Articles | Volume 15, issue 6
https://doi.org/10.5194/os-15-1593-2019
https://doi.org/10.5194/os-15-1593-2019
Research article
 | 
03 Dec 2019
Research article |  | 03 Dec 2019

Commonly used methods fail to detect known propagation speeds of simulated signals from time–longitude (Hovmöller) diagrams

Yair De-Leon and Nathan Paldor

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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 Nathan Paldor on behalf of the Authors (29 Jul 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (01 Aug 2019) by John M. Huthnance
RR by Anonymous Referee #2 (16 Aug 2019)
RR by Anonymous Referee #3 (17 Sep 2019)
ED: Reconsider after major revisions (19 Sep 2019) by John M. Huthnance
AR by Nathan Paldor on behalf of the Authors (10 Oct 2019)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (14 Oct 2019) by John M. Huthnance
AR by Nathan Paldor on behalf of the Authors (06 Nov 2019)  Author's response    Manuscript
ED: Publish as is (12 Nov 2019) by John M. Huthnance
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Short summary
Using simulated signal of sea surface height anomalies (SSHA) where the phase speed of the dominant mode is known a priori, we demonstrate that four of the common methods employed in estimating the propagation speed of SSHA do not identify the correct input mode. This finding explains the lack of progress made in recent years in bridging the gap between the "too fast" Rossby wave phase speed observations by satellites and the phase speed in the highly accurate linear trapped wave theory.