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arXiv 2410.02468astro-ph.EP
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JWST/MIRI 观测下木星大红斑的热力结构与成分

The Thermal Structure and Composition of Jupiter's Great Red Spot From JWST/MIRI

Jake Harkett, Leigh N. Fletcher, Oliver R. T. King, Michael T. Roman, Henrik Melin, Heidi B. Hammel, Ricardo Hueso, Agustín Sánchez-Lavega, Michael H. Wong, Ste… 展开作者

Jake Harkett, Leigh N. Fletcher, Oliver R. T. King, Michael T. Roman, Henrik Melin, Heidi B. Hammel, Ricardo Hueso, Agustín Sánchez-Lavega, Michael H. Wong, Stefanie N. Milam, Glenn S. Orton, Katherine de Kleer, Patrick G. J. Irwin, Imke de Pater, Thierry Fouchet, Pablo Rodríguez-Ovalle, Patrick M. Fry, Mark R. Showalter

AI总结:

利用JWST/MIRI对木星大红斑进行热力结构与成分反演,揭示其上方平流层热点、深层风场结构、南北不对称性及西北小风暴的强对流特征,并开发了FLT-5波长定标方案。

摘要:

2022年7月和8月,詹姆斯·韦布空间望远镜(JWST)/中红外仪器(MIRI,4.9-27.9微米)对木星大红斑(GRS)进行了成像观测。这些观测与哈勃空间望远镜、JWST/NIRCam、甚大望远镜/VISIR以及业余观测者提供的一系列可见光和红外观测同步进行,为木星圆面提供了空间和时间背景。利用NEMESIS软件反演得到的平流层温度结构揭示了大红斑上方存在一系列热点,这些热点可能是大红斑引起的波动活动的后果。在对流层中,温度结构被用于推导大红斑涡旋的热成风结构。只有当哈勃推导的风场高度位于约1,200 mbar(比先前假设的深得多)时,这些风场才与JWST/NIRCam在240 mbar处独立确定的风场一致。在大红斑内部未发现氨的增强,但在该区域内观测到气溶胶升高与磷化氢丰度之间的联系。在反演的温度、氨、磷化氢和气溶胶结构中观测到南北不对称性,这与大红斑在南北方向上的倾斜一致。最后,在大红斑西北方向捕获到一个小风暴,其反演的磷化氢丰度显示出显著过剩,暗示存在强烈的对流活动。尽管如此,该区域未探测到氨冰。JWST的新颖性要求我们开发定制软件来解决数据定标中的挑战,其中包括推导出"FLT-5"波长定标方案,该方案随后已被整合到标准定标流程中。

英文摘要:

Jupiter's Great Red Spot (GRS) was mapped by the James Webb Space Telescope (JWST)/Mid-Infrared Instrument (4.9-27.9 micron) in July and August 2022. These observations took place alongside a suite of visual and infrared observations from; Hubble, JWST/NIRCam, Very Large Telescope/VISIR and amateur observers which provided both spatial and temporal context across the jovian disc. The stratospheric temperature structure retrieved using the NEMESIS software revealed a series of hot-spots above the GRS. These could be the consequence of GRS-induced wave activity. In the troposphere, the temperature structure was used to derive the thermal wind structure of the GRS vortex. These winds were only consistent with the independently determined wind field by JWST/NIRCam at 240 mbar if the altitude of the Hubble-derived winds were located around 1,200 mbar, considerably deeper than previously assumed. No enhancement in ammonia was found within the GRS but a link between elevated aerosol and phosphine abundances was observed within this region. North-south asymmetries were observed in the retrieved temperature, ammonia, phosphine and aerosol structure, consistent with the GRS tilting in the north-south direction. Finally, a small storm was captured north-west of the GRS that displayed a considerable excess in retrieved phosphine abundance, suggestive of vigorous convection. Despite this, no ammonia ice was detected in this region. The novelty of JWST required us to develop custom-made software to resolve challenges in calibration of the data. This involved the derivation of the "FLT-5" wavelength calibration solution that has subsequently been integrated into the standard calibration pipeline.

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