Articles | Volume 19, issue 1
https://doi.org/10.5194/amt-19-185-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Quantifying agricultural N2O and CH4 emissions in the Netherlands using an airborne eddy covariance system
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- Final revised paper (published on 12 Jan 2026)
- Preprint (discussion started on 22 Jul 2025)
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-2025-3297', Anonymous Referee #1, 25 Aug 2025
- AC1: 'Reply on RC1', Paul Waldmann, 22 Oct 2025
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RC2: 'Comment on egusphere-2025-3297', Anonymous Referee #2, 03 Sep 2025
- AC2: 'Reply on RC2', Paul Waldmann, 22 Oct 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Paul Waldmann on behalf of the Authors (25 Nov 2025)
Author's response
Author's tracked changes
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ED: Publish as is (01 Dec 2025) by Glenn Wolfe
AR by Paul Waldmann on behalf of the Authors (15 Dec 2025)
Author's response
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The present study "Quantifying agricultural N2O and CH4 emissions in the Netherlands using an airborne eddy covariance system" describes in detail a measurement system and airborne eddy covariance method for quantifying CH4 and N2O fluxes over an agricultural region. The study is generally clearly presented and extremely detailed in methodology. Novel findings of N2O emissions from agriculture and comparison to inventories are also presented. The authors thoroughly consider uncertainties and potential biases in the measurements. I recommend publication following minor revisions.
Line 32: I believe the current IPCC recommendation for the GWP100 of biogenic CH4 is 27.
General comments/questions, largely for the purposes of improved clarity:
1: I assume that the choice of 90 s was at least partially made to capture all of the eddy scales based on ogives, analysis of the cospectral power, and/or integral timescale. I don't believe an explanation of this was explicitly given in the manuscript. It would be helpful to see in the text a description of what factors went into to choosing the 90 s windows.
2: I found it generally confusing what is meant by leg, vs Flight leg, vs flux segment. It would be useful if clear definitions were explicitly given and/or more consistency in the language were used. e.g. Do these terms always refer to the flight leg, or sometimes to the 90 s intervals as it seemed?
3. The authors mention that spatial homogeneity is required for eddy covariance, but the flux variations over a leg seem to indicate non-homogeneity. I would assume the condition of homogeneity is only necessary over the 90 s windows use for the flux calculations. Does the overlapping windows further loosen this condition? Some discussion of this in the text would be useful.
4. Are the LODs calculated for each 90 s segment (i.e. N represents the number of observations per 90 s flux interval)? If so, are these simply averaged over the flight? If, rather, N is the entire leg, wouldn't this calculation of LOD underestimate the ability of the instrumentation to distinguished spatially-resolved fluxes? In general I think more clarification is needed to contextualize the LODs reported.
5. It would be helpful to have a figure on the flux divergence calculation in the Appendix.
6. Authors mention recent studies utilizing the continuous wavelet transform method, which is often thought of as better for obtaining higher spatial resolution. Is there a reason that the authors used the moving window method instead?