{"title":"Significant Elastic Ground Deformations After the January 15, 2022 Hunga-Tonga Eruption","authors":"Long Tang;Wu Chen;Kai Zheng;Pan Li","doi":"10.1109/LGRS.2025.3545686","DOIUrl":null,"url":null,"abstract":"This study reports the unusual decimeter-scale elastic ground deformations observed by the Global Navigation Satellite System (GNSS) station TONG in Nuku’alofa after the tremendous January 15, 2022 Hunga-Tonga eruption. There are significant uplifts with a maximum of 0.35 m in the vertical direction; the elastic deformations are also obvious with a maximum of 0.15 m in the south direction while are very tiny in the east direction. In addition, the occurred period of the elastic deformations is consistent to the eruption-induced tsunamis recorded in a nearby tide gauge station. The characteristics of the observed elastic deformations confirm their link to the Hunga-Tonga eruption. The possible cause for the elastic deformations is the sustained thrusts from the eruption.","PeriodicalId":91017,"journal":{"name":"IEEE geoscience and remote sensing letters : a publication of the IEEE Geoscience and Remote Sensing Society","volume":"22 ","pages":"1-4"},"PeriodicalIF":0.0000,"publicationDate":"2025-02-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"IEEE geoscience and remote sensing letters : a publication of the IEEE Geoscience and Remote Sensing Society","FirstCategoryId":"1085","ListUrlMain":"https://ieeexplore.ieee.org/document/10902549/","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
This study reports the unusual decimeter-scale elastic ground deformations observed by the Global Navigation Satellite System (GNSS) station TONG in Nuku’alofa after the tremendous January 15, 2022 Hunga-Tonga eruption. There are significant uplifts with a maximum of 0.35 m in the vertical direction; the elastic deformations are also obvious with a maximum of 0.15 m in the south direction while are very tiny in the east direction. In addition, the occurred period of the elastic deformations is consistent to the eruption-induced tsunamis recorded in a nearby tide gauge station. The characteristics of the observed elastic deformations confirm their link to the Hunga-Tonga eruption. The possible cause for the elastic deformations is the sustained thrusts from the eruption.