The nodal dependence of long-period ocean tides  in the Drake Passage

Woodworth, Philip L.; Hibbert, Angela

doi:https://doi.org/10.5194/os-14-711-2018

Articles | Volume 14, issue 4

https://doi.org/10.5194/os-14-711-2018

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

Special issue:

Developments in the science and history of tides (OS/ACP/HGSS/NPG/SE...

https://doi.org/10.5194/os-14-711-2018

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

Articles | Volume 14, issue 4

Research article

|

26 Jul 2018

Research article |

| 26 Jul 2018

The nodal dependence of long-period ocean tides in the Drake Passage

Philip L. Woodworth and Angela Hibbert

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Final revised paper (published on 26 Jul 2018)
Supplement to the final revised paper
Preprint (discussion started on 23 Apr 2018)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'referee comment', Anonymous Referee #1, 23 May 2018
- AC1: 'Replies to Reviewer 1', Philip Woodworth, 26 Jun 2018
RC2: 'Comments on 'The Nodal Dependence of Long-Period Ocean Tides in the Drake Passage'', Xiangbo Feng, 29 May 2018
- AC2: 'Replies to Reviewer 2', Philip Woodworth, 26 Jun 2018

Peer-review completion

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

AR by Philip Woodworth on behalf of the Authors (26 Jun 2018) Author's response Manuscript

ED: Publish as is (27 Jun 2018) by Mattias Green

Short summary

30 years of BPR data at Drake Passage are used to investigate the Mf, Mm and Mt long-period tides. Amplitudes of Mf and Mt, and all phase lags, vary over the nodal cycle as in the equilibrium tide. Mm amplitude is almost constant, and so inconsistent at 3σ from anticipation due to energetic non-tidal variability. Most findings agree with a modern ocean tide model. BPR records are superior to conventional tide gauge data in this work due to lower proportion of non-tidal variability.