Articles | Volume 12, issue 2
Solid Earth, 12, 503–520, 2021
https://doi.org/10.5194/se-12-503-2021
Solid Earth, 12, 503–520, 2021
https://doi.org/10.5194/se-12-503-2021

Research article 25 Feb 2021

Research article | 25 Feb 2021

Characterizing the oceanic ambient noise as recorded by the dense seismo-acoustic Kazakh network

Alexandr Smirnov et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Alexandr Smirnov on behalf of the Authors (18 Aug 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Sep 2020) by CharLotte Krawczyk
RR by Jelle Assink (02 Oct 2020)
ED: Reconsider after major revisions (14 Oct 2020) by CharLotte Krawczyk
AR by Alexandr Smirnov on behalf of the Authors (22 Nov 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (05 Dec 2020) by CharLotte Krawczyk
RR by Jelle Assink (07 Jan 2021)
ED: Publish subject to minor revisions (review by editor) (07 Jan 2021) by CharLotte Krawczyk
AR by Alexandr Smirnov on behalf of the Authors (12 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (13 Jan 2021) by CharLotte Krawczyk
ED: Publish as is (13 Jan 2021) by CharLotte Krawczyk(Executive Editor)
AR by Alexandr Smirnov on behalf of the Authors (17 Jan 2021)  Author's response    Manuscript
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Short summary
Seismic and infrasound methods are techniques used to monitor natural events and explosions. At low frequencies, band signal can be dominated by microbaroms and microseisms. The noise observations in the Kazakh network are performed and compared with source and propagation modeling. The network is dense and well situated for studying very distant source regions of the ambient noise. The prospects are opening for the use of ocean noise in solid Earth and atmosphere tomography.