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Updated: Jul 17, 2026

10:35
Bringing the Visible Universe into Focus with Robo-AO
Published on: February 12, 2013
由NASA红外望远镜设施观测的Shoemaker-Levy 9彗星与木星的碰撞
1Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91109.
概括
彗星Shoemaker-Levy 9的撞击显著加热了木星的大气层,使氨水平增加了50倍以上. 这些事件也导致了大范围的大气干扰和极光活动的增强.
科学领域:
- 行星科学 行星科学
- 彗星科学 彗星科学
- 大气物理学 大气物理学
背景情况:
- 1994年,舒马克-莱维9彗星与木星的碰撞为研究对气体巨星的撞击效应提供了独特的机会.
- 以前的观测提供了有限的数据,这些大规模冲击的直接大气后果.
研究的目的:
- 分析木星对彗星Shoemaker-Levy 9撞击的大气和热反应.
- 量化彗星碎片撞击后大气组成和温度的变化.
主要方法:
- 利用美国国家航空航天局 (NASA) 红外望远镜设施进行观测.
- 1994年7月12日至8月7日进行红外光谱和热成像.
- 分析光谱数据以确定大气组成和温度概况.
主要成果:
- 对C,G和R碎片在撞击后几分钟内观察到强烈的热红外辐射.
- 在所有冲击中记录了平流层变暖,在某些情况下记录了热层变暖.
- 测量了平流层氨丰度的显著增加,超过基线的50倍.
- 检测到与撞击相关的粒子达到高度,压力为几毫巴.
- 在撞击后大约一周,北极近红外极光增加了近五倍.
结论:
- 彗星撞击会在木星大气中造成大量可测量的热和化学干扰.
- 观察到的氨量增加表明木星的平流层内有显著的垂直运输和化学反应.
- 撞击喷射物可以达到高大气水平,影响大气动力学和极光等可观测现象.
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