On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event
Abstract Body wave extraction from oceanic secondary microseismic sources with seismic interferometry provides alternative information to better constrain the Earth's structure. However, sources' spatiotemporal variations raise concerns about travel time measurement robustness. Therefore,...
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ftdoajarticles:oai:doaj.org/article:35e9f56e5fb145189f2230c80ba12bd3 2024-09-15T18:09:43+00:00 On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event L. Tomasetto P. Boué L. Stehly F. Ardhuin H.‐C. Nataf 2024-04-01T00:00:00Z https://doi.org/10.1029/2023GL108018 https://doaj.org/article/35e9f56e5fb145189f2230c80ba12bd3 EN eng Wiley https://doi.org/10.1029/2023GL108018 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL108018 https://doaj.org/article/35e9f56e5fb145189f2230c80ba12bd3 Geophysical Research Letters, Vol 51, Iss 8, Pp n/a-n/a (2024) ambient noise body waves secondary microseisms seismic interferometry Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2023GL108018 2024-08-05T17:49:22Z Abstract Body wave extraction from oceanic secondary microseismic sources with seismic interferometry provides alternative information to better constrain the Earth's structure. However, sources' spatiotemporal variations raise concerns about travel time measurement robustness. Therefore, we study the cross‐correlations’ stability during a single oceanic event. This study focuses on 3 days of data and three seismic arrays' combinations between 8 and 11 December 2014 during storm Alexandra, a “weather bomb” event in southern Greenland. We use the WAVEWATCH III hindcast to model P‐wave noise sources and assess the impact of short‐term source variations on cross‐correlations. Model‐based cross‐correlations compared to data show coherent delays to reference 3D Earth models (∼0–3 s) confirming the robustness of the source model which could explain minor travel time variations (≤1 s). Article in Journal/Newspaper Greenland Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 51 8 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
ambient noise body waves secondary microseisms seismic interferometry Geophysics. Cosmic physics QC801-809 |
spellingShingle |
ambient noise body waves secondary microseisms seismic interferometry Geophysics. Cosmic physics QC801-809 L. Tomasetto P. Boué L. Stehly F. Ardhuin H.‐C. Nataf On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
topic_facet |
ambient noise body waves secondary microseisms seismic interferometry Geophysics. Cosmic physics QC801-809 |
description |
Abstract Body wave extraction from oceanic secondary microseismic sources with seismic interferometry provides alternative information to better constrain the Earth's structure. However, sources' spatiotemporal variations raise concerns about travel time measurement robustness. Therefore, we study the cross‐correlations’ stability during a single oceanic event. This study focuses on 3 days of data and three seismic arrays' combinations between 8 and 11 December 2014 during storm Alexandra, a “weather bomb” event in southern Greenland. We use the WAVEWATCH III hindcast to model P‐wave noise sources and assess the impact of short‐term source variations on cross‐correlations. Model‐based cross‐correlations compared to data show coherent delays to reference 3D Earth models (∼0–3 s) confirming the robustness of the source model which could explain minor travel time variations (≤1 s). |
format |
Article in Journal/Newspaper |
author |
L. Tomasetto P. Boué L. Stehly F. Ardhuin H.‐C. Nataf |
author_facet |
L. Tomasetto P. Boué L. Stehly F. Ardhuin H.‐C. Nataf |
author_sort |
L. Tomasetto |
title |
On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
title_short |
On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
title_full |
On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
title_fullStr |
On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
title_full_unstemmed |
On the Stability of Mantle‐Sensitive P‐Wave Interference During a Secondary Microseismic Event |
title_sort |
on the stability of mantle‐sensitive p‐wave interference during a secondary microseismic event |
publisher |
Wiley |
publishDate |
2024 |
url |
https://doi.org/10.1029/2023GL108018 https://doaj.org/article/35e9f56e5fb145189f2230c80ba12bd3 |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
Geophysical Research Letters, Vol 51, Iss 8, Pp n/a-n/a (2024) |
op_relation |
https://doi.org/10.1029/2023GL108018 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL108018 https://doaj.org/article/35e9f56e5fb145189f2230c80ba12bd3 |
op_doi |
https://doi.org/10.1029/2023GL108018 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
8 |
_version_ |
1810447305465135104 |