Articles | Volume 15, issue 21
https://doi.org/10.5194/bg-15-6747-2018
https://doi.org/10.5194/bg-15-6747-2018
Research article
 | 
13 Nov 2018
Research article |  | 13 Nov 2018

The effect of the 2013–2016 high temperature anomaly in the subarctic Northeast Pacific (the “Blob”) on net community production

Bo Yang, Steven R. Emerson, and M. Angelica Peña

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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
ED: Reconsider after major revisions (30 Sep 2018) by Koji Suzuki
AR by Bo Yang on behalf of the Authors (30 Sep 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (02 Oct 2018) by Koji Suzuki
RR by Anonymous Referee #2 (13 Oct 2018)
ED: Reconsider after major revisions (15 Oct 2018) by Koji Suzuki
AR by Bo Yang on behalf of the Authors (15 Oct 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (19 Oct 2018) by Koji Suzuki
RR by Anonymous Referee #2 (22 Oct 2018)
ED: Publish subject to technical corrections (01 Nov 2018) by Koji Suzuki
AR by Bo Yang on behalf of the Authors (01 Nov 2018)  Manuscript 
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Short summary
A large anomalously warm water patch appeared in the NE Pacific in winter 2013–14 and persisted through 2016. Its effect on biological carbon export was determined using O2 and dissolved inorganic carbon data from a profiling float and a surface mooring. Results show the carbon export decreased after the first year when warmer water invaded and then returned to the previous value, with a similar trend in phytoplankton abundance and corresponding changes in phytoplankton community composition.
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