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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 12 | Copyright
Geosci. Model Dev., 10, 4723-4742, 2017
https://doi.org/10.5194/gmd-10-4723-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

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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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
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 Anna Wenzel on behalf of the Authors (15 Nov 2017)  Author's response    Manuscript
ED: Publish as is (15 Nov 2017) by Paul Halloran
Publications Copernicus
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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.
Both biotic 231Pa and 230Th and abiotic 231Pa and 230Th have been implemented in the ocean model...
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