2024
DOI: 10.1016/j.asr.2023.12.029
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A cyclone formation, eastward plume drag, ion-hydration process, and the consequent ionospheric changes following the 2022 Hunga Tonga-Hunga Ha'apai volcanic eruption

Mohamed Freeshah,
Muhammad Arqim Adil,
Erman Şentürk
et al.
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Cited by 4 publications
(1 citation statement)
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“…As an example, in 2022 the eruption of the Hunga Tonga-Hunga Haapai volcano (southeast of Tonga) triggered the primary cascading hazards, which are eruptive column with ash and gases that extended over 30 km high (Zhao et al 2022). Then, secondary events such as tsunamis, signi cantly affected the local and parts of the Paci c coasts, causing ooding in populated areas (Freeshah et al 2024). According to the World Bank (Partnership et al 2022), the economic damages reached approximately 90 million dollars.…”
Section: Introductionmentioning
confidence: 99%
“…As an example, in 2022 the eruption of the Hunga Tonga-Hunga Haapai volcano (southeast of Tonga) triggered the primary cascading hazards, which are eruptive column with ash and gases that extended over 30 km high (Zhao et al 2022). Then, secondary events such as tsunamis, signi cantly affected the local and parts of the Paci c coasts, causing ooding in populated areas (Freeshah et al 2024). According to the World Bank (Partnership et al 2022), the economic damages reached approximately 90 million dollars.…”
Section: Introductionmentioning
confidence: 99%