Articles | Volume 26, issue 2
https://doi.org/10.5194/acp-26-1373-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Achieving consistency between in-situ and remotely sensed optical and microphysical properties of Arctic cirrus: the impact of far-infrared radiances
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- Final revised paper (published on 27 Jan 2026)
- Preprint (discussion started on 07 Aug 2025)
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-2025-3547', Anonymous Referee #1, 15 Sep 2025
- AC2: 'Reply on RC1', Gianluca Di Natale, 31 Oct 2025
- AC3: 'Reply on RC1', Gianluca Di Natale, 31 Oct 2025
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RC2: 'Comment on egusphere-2025-3547', Anonymous Referee #2, 15 Sep 2025
- AC1: 'Reply on RC2', Gianluca Di Natale, 31 Oct 2025
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AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Gianluca Di Natale on behalf of the Authors (14 Nov 2025)
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ED: Referee Nomination & Report Request started (14 Nov 2025) by Zhibo Zhang
RR by Anonymous Referee #1 (25 Nov 2025)
RR by Anonymous Referee #2 (22 Dec 2025)
ED: Publish subject to minor revisions (review by editor) (30 Dec 2025) by Zhibo Zhang
AR by Gianluca Di Natale on behalf of the Authors (02 Jan 2026)
Author's response
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ED: Publish as is (13 Jan 2026) by Zhibo Zhang
AR by Gianluca Di Natale on behalf of the Authors (16 Jan 2026)
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This paper describes an intercomparison of the properties of cirrus measured by in-situ probes vs those retrieved from a ground-based infrared spectrometer that spans from the mid-infrared to the far-infrared (i.e., from 1500 cm-1 to 400 cm-1). Th authors use a ceilometer to ascertain the base and top of the cirrus clouds, and to estimate their optical depth. Lastly, their infrared retrieval framework also retrieves thermodynamic profiles, which they compare against ERA5 model output and retrieved profiles from a collocated ground-based microwave radiometer.
The paper achieves what it sent out to do, namely, to perform an intercomparison of derived cirrus properties, which includes an evaluation of the assumption of the habit of the ice particles, and thermodynamic profiles. It is well written, and the references included are sufficient.
My main concern is that this intercomparison evaluate 11 samples that were collected within a 30-minute period on a single day at a single location. Thus, I must ask: how representative are these results? Would these same results hold for different atmospheric state conditions (i.e., temperature and humidity profiles) or cirrus conditions (i.e., optically thicker clouds, cirrus generated by other means, etc). This is further complicated by the sky image shown in Figure 2, which suggests that their in-situ aircraft is leaving a contrail (based upon the flight pattern on the right and the clear spiral signature in the sky image). Can we assume the ice habit in the contrail is consistent with the habit of the background cirrus? How much is the contrail impacting either the radiometric observations made by the FINESSE or the in-situ obs (when aircraft starts its next circle)? Additionally, the ice optical depths sampled here are small; less than 0.2 – so again, do the conclusions (e.g., the importance of the far-infrared channels) hold when in cases when the optical depth is larger? Before this paper should be accepted, I would hope that the authors can address these concerns well.
Minor concerns:
Fig 15 (question 1): why do the INCAS points change mean values and have different error bar ranges in the 4 panels? This is most easily seen looking at the bottom-most panel against any of the other three?
Fig 15 (question 2): Why are the FINESSE error bars so much larger for cases 8-11 when HBR is assumed relative to when you assume ½ HBR+ ½ SBR? This does not make sense to me.
You are using a Bayesian retrieval framework, which is able to provide degrees of freedom for signal. For these very small optical depths, what is the DFS for the retrieved effective radius? Does it change when you assume different habits? Does it change when you only use the midinfrared vs when you use both the midinfrared and far infrared? (This would be a pretty convincing point to make, if the far infrared is indeed important).
Fig 17: caption errors: INCAS measurements are green dots, and only using the mid-IR is the violet diamonds
You spend very little time talking about the thermodynamic retrieval and its accuracy. Personally, I do not feel it adds anything to the paper; indeed, it is more distracting. If you elect to keep that portion in the paper for the next iteration, I would want to see much more discussion about it (recognizing that you don’t have strong sources of truth). But, in particular, your statement on line 468 about “excellent agreement…inside the cirrus” needs to be tempered. Does the FINESSE retrieval actually have any information content (i.e., degrees of freedom for signal) at that altitude? I would be very surprised if it did. And if the DFS is very small, then the agreement in temperature within the cirrus is more of a happy coincidence (provided by the statistics of the prior dataset used in the constraint, which you did not discuss at all) then real skill by the retrieval.