论文标题
热型外球星的大气层通过过境光谱(Hearts)III解决。未对准的超热木星黄蜂121b的大气结构
Hot Exoplanet Atmospheres Resolved with Transit Spectroscopy (HEARTS) III. Atmospheric structure of the misaligned ultra-hot Jupiter WASP-121b
论文作者
论文摘要
超热木星提供了有趣的前景,以扩大我们有关动力学演化的理论和极度辐照的大气的特性。在这种情况下,我们介绍了用于过境超热木星黄蜂121b的新光谱的分析。我们首先完善WASP-121B的轨道特性,该特性几乎是极性的(倾斜$ψ^{\ rm north} $ = 88.1 $ \ pm $ \ pm $ 0.25 $^{\ circ} $或$ψ^^{\ rm south} $ = 91.11 $ 0.20 $ 0.20 $ 0.20 $ 0.20 $ 0.20 $ 0.快速旋转(p $ <$ 1.13天),高度倾斜($ i_ \ mathrm {\ star}^{\ rm north} $ = 8.1 $ \ stackrel {+3.0} {_ { - 2.6}} south} $ = 171.9 $ \ stackrel {+2.5} {_ { - 3.4}}}}^{\ circ} $)star。然后,我们提出了一种新方法,该方法利用了重新加载的Rossiter-mclaughlin技术,以分离行星大气的贡献和沿着过境和弦的恒星表面的频谱。它在WASP-121B的HARPS转运光谱上的应用显示,在大气肢体中,金属(可能是原子铁)的吸收特征。信号的宽度(14.3 $ \ pm $ 1.2 km/s)可以通过潮汐锁定的行星的旋转来解释。它的Blueshift(-5.2 $ \ pm $ 0.5 km/s)可以追踪从白天到夜间的强风,或行星热层的各向异性膨胀。
Ultra-hot Jupiters offer interesting prospects for expanding our theories on dynamical evolution and the properties of extremely irradiated atmospheres. In this context, we present the analysis of new optical spectroscopy for the transiting ultra-hot Jupiter WASP-121b. We first refine the orbital properties of WASP-121b, which is on a nearly polar (obliquity $ψ^{\rm North}$=88.1$\pm$0.25$^{\circ}$ or $ψ^{\rm South}$=91.11$\pm$0.20$^{\circ}$) orbit, and exclude a high differential rotation for its fast-rotating (P$<$1.13 days), highly inclined ($i_\mathrm{\star}^{\rm North}$=8.1$\stackrel{+3.0}{_{-2.6}}^{\circ}$ or $i_\mathrm{\star}^{\rm South}$=171.9$\stackrel{+2.5}{_{-3.4}}^{\circ}$) star. We then present a new method that exploits the reloaded Rossiter-McLaughlin technique to separate the contribution of the planetary atmosphere and of the spectrum of the stellar surface along the transit chord. Its application to HARPS transit spectroscopy of WASP-121b reveals the absorption signature from metals, likely atomic iron, in the planet atmospheric limb. The width of the signal (14.3$\pm$1.2 km/s) can be explained by the rotation of the tidally locked planet. Its blueshift (-5.2$\pm$0.5 km/s) could trace strong winds from the dayside to the nightside, or the anisotropic expansion of the planetary thermosphere.