Audible and infrasonic waves generated during the 2022 Hunga eruption: Observations from across Aotearoa New Zealand

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Oliver D. Lamb , Paul A. Jarvis , Geoff Kilgour
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引用次数: 0

Abstract

The 15 January 2022 eruption of Hunga volcano (Kingdom of Tonga) featured one of the most powerful blasts in recent history, generating atmospheric acoustic phenomena observed around the world. Here we examine seismo-acoustic data of the eruption from across Aotearoa New Zealand, host of the densest network of seismo-acoustic sensors in the south-west Pacific. We find clear evidence for two wavepackets of audible acoustics generated by the eruption propagating north-to-south across Aotearoa New Zealand. Celerities estimated from manually picked arrival times indicate that each wavepacket was likely induced by nonlinear phenomena during the passage of Lamb and Pekeris waves, the latter an atmospheric resonance mode not observed prior to the eruption of Hunga volcano. We also highlight results from array processing across a large scale acoustic network, where we successfully detect and estimate backazimuths for coherent low frequency acoustic waves across a maximum aperture of 11 km. The observations presented here provide a new dataset for developing novel techniques for modelling and monitoring of rare atmospheric acoustic phenomena.
2022 年洪加火山爆发期间产生的声波和次声波:新西兰奥特亚罗瓦各地的观测结果
2022 年 1 月 15 日,汤加王国洪加火山喷发,这是近代史上威力最大的一次喷发,产生的大气声学现象在世界各地都能观测到。在此,我们研究了来自新西兰奥特亚罗瓦各地的火山爆发地震声学数据,这里拥有西南太平洋最密集的地震声学传感器网络。我们发现了明确的证据,证明火山爆发产生的两个可听声波包自北向南横穿新西兰奥特亚罗瓦。根据人工选取的到达时间估算出的速度表明,每个波包都可能是在兰姆波和佩克利斯波通过时由非线性现象引起的,后者是在洪加火山爆发前没有观测到的大气共振模式。我们还重点介绍了大规模声学网络阵列处理的结果,我们成功地探测并估算了最大孔径为 11 千米的相干低频声波的后坐力。这里介绍的观测结果为开发罕见大气声学现象建模和监测的新技术提供了新的数据集。
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来源期刊
CiteScore
5.90
自引率
13.80%
发文量
183
审稿时长
19.7 weeks
期刊介绍: An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society. Submission of papers covering the following aspects of volcanology and geothermal research are encouraged: (1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations. (2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis. (3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization. (4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing. (5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts. (6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact.
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