洪加通加-洪加哈帕伊火山爆发引发的多种海
Patrick Lynett1, Maile McCann2, Zili Zhou2
1Tsunami Research Center, Sonny Astani Department of Civil and Environmental Engineering, University of Southern California, Los Angeles, CA, USA. plynett@usc.edu.
Nature
|August 8, 2022
概括
2022年Hunga Tonga-Hunga Ha'apai喷发通过多种机制产生全球海,包括冲击波和空气压力脉冲. 了解这些过程对于评估未来火山事件带来的沿海风险至关重要.
科学领域:
- 地质学
- 火山学
- 海洋学
背景情况:
- 2022年1月15日,Hunga Tonga-Hunga Ha'apai火山爆发,导致大范围的灰降落并产生全球海.
- 这是自1883年克拉卡图火山爆发以来,用现代仪器观测到的大型新兴火山爆发的第一场海.
研究的目的:
- 调查洪加和洪加哈帕伊火山爆发期间造成海的多种机制.
- 分析近距离和远距离海的特征及其影响因素.
- 评估类似地质环境中的沿海危险评估的影响.
主要方法:
- 分析了2022年洪加通加火山爆发的观测数据.
- 通过空气-海洋合,水腔崩和空气压力脉冲的海生成模型.
- 近场和远场海影响的比较.
主要成果:
- 这次喷发通过三个主要机制产生了海:初始冲击波的空海合,水腔的崩,以及全球空气压力脉冲.
- 近场海冲击主要由水源造成.
- 远距离海, 这是异常持久,
结论:
- 气压脉冲机制在产生全球和持续远场海方面发挥了重要作用.
- 连同未来类似事件的海平面上升也可能大大加剧沿海地区的破坏.
- 由于火山爆发而产生的海是全球危险的一个被忽视的来源.
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