来自2022年洪加,加火山爆发的中层层压力源激发了3.6毫赫兹的空海合波
Takashi Tonegawa1, Yoshio Fukao1
1Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa, Yokohama 236-0001, Japan.
Science advances
|June 28, 2023
概括
2022年通加火山爆发引发了羔羊波和流星海. 显而易见的3.6毫赫兹的光谱峰值表明中层层中存在压力源,高于火山羽毛.
科学领域:
- 大气科学 大气科学
- 海洋学 海洋学 海洋学
- 火山学 火山学是一门学科.
背景情况:
- 2022年加火山爆发产生了全球观测到的显著的大气和海洋波.
- 羔羊波和流星海是大规模大气干扰造成的现象.
研究的目的:
- 为了分析来自加火山爆发的Lamb波和meteotsunamis的光谱特征.
- 确定产生这些广泛干扰的源机制和位置.
主要方法:
- 分析空气和海底压力数据以确定光谱峰值.
- 在特定的高度和持续时间上升的压力源的建模.
- 通过共振合和沟相互作用研究波放大.
主要成果:
- 在空气和海底压力数据中发现了一个明显的光谱峰值,约为3.6毫赫兹.
- 观察到Lamb波和热层重力波之间的共振合.
- 模拟显示,压力源位于海拔58-70公里处,位于火山顶上方.
- 天文海在日本海沟中显示放大,这是由于与海模式的近共振.
结论:
- 宽带Lamb波的光谱结构,包括3.6毫赫兹的峰值,指出中层层是太平洋规模空海干扰的起源.
- 加火山爆发对大气的影响显著扩展到上层大气层,影响波浪的产生和传播.
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