Articles | Volume 22, issue 2
https://doi.org/10.5194/nhess-22-617-2022
https://doi.org/10.5194/nhess-22-617-2022
Research article
 | Highlight paper
 | 
25 Feb 2022
Research article | Highlight paper |  | 25 Feb 2022

Multilayer modelling of waves generated by explosive subaqueous volcanism

Matthew W. Hayward, Colin N. Whittaker, Emily M. Lane, William L. Power, Stéphane Popinet, and James D. L. White

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on nhess-2021-109', Stephan Grilli, 25 Aug 2021
  • CC2: 'Comment on nhess-2021-109', Stephan Grilli, 25 Aug 2021
  • RC1: 'Comment on nhess-2021-109', Stephan Grilli, 29 Aug 2021
    • AC1: 'Reply on RC1', Matthew Hayward, 07 Oct 2021
  • RC2: 'Comment on nhess-2021-109', Simon J. Barker, 06 Sep 2021
    • AC2: 'Reply on RC2', Matthew Hayward, 07 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (12 Nov 2021) by Animesh Gain
AR by Matthew Hayward on behalf of the Authors (12 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (22 Nov 2021) by Animesh Gain
RR by Anonymous Referee #3 (16 Dec 2021)
RR by Simon J. Barker (22 Dec 2021)
ED: Publish subject to minor revisions (review by editor) (01 Jan 2022) by Animesh Gain
AR by Matthew Hayward on behalf of the Authors (02 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (25 Jan 2022) by Animesh Gain
ED: Publish as is (25 Jan 2022) by Animesh Gain
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Short summary
Volcanic eruptions can produce tsunamis through multiple mechanisms. We present validation cases for a numerical method used in simulating waves caused by submarine explosions: a laboratory flume experiment and waves generated by explosions at field scale. We then demonstrate the use of the scheme for simulating analogous volcanic eruptions, illustrating the resulting wavefield. We show that this scheme models such dispersive sources more proficiently than standard tsunami models.
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