Articles | Volume 14, issue 4
https://doi.org/10.5194/os-14-633-2018
https://doi.org/10.5194/os-14-633-2018
Research article
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11 Jul 2018
Research article | Highlight paper |  | 11 Jul 2018

On the role of the North Equatorial Counter Current during a strong El Niño

David John Webb

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by David Webb on behalf of the Authors (23 Apr 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Apr 2018) by Matthew Hecht
RR by Lauren Kuntz (08 May 2018)
RR by Anonymous Referee #3 (24 May 2018)
ED: Publish subject to minor revisions (review by editor) (29 May 2018) by Matthew Hecht
AR by David Webb on behalf of the Authors (02 Jun 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (22 Jun 2018) by Matthew Hecht
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Short summary
Results from a high-resolution ocean model show that during the strong El Niños of 1983 and 1998, transport of warm water in the equatorial Pacific was dominated by the North Equatorial Counter Current and not by equatorial Kelvin waves. The results show why the NECC fails to do this in most years and how stronger than normal annual Rossby waves near the Equator can both trigger the El Niño in the western Pacific and help to ensure that the warm water arrives off South America around Christmas.