Volcanic lightning reveals umbrella cloud dynamics of the 15 January 2022 Hunga volcano eruption, Tonga

被引:1
|
作者
Jarvis, P. A. [1 ]
Caldwell, T. G. [1 ]
Noble, C. [2 ]
Ogawa, Y. [3 ,6 ]
Vagasky, C. [4 ,5 ]
机构
[1] GNS Sci, POB 30368, Lower Hutt 5040, New Zealand
[2] MetService, POB 722, Wellington 6140, New Zealand
[3] Tokyo Inst Technol, Inst Innovat Res, Multidisciplinary Resilience Res Ctr, Tokyo, Japan
[4] Vaisala Inc, Louisville, CO USA
[5] Univ WI Madison, Dept Plant & Agroecosyst Sci, Madison, WI USA
[6] Tohoku Univ, Res Ctr Predict Earthquakes & Volcan Erupt, Grad Sch Sci, Sendai, Japan
关键词
Hunga; Volcanic lightning; Satellite; Umbrella cloud; SAKURAJIMA-VOLCANO; HAAPAI VOLCANO; PLUMES; ELECTRIFICATION;
D O I
10.1007/s00445-024-01739-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The 15 January 2022 eruption of Hunga volcano, Tonga, significantly impacted the Kingdom of Tonga as well as the wider Pacific region. The eruption column attained a maximum height of 58 km whilst the umbrella cloud reached a diameter approaching 600 km within about 3 h. The frequency of volcanic lightning generated during the eruption was also unprecedented, with the Vaisala Global Lightning Database (GLD360) recording over 3 x 10(5) strikes over a 2-h period. We have combined Himawari-8 satellite imagery with the spatiotemporal distribution of lightning strikes to constrain the dynamics of umbrella spreading and infer a timeline of events for the climactic phase of the eruption. Lightning was initially concentrated directly above Hunga, with an areal extent that grew with the observed eruption cloud. However, about 20 min after the eruption onset, radial structure appeared in the lightning spatial distribution, with strikes clustered both directly above Hunga and in an annulus of radius similar to 50 km. Comparison with satellite imagery shows that this annulus coincided with the umbrella cloud front. The lightning annulus and umbrella front grew synchronously to a radius of similar to 150 km before the umbrella cloud growth rate decreased whilst the annulus itself contracted to a smaller radius of about 50 km again. We interpret that the lightning annulus resulted from an enhanced rate of particle collisions and subsequent triboelectrification due to enhanced vorticity in the umbrella cloud head. Our results demonstrate that volcanic lightning observations can provide insights into the internal dynamics of umbrella clouds and should motivate more quantitative models of umbrella spreading.
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页数:17
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