the wave-induced cloud structures to observable parameters in order to deduce the atmospheric density. Numerical simulations show that the $ρ, p, T$ variations caused by gravity waves lead to an increase of the nucleation rate by up to a factor 20, and an increase of the mantle growth rate by up to a factor 1.6, compared to their equilibrium values. An exploration of the wider parameter space shows that in absolute terms, the increase in nucleation due to IGW is stronger in cooler (T dwarfs) and TiO2-rich sub-stellar atmospheres. The relative increase, however, is greater in warmer (L dwarf) and TiO2-poor atmospheres due to conditions less suited for efficient nucleation at equilibrium. These variations lead to banded areas in which dust formation is much more pronounced, similar to the cloud structures observed on Earth. We show that IGW in the atmosphere of sub-stellar objects can produce banded clouds structures similar to that observed on Earth. We propose a method with which potential observations of banded clouds could be used to estimate the atmospheric density of sub-stellar objects.

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