Megameter propagation and correlation of T-waves from Kermadec Trench and Islands

On 18 June 2020 and 4 March 2021, very energetic low-frequency underwater T-wave signals (2 to 25 Hz) were recorded at the Comprehensive Nuclear-Test-Ban Treaty (CTBT) International Monitoring System (IMS) hydrophone stations in the Pacific Ocean (Stations HA11 and HA03) and the South Atlantic Ocean...

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Main Authors: Tiago C. A. Oliveira, Peter Nielsen, Ying-Tsong Lin, Noriyuki Kushida, Sérgio M. Jesus
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-11-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.1009013/full
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author Tiago C. A. Oliveira
Peter Nielsen
Ying-Tsong Lin
Noriyuki Kushida
Sérgio M. Jesus
author_facet Tiago C. A. Oliveira
Peter Nielsen
Ying-Tsong Lin
Noriyuki Kushida
Sérgio M. Jesus
author_sort Tiago C. A. Oliveira
collection DOAJ
description On 18 June 2020 and 4 March 2021, very energetic low-frequency underwater T-wave signals (2 to 25 Hz) were recorded at the Comprehensive Nuclear-Test-Ban Treaty (CTBT) International Monitoring System (IMS) hydrophone stations in the Pacific Ocean (Stations HA11 and HA03) and the South Atlantic Ocean (Station HA10). This work investigates the long-range (megameters) propagation of these T-waves. Their sources were three powerful submarine earthquakes in the Kermadec Trench and Islands, located at approximately 6000, 8800, and 15100 km from Stations HA11, HA03, and HA10, respectively. Arrival time and back azimuth of the recorded T-waves were estimated using the Progressive Multi-Channel Correlation algorithm installed on the CTBT Organization (CTBTO) virtual Data Exploitation Centre (vDEC). Different arrivals within the duration of the earthquake signals were identified, and their correlations were also analyzed. The data analysis at HA03 and HA10 revealed intriguing T-wave propagation paths reflecting, refracting, or even transmitting through continents, as well as T-wave excitation along a chain of seamounts. The analysis also showed much higher transmission loss (TL) in the propagation paths to HA11 than to HA03 and HA10. Moreover, strong discrepancies between expected and measured back azimuths were observed for HA11, and a three-dimensional (3D) parabolic equation model was utilized to identify the cause of these differences. Numerical results revealed the importance of 3D effects induced by the Kermadec Ridge, Fiji archipelago, and Marshall Islands on T-wave propagation to HA11. This analysis can guide future improvements in underwater event localization using the CTBT-IMS hydroacoustic sensor network.
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spelling doaj.art-3f1f15d7905642b18b749cdb3bea31f82022-12-22T04:14:08ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-11-01910.3389/fmars.2022.10090131009013Megameter propagation and correlation of T-waves from Kermadec Trench and IslandsTiago C. A. Oliveira0Peter Nielsen1Ying-Tsong Lin2Noriyuki Kushida3Sérgio M. Jesus4Physics Department and Centre of Environmental and Marine Studies, University of Aveiro, Aveiro, PortugalIndependent Researcher, Esbjerg N, DenmarkApplied Ocean Physics and Engineering Department, Woods Hole Oceanographic Institution, Woods Hole, MA, United StatesInternational Data Centre, Comprehensive Nuclear-Test-Ban Treaty Organization, Vienna, AustriaLaboratory of Robotics and Engineering Systems, University of Algarve, Faro, PortugalOn 18 June 2020 and 4 March 2021, very energetic low-frequency underwater T-wave signals (2 to 25 Hz) were recorded at the Comprehensive Nuclear-Test-Ban Treaty (CTBT) International Monitoring System (IMS) hydrophone stations in the Pacific Ocean (Stations HA11 and HA03) and the South Atlantic Ocean (Station HA10). This work investigates the long-range (megameters) propagation of these T-waves. Their sources were three powerful submarine earthquakes in the Kermadec Trench and Islands, located at approximately 6000, 8800, and 15100 km from Stations HA11, HA03, and HA10, respectively. Arrival time and back azimuth of the recorded T-waves were estimated using the Progressive Multi-Channel Correlation algorithm installed on the CTBT Organization (CTBTO) virtual Data Exploitation Centre (vDEC). Different arrivals within the duration of the earthquake signals were identified, and their correlations were also analyzed. The data analysis at HA03 and HA10 revealed intriguing T-wave propagation paths reflecting, refracting, or even transmitting through continents, as well as T-wave excitation along a chain of seamounts. The analysis also showed much higher transmission loss (TL) in the propagation paths to HA11 than to HA03 and HA10. Moreover, strong discrepancies between expected and measured back azimuths were observed for HA11, and a three-dimensional (3D) parabolic equation model was utilized to identify the cause of these differences. Numerical results revealed the importance of 3D effects induced by the Kermadec Ridge, Fiji archipelago, and Marshall Islands on T-wave propagation to HA11. This analysis can guide future improvements in underwater event localization using the CTBT-IMS hydroacoustic sensor network.https://www.frontiersin.org/articles/10.3389/fmars.2022.1009013/fullunderwater soundscape3DPECTBT-IMSpassive acousticsDTK-GPMCCsubmarine earthquake
spellingShingle Tiago C. A. Oliveira
Peter Nielsen
Ying-Tsong Lin
Noriyuki Kushida
Sérgio M. Jesus
Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
Frontiers in Marine Science
underwater soundscape
3DPE
CTBT-IMS
passive acoustics
DTK-GPMCC
submarine earthquake
title Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
title_full Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
title_fullStr Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
title_full_unstemmed Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
title_short Megameter propagation and correlation of T-waves from Kermadec Trench and Islands
title_sort megameter propagation and correlation of t waves from kermadec trench and islands
topic underwater soundscape
3DPE
CTBT-IMS
passive acoustics
DTK-GPMCC
submarine earthquake
url https://www.frontiersin.org/articles/10.3389/fmars.2022.1009013/full
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AT noriyukikushida megameterpropagationandcorrelationoftwavesfromkermadectrenchandislands
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