Articles | Volume 25, issue 15
https://doi.org/10.5194/acp-25-8929-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Contributions of lightning to long-term trends and inter-annual variability in global atmospheric chemistry constrained by Schumann resonance observations
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- Final revised paper (published on 14 Aug 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 10 Mar 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2025-370', Anonymous Referee #1, 26 Mar 2025
- AC1: 'Reply on RC1', Yuzhong Zhang, 14 May 2025
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RC2: 'Comment on egusphere-2025-370', Anonymous Referee #2, 18 Apr 2025
- AC2: 'Reply on RC2', Yuzhong Zhang, 14 May 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Yuzhong Zhang on behalf of the Authors (14 May 2025)
Author's response
Author's tracked changes
EF by Katja Gänger (15 May 2025)
Manuscript
EF by Katja Gänger (15 May 2025)
Supplement
ED: Publish as is (26 May 2025) by Christopher Cantrell
AR by Yuzhong Zhang on behalf of the Authors (28 May 2025)
This is an excellent paper scientifically and is also very well written. The authors use observations of the Schumann Resonance to modify the existing lightning parameterization in the GEOS-Chem model. The existing Price and Rind cloud-top height prediction scheme for flash rate, as modified by Murray et al. based on satellite lightning observations, produced an increase in flash rates over the 2013 to 2021 period. Correcting the parameterization using the Schumann Resonance yielded no significant trend, which is in line with observations. The authors used the revised scheme in GEOS-Chem simulations for the period, examining the effects of the change in lighntning scheme on NOx, O3, and OH. The updated scheme does better at producing interannual variability in these species. The authors also examine the effects of a 10% decrease in lightining in 2020 on methane growth as a result of the decreased OH. I have some suggestions for minor changes. Once they are attended to, the paper should be ready for acceptance.
Details:
lines 121-125: It would be worth noting that also the results of Allen et al. (2019, JGR) and Bucsela et al. (2019, JGR) from use of OMI NO2, also found little difference in LNOx production per flash between midlatitudes and tropics.
Figures 2, 4, 5, 6, and 7: It is difficult to tell the gray and blue bars and lines apart. A different color is needed for one of them.
Figure 6: This figure needs better explanation. From this figure I don't see how the non-lightning contribution is a difference between the observationa and the model lightning contribution. For 2020, how do these bars imply a 54% contribution of lightning to the methane growth? Why is there a methane growth rate bar for 2021, but not the lighting and non-lightning bars?
lines 271-273: There is a significant amount of fire in South America during September to November. I think you should choose a different set of months (maybe December to February).
Figure 7 - cation: "green" should be "gray"