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Updated: May 5, 2026

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围绕木星两极的旋风群
Nature
|March 9, 2018
概括
木星的极地呈现出独特的多边形气旋模式, 与其他行星所见的不同. 这些持续的,不合并的旋风挑战了当前的行星大气动态模型.
科学领域:
- 星球科学
- 大气动力学
- 流体力学
背景情况:
- 木星的低度有轴对称的区域和带.
- 高度过渡到普遍的气旋活动.
- 之前的任务由于轨迹的限制而对极地地区的描述有限.
研究的目的:
- 描述木星以前没有观察到的极地天气系统.
- 调查木星极点的独特气旋模式.
主要方法:
- 分析来自朱诺号太空船极地轨道的可见和红外图像.
- 在20分钟至4小时间隔进行时间间隔图像分析,以确定旋风循环.
主要成果:
- 在木星的两极都发现了持续的多边形气旋.
- 在一个北极旋风周围观察到八个环极旋风.
- 在南方的单个极地旋风周围观察到五个环极旋风.
结论:
- 木星的极地气旋形成了前所未有的结构, 与其他已知的行星特征不同.
- 这些旋风的持续性和构造,为了解行星大气动态和科里奥利斯β效应带来了新的挑战.
- 这些极地气旋的进化路径和不合并行为仍然未知.
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