Articles | Volume 18, issue 6
https://doi.org/10.5194/os-18-1573-2022
https://doi.org/10.5194/os-18-1573-2022
Research article
 | 
01 Nov 2022
Research article |  | 01 Nov 2022

A numerical study of near-inertial motions in the Mid-Atlantic Bight area induced by Hurricane Irene (2011)

Peida Han and Xiping Yu

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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-2022-635', Anonymous Referee #1, 15 Aug 2022
  • RC2: 'Comment on egusphere-2022-635', Anonymous Referee #2, 18 Aug 2022
  • EC1: 'Comment on egusphere-2022-635', Karen J. Heywood, 13 Sep 2022
    • AC5: 'Reply on EC1', Xiping Yu, 14 Sep 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Xiping Yu on behalf of the Authors (14 Sep 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (25 Sep 2022) by Karen J. Heywood
AR by Xiping Yu on behalf of the Authors (05 Oct 2022)  Author's response   Author's tracked changes 
EF by Polina Shvedko (06 Oct 2022)  Manuscript 
ED: Publish as is (09 Oct 2022) by Karen J. Heywood
AR by Xiping Yu on behalf of the Authors (10 Oct 2022)
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Short summary
Hurricane Irene generated strong near-inertial currents in ocean waters when passing over the Mid-Atlantic Bight of the US East Coast in late August 2011. It is demonstrated that a combination of valuable field data and detailed model results can be exploited to study the development and decay mechanism of this event. The near-inertial kinetic energy is shown to mainly have been gained from wind power during the hurricane event. Its decay, however, depends on several factors.