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BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3511–3543, 2020
https://doi.org/10.5194/bg-17-3511-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 17, 3511–3543, 2020
https://doi.org/10.5194/bg-17-3511-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 08 Jul 2020

Research article | 08 Jul 2020

N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions

Fortunat Joos et al.

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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 (05 Jul 2019) by Sönke Zaehle
AR by Fortunat Joos on behalf of the Authors (16 Jul 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Sep 2019) by Sönke Zaehle
RR by Anonymous Referee #2 (12 Sep 2019)
RR by Anonymous Referee #1 (21 Oct 2019)
ED: Reject (26 Nov 2019) by Sönke Zaehle
ED: Reconsider after major revisions (20 Jan 2020) by Martin De Kauwe
AR by Fortunat Joos on behalf of the Authors (22 Jan 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Jan 2020) by Martin De Kauwe
RR by Anonymous Referee #1 (27 Feb 2020)
RR by Anonymous Referee #3 (29 Apr 2020)
ED: Publish subject to minor revisions (review by editor) (30 Apr 2020) by Martin De Kauwe
AR by Fortunat Joos on behalf of the Authors (11 May 2020)  Author's response    Manuscript
ED: Publish as is (20 May 2020) by Martin De Kauwe
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Short summary
Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N) cycling and N2O emissions over the past 21 000 years are compared with reconstructed N2O emissions. Modelled and reconstructed emissions increased strongly during past abrupt warming events. This evidence appears consistent with a dynamic response of biological N fixation to increasing N demand by ecosystems, thereby reducing N limitation of plant productivity and supporting a land sink for atmospheric CO2.
Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N)...
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