Tracking tsunami propagation and Island's collapse after the Hunga Tonga Hunga Ha'apai 2022 volcanic eruption from multi-space observations
School authors:
author photo
Rodrigo Alberto Cienfuegos
author photo
Marcos Simon Moreno
External authors:
  • Mahesh N. Shrivastava ( Universidad Catolica del Norte , Ctr Invest Gest Integrada Riesgo Desastres , Millenium Inst Volcan Risk Res Ckelar Volcanoes )
  • A. S. Sunil ( Cochin University Science & Technology )
  • Ajeet K. Maurya ( Babasaheb Bhimrao Ambedkar University )
  • Felipe Aguilera ( Universidad Catolica del Norte , Millenium Inst Volcan Risk Res Ckelar Volcanoes )
  • Simon Orrego ( Universidad Catolica del Norte )
  • P. S. Sunil ( Cochin University Science & Technology )
Abstract:

The quantity and accuracy of satellite-geodetic measurements have increased over time, revolutionizing the monitoring of tectonic processes. Global Navigation Satellite System (GNSS) and satellite radar signals provide observations beyond ground deformation, including how earthquake and tsunami processes affect variations in the ionosphere. Here, we study the Hunga Tonga Hunga Ha'apai (HTHH) volcanic eruption 2022 and its associated tsunami propagation with the analysis GNSS derived Total Electron Content (TEC), Synthetic Aperture Radar (SAR) Sentinel-1 data, complemented with tide gauge observations. We utilize GNSS sites data within a similar to 5000 km radius from the volcanic eruption for estimating the ionospheric perturbation as Vertical TEC. We give evidence on the detection of acoustic gravity, internal gravity, and atmospheric Lamb waves signatures in the TEC perturbation. In particular, the internal gravity waves that concentrated in the southwest of Tonga, directly correlates with the observed tsunami propagation direction as accounted by the tide gauge measurements. However, the acoustic gravity wave signature in the TEC is dominant in the north direction suggesting a surface deformation, which could be verified using Sentinel-1A SAR amplitude data. The analysis presented herein shows that within 5 h of the volcanic eruption, the central part of the HTHH island landscape disappeared with the biggest explosion. The unprecedented detail resolved by integrating satellite data yields previously unknown details of the deformation of the 2022 HTHH volcano eruption.

UT WOS:001125371600010
Number of Citations 5
Type
Pages
ISSUE 1
Volume 13
Month of Publication NOV 17
Year of Publication 2023
DOI https://doi.org/10.1038/s41598-023-46397-1
ISSN
ISBN