Articles | Volume 10, issue 12
https://doi.org/10.5194/gmd-10-4723-2017
https://doi.org/10.5194/gmd-10-4723-2017
Model description paper
 | 
22 Dec 2017
Model description paper |  | 22 Dec 2017

231Pa and 230Th in the ocean model of the Community Earth System Model (CESM1.3)

Sifan Gu and Zhengyu Liu

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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 Sifan Gu on behalf of the Authors (11 Aug 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (23 Aug 2017) by Paul Halloran
RR by Anonymous Referee #3 (30 Aug 2017)
ED: Publish subject to minor revisions (Editor review) (09 Oct 2017) by Paul Halloran
AR by Sifan Gu on behalf of the Authors (19 Oct 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (25 Oct 2017) by Paul Halloran
AR by Sifan Gu on behalf of the Authors (27 Oct 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (06 Nov 2017) by Paul Halloran
AR by Sifan Gu on behalf of the Authors (10 Nov 2017)
ED: Publish as is (15 Nov 2017) by Paul Halloran
AR by Sifan Gu on behalf of the Authors (15 Nov 2017)  Manuscript 
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Short summary
Both biotic 231Pa and 230Th and abiotic 231Pa and 230Th have been implemented in the ocean model of CESM. Under present-day climate forcing, our model is able to simulate water column 231Pa and 230Th activity and the sediment 231Pa-to-230Th activity ratio in good agreement with observations. In HOSING experiments, the biotic and abiotic sediment 231Pa-to-230Th activity ratios behave similarly over large areas of low productivity, but can differ substantially in some regions of high productivity.