论文标题
WASP-5 B的近红外和光学发射
Near infrared and optical emission of WASP-5 b
论文作者
论文摘要
环境:外行星的热发射使得可以研究其大气中的重要物理过程并得出更精确的轨道元素。目的:通过使用新的近红外和光学数据,我们研究了这些数据如何限制行星大气的轨道偏心率和热特性。方法:苔丝卫星从两个扇区获得的完整光曲线用于对行星相变的幅度提出上限,并估计掩盖深度。在2个Mass K(KS)频段中,已经出版的两个,但未发表的后续观测值在此近红外波段中得出了更精确的掩盖光曲线。结果:KS频段中合并的掩盖光曲线包含4515个数据点。数据证实了较早的偏心率估计的结果,表明圆形轨道:e = 0.005 +/- 0.015。 KS带中(2.70 +/- 0.14)PPT的通量抑郁症的高值不包括10个Sigma水平的简单黑体发射,并且在(4-7)Sigma水平上也不同意当前大气模型。从对苔丝数据的分析中,在视觉频段中,我们发现了次要食物的近噪声水平检测的初步证据,并将约束放在行星相变的相关振幅上。正式盒子的固定深度为(0.157 +/- 0.056)ppt。这意味着完全有效的大气循环的Ag = 0.43 +/- 0.15相对较高的几何反照率,Ag = 0.29 +/- 0.15完全没有循环。对于氧增强或碳增大大气模型,看不到偏好。
CONTEXT: Thermal emission from extrasolar planets makes it possible to study important physical processes in their atmospheres and derive more precise orbital elements. AIMS: By using new near infrared and optical data, we examine how these data constrain the orbital eccentricity and the thermal properties of the planet atmosphere. METHODS: The full light curves acquired by the TESS satellite from two sectors are used to put upper limit on the amplitude of the planet's phase variation and estimate the occultation depth. Two, already published and one, yet unpublished followup observations in the 2MASS K (Ks) band are employed to derive a more precise occultation light curve in this near infrared waveband. RESULTS: The merged occultation light curve in the Ks band comprises 4515 data points. The data confirm the results of the earlier eccentricity estimates, suggesting circular orbit: e=0.005+/-0.015. The high value of the flux depression of (2.70+/-0.14) ppt in the Ks band excludes simple black body emission at the 10 sigma level and disagrees also with current atmospheric models at the (4-7) sigma level. From the analysis of the TESS data, in the visual band we found tentative evidence for a near noise level detection of the secondary eclipse, and placed constraints on the associated amplitude of the planet's phase variation. A formal box fit yields an occultation depth of (0.157+/-0.056) ppt. This implies a relatively high geometric albedo of Ag=0.43+/-0.15 for fully efficient atmospheric circulation and Ag=0.29+/-0.15 for no circulation at all. No preference can be seen either for the oxygen-enhanced, or for the carbon-enhanced atmosphere models.