Estimating ocean tide model uncertainties for electromagnetic inversion studies

Saynisch, Jan; Irrgang, Christopher; Thomas, Maik

doi:https://doi.org/10.5194/angeo-36-1009-2018

Articles | Volume 36, issue 4

https://doi.org/10.5194/angeo-36-1009-2018

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

Special issue:

Dynamics and interaction of processes in the Earth and its...

https://doi.org/10.5194/angeo-36-1009-2018

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

Articles | Volume 36, issue 4

Regular paper

|

17 Jul 2018

Regular paper |

| 17 Jul 2018

Estimating ocean tide model uncertainties for electromagnetic inversion studies

Jan Saynisch, Christopher Irrgang, and Maik Thomas

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Final revised paper (published on 17 Jul 2018)
Preprint (discussion started on 13 Apr 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Referee Comments', Jakub Velimsky, 16 May 2018
- AC1: 'Authors response', Jan Saynisch, 20 Jun 2018
- AC3: 'Updated manuscript', Jan Saynisch, 20 Jun 2018
RC2: 'Motional Induction', R. TYLER, 01 Jun 2018
- RC3: 'Typo in Tyler Review', R. TYLER, 01 Jun 2018
  - AC2: 'Authors response', Jan Saynisch, 20 Jun 2018
- AC2: 'Authors response', Jan Saynisch, 20 Jun 2018
- AC4: 'Updated Manuscript', Jan Saynisch, 20 Jun 2018

Peer-review completion

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

ED: Publish as is (09 Jul 2018) by Alexey Kuvshinov

AR by Jan Saynisch-Wagner on behalf of the Authors (09 Jul 2018)

Short summary

By induction, ocean tides generate electromagnetic signals. Since the launch of magnetometer satellite missions, these signals are increasingly used to infer electromagnetic properties of the Earth. In many of these inversions, ocean tide models are used to estimate oceanic tidal electromagnetic signals which are generated via electromagnetic induction. This study's goal is to provide tide model errors for electromagnetic inversion studies.