Electromagnetic characteristics of ENSO

Petereit, Johannes; Saynisch, Jan; Irrgang, Christopher; Weber, Tobias; Thomas, Maik

doi:https://doi.org/10.5194/os-14-515-2018

Articles | Volume 14, issue 3

https://doi.org/10.5194/os-14-515-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/os-14-515-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 3

Research article

| Highlight paper

|

25 Jun 2018

Research article | Highlight paper |

| 25 Jun 2018

Electromagnetic characteristics of ENSO

Johannes Petereit, Jan Saynisch, Christopher Irrgang, Tobias Weber, and Maik Thomas

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Final revised paper (published on 25 Jun 2018)
Preprint (discussion started on 28 Feb 2018)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of “Electromagnetic characteristics of ENSO” by Petereit, Saynisch, Irrgang, Weber, and Thomas for Ocean Sciences', Anonymous Referee #1, 06 Apr 2018
- RC2: 'review', Anonymous Referee #2, 13 Apr 2018
  - AC1: 'Answer to review #2', Johannes Petereit, 23 May 2018
- AC1: 'Answer to review #2', Johannes Petereit, 23 May 2018
- AC2: 'Answer to review #1', Johannes Petereit, 23 May 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Johannes Petereit on behalf of the Authors (23 May 2018) Author's response Manuscript

ED: Publish as is (30 May 2018) by Neil Wells

AR by Johannes Petereit on behalf of the Authors (01 Jun 2018)

Short summary

The study finds that changes in seawater temperature due to El Niño and La Niña, anomalous warm and cold events, are in principle detectable by means of the oceanic tidally induced magnetic field. Furthermore, subsurface processes in the onset of those anomalous events lead the surface processes by several months. This causes a lead in the oceanic tidally induced magnetic field signals over sea-surface temperature signals.