Articles | Volume 22, issue 24
https://doi.org/10.5194/bg-22-8031-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Dynamics and environmental drivers of methane and nitrous oxide fluxes at the soil and ecosystem levels in a wet tropical forest
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- Final revised paper (published on 16 Dec 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 07 Aug 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2025-3501', Anonymous Referee #1, 25 Aug 2025
- AC1: 'Reply on RC1', Laëtitia Brechet, 08 Oct 2025
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RC2: 'Comment on egusphere-2025-3501', Anonymous Referee #2, 26 Aug 2025
- AC2: 'Reply on RC2', Laëtitia Brechet, 08 Oct 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (review by editor) (24 Oct 2025) by Lutz Merbold
AR by Laëtitia Brechet on behalf of the Authors (07 Nov 2025)
Author's response
Author's tracked changes
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ED: Publish as is (22 Nov 2025) by Lutz Merbold
AR by Laëtitia Brechet on behalf of the Authors (29 Nov 2025)
Author's response
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Overall, this paper is a useful addition to the literature. Better characterizing greenhouse gas fluxes from tropical soils, and identifying drivers, is a timely and important research question. The combination of automated chambers and eddy-flux, especially for N2O, is very novel for tropical forests. Overall, given the well-known spatial and temporal heterogeneity of N2O fluxes even in much more homogenous ecosystems, I am not surprised that fluxes were not well explained by simple environmental variables, even with the data density of this paper. This is a dataset that will certainly be of interest to many people. Several of the methodological lessons learned (such as lack of storage of N2O and Ch4 under the canopy, revealed by vertical profile measurements) are also likely to be of use to other researchers.
I have one significant concern that I think merits serious consideration- the choice to exclude high fluxes from analysis (and indeed not to present them at all, making it very difficult to judge how important they might be). Specifically, the authors did not present (or include in analysis) any fluxes outside the 5th-95th percentile (per line 248), even after rigorous data cleaning steps that should have weeded out any anonymously high fluxes that were methodological artifacts. I realize that it is very difficult to scale rare, high fluxes without very good estimates of their probability. However, I do not thing that dismissing them entirely makes any sense, and no specific rationale or citation was given for the choice. Rare, very high N2O fluxes are not at all uncommon in tropical forests in my personal experience, but rarely do we have the data density (as we do here!) to judge their potential importance. These excluded fluxes- depending on their magnitude, could be potentially important for net ecosystem emissions, especially because they’re probably quite skewed- extreme production events could be somewhat common but extreme consumption events likely are not.
To summarize- I am not necessarily suggesting that all data needs to incorporated into scaling, but I would strongly suggest 1) presenting the relative magnitude of the excluded fluxes compared to the data that was included. Were they common and somewhat high? Or more rare and extremely high? 2) At least conducting some sort of sensitivity of means, medians etc to the inclusion or exclusion of these omitted values (including perhaps making a range of assumptions about their probability, in the case of very high outliers). I also would hazard, and add caveats, against comparisons with any other rate fluxes from tropical sites that may indeed have included hot spots and hot moments in their scaling efforts. Overall it seems counterintuitive to highlight the heterogeneity of soil GHG fluxes and then ignore a potential large fraction of the variation.
Finally, data should be posted in an accessible database online in keeping with the specifications of this journal (rather than ‘on request’).