Articles | Volume 23, issue 12
https://doi.org/10.5194/nhess-23-3671-2023
https://doi.org/10.5194/nhess-23-3671-2023
Research article
 | 
29 Nov 2023
Research article |  | 29 Nov 2023

The 2021 La Palma volcanic eruption and its impact on ionospheric scintillation as measured from GNSS reference stations, GNSS-R and GNSS-RO

Carlos Molina, Badr-Eddine Boudriki Semlali, Guillermo González-Casado, Hyuk Park, and Adriano Camps

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1089', Anonymous Referee #1, 03 Jan 2023
    • AC1: 'Reply on RC1', Carlos Molina, 20 Mar 2023
  • RC2: 'Comment on egusphere-2022-1089', Anonymous Referee #2, 06 Feb 2023
    • AC2: 'Reply on RC2', Carlos Molina, 21 Mar 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (01 May 2023) by Rachid Omira
AR by Carlos Molina on behalf of the Authors (12 Jun 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 Jun 2023) by Rachid Omira
RR by Anonymous Referee #1 (09 Aug 2023)
RR by Anonymous Referee #2 (14 Aug 2023)
ED: Publish subject to minor revisions (review by editor) (04 Sep 2023) by Rachid Omira
AR by Carlos Molina on behalf of the Authors (19 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (10 Oct 2023) by Rachid Omira
AR by Carlos Molina on behalf of the Authors (11 Oct 2023)  Manuscript 
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Short summary
Global navigation satellite system signals are used to measure the perturbations induced in the ionosphere by earthquakes related to volcanic eruptions. The study uses data from ground stations and satellites measuring the signals reflected on the ocean or during radio occultation. The results shows a small correlation, but given the small magnitude of the earthquakes, it is difficult to apply this concept to any practical application that finds earthquake proxies in ionospheric perturbations.
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