Bruhl et al.: “Radiative forcing and stratospheric ozone changes due to major forest fires and recent volcanic eruptions including Hunga Tonga” Uses the EMAC model to investigate recent extreme stratospheric events. i.e., The 2019/2020 Australian wildfires and the Hunga volcanic event. There results add to the growing body of literature by reproducing the wildfire HCl solubility theory and by simulating Hunga effects with a different model (reproducing results is valid and important contribution to the literature). However, the paper suffers from a lack of an appropriate literature review, especially regarding science around Hunga and its effect on ozone loss. The authors also need to discuss how their work falls within the existing literature within the discussion of their results. For example, do their results agree with Solomon et al. (2023) that proposed enhanced HCl solubility in wildfire smoke? How do their Hunga ozone depletion agree/disagree with other studies on Hunga and ozone. The papers description of simulations performed and how figure results are presented also needs to updated to make the results and conclusions of the paper easier to understand. Overall, the paper fits ACP’s scope and would be a good contribution to the literature, but it currently needs major revisions. Please see below for details.

Major comments

The author’s need to do a proper literature review regarding Hunga in particular. I know you mention Santee et al., (2024) and direct readers there for other studies, but you are modelling Hunga impacts, so please provide a proper literature review here and later on discuss your results in the context of these references and their conclusions. Same needs to be done when discussing the wildfire results. Some other studies are linked below. Wilmouth, D. M., Østerstrøm, F. F., Smith, J. B., Anderson, J. G., and Salawitch, R. J.: Impact of the Hunga Tonga volcanic eruption on stratospheric composition, Proc. Natl. Acad. Sci. U.S.A., 120, e2301994120, https://doi.org/10.1073/pnas.2301994120, 2023. An important study looking at gas phase changes due to Hunga.

• • Wohltmann, I., Santee, M. L., Manney, G. L., and Millán, L. F.: The Chemical Effect of Increased Water Vapor From the Hunga Tonga‐Hunga Ha’apai Eruption on the Antarctic Ozone Hole, Geophysical Research Letters, 51, e2023GL106980, https://doi.org/10.1029/2023GL106980, 2024. A modelling study looking at 2023 and Hunga in the Antarctic.
  • Zhou, X., Dhomse, S. S., Feng, W., Mann, G., Heddell, S., Pumphrey, H., Kerridge, B. J., Latter, B., Siddans, R., Ventress, L., Querel, R., Smale, P., Asher, E., Hall, E. G., Bekki, S., and Chipperfield, M. P.: Antarctic Vortex Dehydration in 2023 as a Substantial Removal Pathway for Hunga Tonga‐Hunga Ha’apai Water Vapor, Geophysical Research Letters, 51, https://doi.org/10.1029/2023gl107630, 2024. A study on the Antarctic being a dehydration pathway for Hunga H2O. Also models at Antarctic ozone changes due to Hunga.
  • Manney, G. L., Santee, M. L., Lambert, A., Millán, L. F., Minschwaner, K., Werner, F., Lawrence, Z. D., Read, W. G., Livesey, N. J., and Wang, T.: Siege in the Southern Stratosphere: Hunga Tonga‐Hunga Ha’apai Water Vapor Excluded From the 2022 Antarctic Polar Vortex, Geophysical Research Letters, 50, e2023GL103855, https://doi.org/10.1029/2023GL103855, 2023. An observational study on how Hunga H2O was excluded from the 2022 vortex.
  • Schoeberl, M. R., Wang, Y., Ueyama, R., Taha, G., Jensen, E., and Yu, W.: Analysis and Impact of the Hunga Tonga‐Hunga Ha’apai Stratospheric Water Vapor Plume, Geophysical Research Letters, 49, https://doi.org/10.1029/2022gl100248, 2022. Looks at the radiative impact.
  • Fleming, E. L., Newman, P. A., Liang, Q., and Oman, L. D.: Stratospheric Temperature and Ozone Impacts of the Hunga Tonga‐Hunga Ha’apai Water Vapor Injection, JGR Atmospheres, 129, e2023JD039298, https://doi.org/10.1029/2023JD039298, 2024. A modelling study that includes the Antarctic ozone response of Hunga.
  • Krzysztof Wargan, Gloria L Manney, Nathaniel J Livesey. Factors contributing to the unusually low Antarctic springtime ozone in 2020-2023. ESS Open Archive . February 12, 2025. DOI: 10.22541/essoar.173940272.21623654/v1 (preprint). This is a preprint but could give some good insights.

Regarding modelling HCl solubility, the authors are using the methodology of Solomon et al., (2023) and therefore need to make sure they mention that their results are agreeing/confirming (or not) with that study, but with a different model.

I find the description of the simulations in section 2.1 and 3 very confusing. You mention, in multiple instances, simulations where you co-inject SO₂. A lot of times I interpreted the co-injection as a sensitivity simulation, but how does this differ from what actually happened? For example on line 138 you mention an experiment with co-injection. Is the only difference between this run and the normal Hunga run an extra 100 Kt of SO2? Was the normal hunga run also have co-injected H2O and SO2?  These sections need to be made clearer, with each distinct simulation having a title. It would make things even clearer if the titles of the different simulations were included in a legend in the figures. A table that shows the different simulations with what is and isn’t included would also be welcome.

A lot of the results presented in the figures are hard to distinguish. A lot of times there is just too much going on in each figure and combined with a lack of legends can make it hard to process without having to continuously read the caption to understand what each line represents. I suggest including legends and expanding some of the figures into more panels. For example, Figure 4 can be a 4 panel figure separating HCl and ClO. That way readers could actually distinguish ClO. Figures also need axis labels and panel letters.

I find it hard to distinguish how large/significant the wildfire or Hunga induced anomalies from your experiments are compared to your control without also presenting an MLS baseline and variability. A major concern I have is your model’s timing of ~August HCl recovery in the polar region in 2020-2023. In 2019, HCl in your model control simulation recovers similarly to MLS, but in 2020, HCl in your control and experiments seem to recover almost a month later than MLS. This will give an extra month (September) where you will likely have enhanced activated chlorine due to enhanced het. chem than what is likely occurring in MLS and therefore you may be overestimating your ozone loss. If HCl in your experiments recover later than your control it would be different, but they are recovering at the same time, and the timing does not agree with MLS. This needs to be addressed by comparing with MLS HCl climatology and investigated if it is a dynamical or chemical issue in your simulations.

Specific comments

Line 2: The author’s state “Similar to major volcanic eruptions”. Dynamically similar, sure. But, chemically it seems to be quite different.

Line 2-5: Please change: “Using the chemistry climate model EMAC, we demonstrate that organic carbon emitted from forest fires, injected into the stratosphere through pyro-cumulonimbi, enhances heterogeneous chlorine activation due to increased solubility of HCl in particles containing organic acids and an augmented aerosol surface area”. To “Using the chemistry climate model EMAC, we demonstrate that organic carbon emitted from forest fires, injected into the stratosphere through pyro-cumulonimbi, enhances heterogeneous chlorine activation due to increased solubility of HCl in particles containing organic acids and an augmented aerosol surface area, in agreement with existing literature.” It is great that you are confirming previous results with a different model, but isn't a novel conclusion.

Line 8 and other instances: I believe the current accepted naming is just “Hunga”. Please check and update throughout the paper.

Line 9: “The water vapour injection from the volcano altered only the vertical distribution of ozone loss.” As opposed to what? Latitudinal? A restructuring of the vertical profile? I don’t see presentation of these results anywhere apart from a mention in the conclusions.

Line 17: “There are some other references you should consider mentioning here regarding dynamics” Yu et al. (2019); Damany-Pearce et al., (2023)

• Yu, P., Toon, O. B., Bardeen, C. G., Zhu, Y., Rosenlof, K. H., Portmann, R. W., Thornberry, T. D., Gao, R.-S., Davis, S. M., Wolf, E. T., De Gouw, J., Peterson, D. A., Fromm, M. D., and Robock, A.: Black carbon lofts wildfire smoke high into the stratosphere to form a persistent plume, Science, 365, 587–590, https://doi.org/10.1126/science.aax1748, 2019.
• Damany-Pearce, L., Johnson, B., Wells, A., Osborne, M., Allan, J., Belcher, C., Jones, A., and Haywood, J.: Australian wildfires cause the largest stratospheric warming since Pinatubo and extends the lifetime of the Antarctic ozone hole, Scientific Reports, 12, 1–15, https://doi.org/10.1038/s41598-022-15794-3, 2022.

Line 18: “More important references regarding wildfire chemistry” Stone et al., (2025); Solomon et al., (2022)

• Stone, K., Solomon, S., Yu, P., Murphy, D. M., Kinnison, D., and Guan, J.: Two-years of stratospheric chemistry perturbations from the 2019/2020 Australian wildfire smoke, Atmos. Chem. Phys., 25, 7683–7697, https://doi.org/10.5194/acp-25-7683-2025, 2025.
• Solomon, S., Dube, K., Stone, K., Yu, P., Kinnison, D., Toon, O. B., Strahan, S. E., Rosenlof, K. H., Portmann, R., Davis, S., Randel, W., Bernath, P., Boone, C., Bardeen, C. G., Bourassa, A., Zawada, D., and Degenstein, D.: On the stratospheric chemistry of midlatitude wildfire smoke, Proceedings of the National Academy of Sciences of the United States of America, 119, 1–9, https://doi.org/10.1073/pnas.2117325119, 2022.

Line 20: The authors state: “This holds for the Australian fires in December 2019 to January 2020 as well as Canadian fires in 2017” Are you referring to chemistry here? Because there is no direct evidence (only correlation) that 2017 and 2019 Northern Hemisphere wildfires affected chemistry. If you are referring to dynamics please adjust this sentence to be clearer.

Line 29: The author’s are referencing a news article (Cutts). Please reference the actual papers. In this case it looks like Ansmann et al., 2023 and Solomon et al., 2023 that you have already reference elsewhere in the paper.

Line 46: What does “Slightly nudged mean?” Please define exactly how the QBO is nudged.

Line 55. What are the reactions that are included in the model?

Line 60. If Kohl et al continues to 2023, when does the previous Shallock et al., dataset end?

Figure 1 caption: What is GloSSAC? Is it an observational dataset? A model? It isn’t defined anywhere just mentioned again on lines 119 and 130

Line 123-124: The author’s state “In April 2023 there appears to be a southern midlatitude

volcanic event missing in our inventory or the Hunga Tonga SO2 injection is underestimated.” What do you mean there appears to be? If you think there is an event missing in your dataset, please check it, and then either correct it or definitively state that it is missing. Also, why would an underestimation of the Hunga SO2 injection affect April 2023 values, a year after the eruption, but not earlier? Your model aerosols e-folding time could be incorrect too.

Line 124-125: The author’s state: “Also in April 2023 some source of aerosol is missing in the tropics” I can't see this. It looks like you are overestimating SAD in the tropics compared to OSIRIS after April 2023. Please check.

Line 144-145: “Hunga Tonga causes a heating rate by up to 0.025 K/d at 25 km in the tropics and 0.011 K/d in southern midlatitudes.” How does this compare to the current literature? Also in agreement with Yu et al. and other studies?

Figure 5. Please be consistent in naming ClONO2. Figure 5 panel title uses ClNO3.

Line 165-167. Please discuss in context of existing literature (Solomon et al., 2023; Stone et al., 2025; Ma et al., 2024). If you are confirming results from Solomon et al., (2023) (but with a different model) please put that in your discussion.

Line 177-178: “and almost complete loss at the edge of the ozone hole in winter 2020 in agreement with MLS (black, red and green curves).” The ozone loss seen in the control run in the polar region looks comparable to MLS if you consider the offset in your model here. With this offset it is hard to see if your control run or your experiment better represent the observations.

Line 180-184: Do you have simulations with combined dynamical and chemistry effects? Or are they separate? Again, it is hard to understand exactly what is happening in each simulation based on your descriptions.

Line 184: “The loss due to the eruption of Hunga Tonga is up to about 15 DU in 2022 and 2023 (Fig. 8b).” Where? Midlatitudes? Polar region? How does this compare to existing literature?

Line 192-193: “To obtain agreement with the chlorine activation in polar regions observed by MLS it is essential to include the enhanced solubility of HCl in particles containing organic acids from major forest fires.” Please add in a statement like “In agreement with Solomon et al., (2023)” or something similar.

Line 197-198: “Hunga Tonga water vapour had only a small effect on ozone and radiative forcing.” Is this discussed anywhere in the paper? I can’t find it, but apologies if I missed it. If it is not discussed please add it in and also please compare to existing literature. For example: Zhang et al., 2024 shows ozone decreases in the midlatitudes due to the diluting of aerosols increasing the HOBr +HCl reaction. Wilmouth et al., 2023 also shows gas phase ozone loss in the midlatitudes due to elevated OH from the injected water vapor? How do your results compare with these and other papers?

Line 199-: “Co-injection of SO2 and H2O leads to features not observed since it almost prevents the descent of the H2O plume by radiative cooling in the early phase due to heating of the sulfur aerosol which is formed too rapidly, related to strongly enhanced OH, which leads to a too late arrival of the additional water vapour in the lower stratosphere at mid and high southern latitudes.” Again, I am confused my co-injected is presented like a sensitivity study. Is it not what actually happened? Or does co-injection mean at the same altitude?

Line 204: “causes a change in the vertical distribution with almost no effect on total ozone,” Where is this discussed/presented in the paper?

Technical corrections

Line 30. Change "Since decades" to “In decades”

There are a lot of undefined acronyms throughout the paper. Please define acronym’s when they first appear. For example, EMAC is not defined were it first appears on line 34. ECHAM5 on line 43, GMXE, EQSAM, MSBM etc.

Line 43: MESSy is spelled out, therefore please but in brackets.

Line 44: I believe ERA5 is typically not hyphenated.

Line 54: “PSC”

Line 62. Suggest changing “Including several hundreds of explosive” to “Including several hundred explosive”.

Line 109-110: Please reword: “optical depth (SAOD) for tropics and southern and northern midlatitudes is” to “optical depth (SAOD) for the tropics, the southern midlatitudes, and the northern midlatitudes” or something similar.

Line 110-111: I believe you want a comma after this sentence instead of a period“1. Considering the organic aerosol from major forest fires is essential for agreement with the observations by OSIRIS.”

Line 174. Do you mean H2O or are you referring to Figure A3?

Line 195: is it 28 DU or 30 DU as mentioned earlier?

Line 197: “up to 15 DU…” where is this occurring? Midlatitudes? Polar region?

This manuscript presents findings from interactive stratospheric aerosol and chemistry simulations with a 3D composition climate model, to quantify the radiative and chemical effects on the stratosphere from recent intense wildfires and explosive volcanic eruptions.

The January 2022 Hunga eruption is found to cause a modest depletion of the stratospheric ozone layer throughout the 2022 Southern Hemisphere, with also the intense wildfires from Australia (Dec 2019) and Canada (NH summer 2019 and 2020) causing additional ozone loss in 2019 and 2020.

These impacts are found to be caused primarily by stratospheric aerosol particles from these sources, and although the emission of water vapour from Hunga is found to have altered the vertical location of the aerosol and caused some PSC-driven impacts, the direct effects from the emitted water vapour are smaller than these indirect effects.

The scientific writing style is generally quite good, and the findings presented are generally well-described and summarised.  However, two of the initial Figures within the paper need to be revised, to give a clearer presentation of the stratospheric AOD and SAD enhancements after Hunga.  

Specifically, Figure 1 gives the impression that the forest fires caused larger global stratospheric AOD enhancement, which is not the case. 

The magnitude of the observed global stratospheric AOD in 2022 summer has been established (Khaykin et al., 2022; Legras et al., 2022;  Knepp et al., 2024; Joerimann et al., 2025) to have been substantially higher in 2022 than in 2020 and 2021 (indeed 2022 had the highest since the Pinatubo aerosol in 1992), and this can be seen clearly for example within Figure 10c of Khaykin et al. (2022).

There is a similar issue with Figure 3, with the 2019-2023 variation in SAD shown only at 1 altitude level (68hPa), this being in the lowermost stratosphere, the altitude at which the wildfires emitted, but ~5-10km below the altitude of the Hunga aerosol.

Figures 18 and 19 of Knepp et al. (2024) show clearly that the Hunga aerosol was present at a higher altitude, much deeper into the stratosphere (20-30km; ~30-50hPa), and the 68 hPa level selected for the SAD comparison (Figure 3 upper-panel and lower-panel).

The submitted manuscript then presents readers with an incorrect impression that the 2022 Hunga SAD-enhancement was lower than that from the 2019-2020 wildfires, when it’s simply that the stronger Hunga aerosol was at higher altitude than the level shown.

These are the  2 “main minor revisions”, that Figures 1 and 3 as currently drawn do not provide an adequate representation of the relative impacts on the stratosphere. Figure 3 shows only the impacts in the lowermost stratosphere (68 hPa), and Figure 1 gives stronger-looking lines to the more-uncertain limb-scatter instruments (OMPS-LP, OSIRIS) and weaker-looking dashed lines to the gold-standard SAGE-III aerosol measurements (these going off-the-scale on the plot).

The aerosol extinction derived from the OMPS-LP and OSIRIS limb-scatter instruments is known to be much more uncertain than SAGE-III, due primarily to having to make assumptions on particle size. In contrast, the SAGE-III instrument does not have to make an assumption about particle size, the solar occulation method measuring the extinction of sunlight directly.

In summary, Figure 1 needs to be re-drawn with a solid line used for the GloSSAC stratospheric AOD, this being the benchmark stratospheric AOD dataset (currently represented by a dotted line), and the current solid line used for OSIRIS changed to a dotted line.  The y-axis range also needs to be increased accordingly (see revision M-MR1 below).  And Figure 3 needs to show an integrated

I note however these are entirely presentational issue, and the required revisions remain at a minor level, and it will I expect be a relatively quick job to amend the Figures for this change.

Overall the paper presents a very interesting quantification of the relative magnitude of the effects, and the later Figures do compare like-for-like with the radiative forcing, albeit those based on this particular model’s predictions.   

And then I am recommending minor revisions overall, referring to these Figure changes as the only two “main minor revisions” (M-MR1, M-MR2), these listed below with the specific info on the modifications needed for these 2 Figures.  There may need also to be some changes  tothe associated interpretation, the Hunga impacts to be given more prominence than currently, the 2022 enhancement to the stratospheric AOD clearly substantially larger than that from the wildfires in 2019-2021.

Whilst the model predictions of the ozone layer and radiative impacts may indicate a stronger effect from the fires,  this is a model result, and I am aware from a current Hunga aerosol intercomparison (Aquila et al., in prep.) that the EMAC predicted Hunga aerosol is weaker than in other models.

The manuscript can of course present the model findings, but the model being low-biased compared to the main Hunga enhancement in 2022 (compared to the benchmark SAGE-III/GloSSAC observations) needs to be noted as a significant caveat in the interpretation.

With the current administration of the US, the SAGE-III instrument may well be ended prematurely,  and then model-observation comparisons in the future may have to rely more exclusively on the limb-scatter instruments. The large difference between the OSIRIS limb scatter stratospheric AOD retrievals, and that from the benchmark GloSSAC/SAGE-III solar occultation, during the Hunga period, illustrates the importance of retaining SAGE-III.

Figure 3 needs to be re-drawn to show impacts comparing vertically-integrated stratospheric column-SAD, then inclusive of both impacts, and providing readers of the article with a balanced representation of stratospheric variations through the 2019-2023 period.

The 3^rd main minor revision relates to the axis-label presentation of the Figures being quite poor, the y-axis values in Figure 1 given simply as log10 of the stratospheric AOD, and there being no y-axis labels for the reader to appreciate what quantity is shown there.

Again, these presentational issues are relatively easy to correct.  And whilst this is somewhat disappointing that the authors should have submitted an article that seems not yet ready for expert peer review, I am aware of the APARC Hunga impacts report has a deadline of 31^st July for papers to be citable, and may have affected the authors decision to submit prematurely.

It is also understandable, though somewhat regrettable, that a time-pressed Topical Editor (TE) was not able to flag these basic axis-label issues within an initial TE review.

Overall this is a solid paper, and the article is certainly within scope for ACP, and the findings presented are important, and will be of substantial interest to the community, once the revised manuscript can adequately represent the stratosphere’s variation through this period.  

The scientific writing is generally quite good, and although the writing style is quite brief, the main results are presented in a fair way, aside from the initial Figures 1 and 3.  

Main minor revisions

M-MR-1) Re-plot Figure 1 with solid black line for GloSSAC (benchmark for stratospheric AOD)



As noted in the general comments above, please switch-round the dotted and solid lines given currently for the stratospheric AOD for GloSSAC and OSIRIS.

This is needed because the OSIRIS is a limb-scatter instrument, then much less certain aerosol retrieval than for the SAGE-III instrument, providing the main basis of GloSSAC.

The colour black should also be reserved for observations, and please also use then change the model lines to be coloured green, with black used for the observation datasets.

Please also update the y-axis range, to include the peak post-Hunga GloSSAC sAOD values.

The GloSSAC observed stratospheric AOD “off the scale” during 2022, in the lower-panel of the current version of Figure 1 (for southern hemisphere stratospheric AOD).

M-MR-2) The current Figure 3 needs to be re-drawn for vertically-integrated SAD, to include the main Hunga impacts being at higher altitude than those from the 2019/2020 wildfires.

This is particularly evident within Figure 3, the Surface Area Density shown only for 1 selected altitude (68hPa).  It is clear when referring to Figures 18 and 19 from Knepp et al. (2024) or Figure 7a from Joerimann et al. (2025) that the observed post-Hunga SAD is significantly higher in magnitude than the wildfires (and also at higher altitude).

Had a 50hPa or 30hPa level been chosen for this southern mid-latitude comparison (the upper panel of Figure 3) the reader would have been presented with a timeline showing only a very minor enhancement in 2020 and 2021, and a much larger enhancement in 2022 (see Knepp et al., 2024, Figure 19).

Other minor revisions

O-MR-1) Abstract, line 1 – It’s important to be clear the causality requires a conditional clause. Please insert “can” before “affect stratospheric chemistry” (it’s only the exceptionally intense wildfires in 2019/2020 that have been shown to have this effect).

O-MR-2) Abstract, line 3 – Similarly to above, the Abstract needs to be clear it is these particular wildfires that are shown to have this effect (the majority of wildfires do not have this effect).   Change “emitted from wildfires” to “emitted from intense wildfires in 2019/2020”.

O-MR-3) Abstract, line 4 – Change “due to increased solubility of HCl in particles containing organic acids”  -- the “due to” is not quite right there – it’s the abundance of the smoke in the stratosphere that causes the effect (from the intense fires).  Suggested re-wording is “related to a high solubility of HCl in aerosol particles containing organic acids”. 

O-MR-4) Abstract, line 5 – Change “the upward transport of the pollution plumes resulted in”.

The “upward transport” could be misunderstood by some readers to mean a longer timescale effect. But it was actually the extreme intensity of the fire, that  then caused a very deep plume, to then detrain the smoke at altitudes above the tropopause.   

Suggested re-wording is to change

“Following the 2019/2020 Australian megfires, the upward transport of the pollution plumes resulted in ozone depletion in the…” to

“The extreme intensity of the 2019/2020 Australian wildfires, meant the smoke plume reached the stratosphere, causing in significant ozone depletion in the…”

O-MR-5) Abstract, line 6 – Please change “It diminished column ozone” – the preceding sentence already stated there was significant ozone depletion, and this “It diminished” phrasing also needs to be improved for peer-reviewed article. 

Suggest to change

“It diminished column ozone in the following two years…”

to

“With the long residence time in the stratosphere, the wildfire smoke diminished column ozone for the following two years….

O-MR-6) Introduction, line 16 – Re-word “Since about 2017 it was observed…”.  This is the 1^st sentence of the Introduction, and the “about” is really quite poor wording there.   Suggest to adapt the sentence, and cite Mike Fromm’s earlier papers (e.g. Fromm et al., 2004, 2005) which pointed out these effects from intense boreal forest fires.

O-MR-7) Introduction, lines 19-20 – “This holds for the Australian wildfires” – not clear what was meant here.

O-MR-8) Introduction, line 24 – Re-word sentence – improve “like for example Hunga Tonga” for scientific language.

O-MR-9) Introduction, line 25 – Similarly, the tense here is not quite right, change “lifting” to “lifted”.

O-MR-10) Introduction, line 28 – Again, improve the scientific writing here, re-word “This and the about 10km thick layer” to be more precise.  This is also the first time the depth of the smoke aerosol is mentioned, and suggest to hint at the timescale being significant prior to becoming this 10km deep, e.g. maybe “The initial layer of smoke aerosol progressed to a 10km depth enhancement …..” or similar.

O-MR-11) Introduction, line 30 – Scientific writing poor here also – “has been analyzed in several studies” – please be clear what type of studies these are – presumably it was meant the observational studies in the initial period after the eruption?  If you meant modelling studies, be clear if you mean interactive stratospheric aerosol studies -- and there’s actually been relatively few of these – the study of Zhu et al. (2022) and Li et al. (2024)

O-MR-12) Line 40, heading for section 2 – the “and used satellite data” is not great.  And suggest to include the words “interactive aerosol” to be clear these are interactive stratospheric aerosol CCM simulations.    Suggest to change to:

“Interactive chemistry-climate model simulations and satellite measurement datasets”

O-MR-13) Section 2.1 -- Line 42 – It seems too abrupt to simply begin “EMAC consists of” – and I think the acronym has not yet been introduced.  Suggest to re-word to:

“For this study, we analyse interactive stratospheric aerosol simulations with the ECHAM/MESSY Atmospheric Chemistry model (EMAC)…”.

O-MR-14) Line 44 – put “up to 100 hPa” in brackets here, i.e. “(up to 100 hPa)”.

O-MR-15) Line 54 – Re-word “accelerating the classical PCS reactions for chlorine activation also in mid-latitudes”.  I think you meant that the presence of the extra aerosol means there’s substantial additional heterogeneous chemistry occurring in mid-latitude, adding to that on the PSCs at high latitudes.  Please re-word to better explain what you meant here.

O-MR-16) Line 80 – Section 2.2 heading – change “OSIRIS” to “OSIRIS aerosol extinction”.

O-MR-17) Line 89 – Section 2.3 heading – change “OMPS-LP” to “OMPS-LP aerosol extinction”.

O-MR-18) Line 99 – Section 2.4 heading: change “AURA-MLS” to “Aura-MLS trace gas retrievals”

O-MR-19) Lines 105-107 – Please specify which species you are using to evaluate the model here.

O-MR-20) Caption to Figures 1, 2 and 3– The captions to these Figures notes 500 kt SO2 in the red-line sensitivity simulation, but this is difficult for a time-pressed reader to interpret.   Please add “All simulations other than the no-Hunga or 500 kt Hunga run apply 400 kt of SO2.

References

Fromm et al. (2004) “New directions: Eruptive transport to the stratosphere: Add fire-convection to volcanoes”, Atmos. Environ., vol. 38, 163-165.

Fromm et al. (2005) “Pyro-cumulus injection of smoke to the stratosphere: Observations and impact of a super blow-up in northwestern Canada on 3-4 August 1998”, J. Geophys. Res., 110, https://doi.org/10.1029/2004JD005350

Joerimann, A., Sukhodolov, T., Luo, B. et al. (2025), “A REtrieval Method for optical and physical Aerosol Properties in the stratosphere (REMAPv1)”,  in review, in Geosci. Mod. Dev.,

https://doi.org/10.5194/egusphere-2025-145

Khaykin, S., Podklajen, A., Ploeger, F. et al. (2022), “Global perturbation of stratospheric water and aerosol burden by Hunga eruption” , Comm. Earth Env.,

https://doi.org/10.1038/s43247-022-00652-x

Knepp, T., Kovilakam, M., Thomason, L. et al. (2024), “Characterization of stratospheric particle size distribution uncertainties using SAGE II and SAGE III/ISS extinction spectra”, Atmos. Meas. Tech., 17, 2025–2054, 2024, https://doi.org/10.5194/amt-17-2025-2024

Li, C., Peng, Y, E. Asher et al. (2024) “Microphysical simulations of the 2022 Hunga volcano eruption using a sectional aerosol model”, Geophys. Res. Lett., vol. 51, issue 11.,

https://doi.org/10.1029/2024GL108522

Zhu, Y., Bardeen, C., Tilmes, S. et al. (2022) “Perturbations in stratospheric aerosol evolution due to the water-rich plume of the 2022 Hunga-Tonga eruption”, Comms. Earth Env., 3, 248

https://doi.org/10.1038/s43247-022-00580-w