Articles | Volume 19, issue 6
https://doi.org/10.5194/amt-19-2103-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Operational calibration of a ground-based fully polarimetric radiometer for stratospheric temperature retrievals
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- Final revised paper (published on 26 Mar 2026)
- Preprint (discussion started on 16 Sep 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-2025-2561', Anonymous Referee #1, 02 Oct 2025
- AC1: 'Reply on RC1', Witali Krochin, 06 Oct 2025
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RC2: 'Comment on egusphere-2025-2561', Anonymous Referee #2, 06 Oct 2025
- AC2: 'Reply on RC2', Witali Krochin, 17 Oct 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Witali Krochin on behalf of the Authors (04 Nov 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (11 Dec 2025) by Dietrich G. Feist
RR by Anonymous Referee #2 (19 Jan 2026)
ED: Reconsider after major revisions (23 Jan 2026) by Dietrich G. Feist
AR by Witali Krochin on behalf of the Authors (09 Feb 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (13 Mar 2026) by Dietrich G. Feist
AR by Witali Krochin on behalf of the Authors (13 Mar 2026)
Manuscript
Review of Krochin et al., Operational calibration of a fully polarimetric radiometer for stratospheric temperature retrievals.
This study shows that using polarimetric information can result in a small improvement in temperature retrievals form a ground-based radiometer. As such, it provides an especially useful study for any group trying to determine the cost-benefit of developing a system with full polarization capability for making such measurements. It is certainly appropriate for publication.
Line 92 – “Overall, it was found that the ratio between the middle atmospheric signal and the tropospheric signal amplitude increases from 1.05 to 1.2.” Does this sentence refer to the range of ratios over several months at Jungfraujoch? I think that is the case, but what is confusing is that there is then a mention of observations at Bern. Is there a separate range of amplitude ratio variations at Bern? I think part of the idea of this paragraph is to show the advantage of measuring from Jungfraujoch, but it is strange that this is all based on two single days of measurements.
Line 109 –Is it obvious that these 5 measurements suggested are sufficiently orthogonal to determine the 20 unknowns?
Line 232 – Does “Δϕ = 0.65±0.01π” mean “Δϕ = 0.65π ±0.01π”?
Figure 13 – Would I be correct in understanding that the Q-component is the small difference between the blue and red lines in the top panels. If so, could this be plotted on the middle panels?
Line 282 – As I understand it the opacity is determined directly from the temperature, pressure, and humidity profiles obtained from other sensors, so no information directly from the measurements (e.g. a tipping curve) is used to determine the tropospheric opacity. Do I understand this correctly?