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木星极光电离层和热层的同步红外观测。

Simultaneous Infrared Observations of the Jovian Auroral Ionosphere and Thermosphere.

作者信息

Wang Ruoyan, Stallard Tom S, Melin Henrik, Baines Kevin H, Moore Luke, O'Donoghue James, Johnson Rosie E, Thomas Emma M, Knowles Katie L, Tiranti Paola I, Miller Steve

机构信息

School of Physics and Astronomy University of Leicester Leicester UK.

Department of Mathematics Physics and Electrical Engineering Northumbria University Newcastle upon Tyne UK.

出版信息

J Geophys Res Space Phys. 2024 Dec;129(12):e2024JA032891. doi: 10.1029/2024JA032891. Epub 2024 Nov 30.

DOI:10.1029/2024JA032891
PMID:39618907
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11608104/
Abstract

Simultaneous observations of and in Jupiter's northern infrared aurora were conducted on 02 June 2017 using Keck-NIRSPEC to produce polar projection maps of radiance, rotational temperature, column density, and radiance. The temperature variations within the auroral region are K, generally consistent with previous studies, albeit with some structural differences. Known auroral heating sources including particle precipitation, Joule heating, and ion drag have been examined by studying the correlations between each derived quantity, yet no single dominant mechanism can be identified as the main driver for the energetics in Jupiter's northern auroral region. It appears that a complex interaction exists between the heating driven by various mechanisms and the cooling from the thermostat effect. Comparisons between the temperature and the line-of-sight ion velocity in the reference frame of (a) the planetary rotation and (b) the neutral atmosphere further suggest that the local thermodynamic equilibrium effect may play an important role in thermospheric heating at Jupiter. Along with previously reported heating events that occurred in both the lower and upper atmosphere, it is speculated that the heating source may originate from an altitude above Jupiter's stratosphere but below the peak altitude of overtone and quadrupole emissions.

摘要

2017年6月2日,利用凯克天文台近红外摄谱仪(Keck-NIRSPEC)对木星北部红外极光中的[具体物质1]和[具体物质2]进行了同步观测,以生成[具体物质1]辐射率、旋转温度、柱密度和[具体物质2]辐射率的极射赤面投影图。极光区域内的温度变化为[X]K,总体上与之前的研究一致,尽管存在一些结构差异。通过研究每个导出量之间的相关性,对包括粒子沉降、焦耳加热和离子拖曳在内的已知极光加热源进行了研究,但没有单一的主导机制可以被确定为木星北部极光区域能量学的主要驱动因素。看来,各种机制驱动的加热与[物质名称]恒温器效应导致的冷却之间存在复杂的相互作用。在(a)行星自转和(b)中性大气的参考系中,[具体物质1]温度与视线离子速度之间的比较进一步表明,局部热力学平衡效应可能在木星热层加热中起重要作用。连同之前报道的发生在低层和高层大气中的加热事件,据推测加热源可能起源于木星平流层以上但低于[具体物质1]泛音和[具体物质2]四极发射峰值高度的高度。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/2dc9cf41157a/JGRA-129-0-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/c8a6179bfc4e/JGRA-129-0-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/cc2d23de7ad4/JGRA-129-0-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/e308b7019de1/JGRA-129-0-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/2dc9cf41157a/JGRA-129-0-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/c8a6179bfc4e/JGRA-129-0-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/cc2d23de7ad4/JGRA-129-0-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/e308b7019de1/JGRA-129-0-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c9e/11608104/2dc9cf41157a/JGRA-129-0-g004.jpg

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本文引用的文献

1
Global upper-atmospheric heating on Jupiter by the polar aurorae.木星极地极光引起的全球高层大气加热。
Nature. 2021 Aug;596(7870):54-57. doi: 10.1038/s41586-021-03706-w. Epub 2021 Aug 4.
2
Cooling by H3(+) emission.通过 H3(+) 发射进行冷却。
J Phys Chem A. 2013 Oct 3;117(39):9770-7. doi: 10.1021/jp312468b. Epub 2013 Jul 26.
3
H3+ cooling in planetary atmospheres.行星大气中的 H3+ 冷却。
Faraday Discuss. 2010;147:283-91; discussion 379-403. doi: 10.1039/c004152c.