TY - JOUR
T1 - 3D Traveling Ionospheric Disturbances During the 2022 Hunga Tonga–Hunga Ha’apai Eruption Using GNSS TEC
AU - Cahyadi, Mokhamad Nur
AU - Muslim, Buldan
AU - Muafiry, Ihsan Naufal
AU - Gusman, Aditya Riadi
AU - Handoko, Eko Yuli
AU - Anjasmara, Ira Mutiara
AU - Putra, Meilfan Eka
AU - Wulansari, Mega
AU - Lestari, Dwi Sri
AU - Jin, Shuanggen
AU - Sri Sumantyo, Josaphat Tetuko
N1 - Publisher Copyright:
© 2024. American Geophysical Union. All Rights Reserved.
PY - 2024/3
Y1 - 2024/3
N2 - The dual frequency Global Navigation Satellite System (GNSS) observations could determine the total electron content (TEC) in the ionosphere. In this study, GNSS TEC was applied to detect traveling ionospheric disturbances (TIDs) after the eruption of Hunga Tonga–Hunga Ha’apai (HTHH) on 15 January 2022. The eruption caused two types of tsunamis, first is tsunami generated by atmospheric wave (meteo-tsunami) and second is caused by eruption induces water displacement or tsunami classic. At the same time with former tsunami, the atmospheric wave (shock and lamb waves) also caused TIDs at a speed of approximately ∼0.3 km/s. We found moderate correlation between this TIDs amplitude and the tsunami wave height model from tide gauge stations in New Zealand (0.64) and Australia (0.65). Further we attempted to reveal 3D structure of the TIDs in New Zealand, South Australia, and Philippines using 3D tomography. The tomography was set up > 1,170 blocks, as large as 1.0° (east–west) × 1.0° (north–south) × 100 km (vertical), up to 600 km altitude over selected regions. Tomogram shows beautiful concentric directivity of the first TIDs generated by atmospheric wave (AW).
AB - The dual frequency Global Navigation Satellite System (GNSS) observations could determine the total electron content (TEC) in the ionosphere. In this study, GNSS TEC was applied to detect traveling ionospheric disturbances (TIDs) after the eruption of Hunga Tonga–Hunga Ha’apai (HTHH) on 15 January 2022. The eruption caused two types of tsunamis, first is tsunami generated by atmospheric wave (meteo-tsunami) and second is caused by eruption induces water displacement or tsunami classic. At the same time with former tsunami, the atmospheric wave (shock and lamb waves) also caused TIDs at a speed of approximately ∼0.3 km/s. We found moderate correlation between this TIDs amplitude and the tsunami wave height model from tide gauge stations in New Zealand (0.64) and Australia (0.65). Further we attempted to reveal 3D structure of the TIDs in New Zealand, South Australia, and Philippines using 3D tomography. The tomography was set up > 1,170 blocks, as large as 1.0° (east–west) × 1.0° (north–south) × 100 km (vertical), up to 600 km altitude over selected regions. Tomogram shows beautiful concentric directivity of the first TIDs generated by atmospheric wave (AW).
KW - GNSS
KW - TEC
KW - Tonga
KW - ionospheric disturbances
KW - tomography
UR - http://www.scopus.com/inward/record.url?scp=85186625084&partnerID=8YFLogxK
U2 - 10.1029/2023JA031806
DO - 10.1029/2023JA031806
M3 - Article
AN - SCOPUS:85186625084
SN - 2169-9380
VL - 129
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 3
M1 - e2023JA031806
ER -