Articles | Volume 18, issue 22
https://doi.org/10.5194/amt-18-6959-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Impact of lower atmospheric scattering on ground-based optical thermospheric wind observations with spatially uneven airglow
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- Final revised paper (published on 24 Nov 2025)
- Preprint (discussion started on 11 Aug 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-2025-3326', Anonymous Referee #2, 28 Aug 2025
- AC1: 'Reply on RC1', Xiaolong Wei, 26 Sep 2025
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RC2: 'Comment on egusphere-2025-3326', Anonymous Referee #1, 29 Aug 2025
- AC2: 'Reply on RC2', Xiaolong Wei, 26 Sep 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Xiaolong Wei on behalf of the Authors (26 Sep 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (29 Sep 2025) by Wen Yi
RR by Anonymous Referee #2 (29 Sep 2025)
RR by Anonymous Referee #1 (08 Oct 2025)
ED: Publish subject to minor revisions (review by editor) (13 Oct 2025) by Wen Yi
AR by Xiaolong Wei on behalf of the Authors (16 Oct 2025)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to minor revisions (review by editor) (21 Oct 2025) by Wen Yi
ED: Publish as is (27 Oct 2025) by Wen Yi
AR by Xiaolong Wei on behalf of the Authors (28 Oct 2025)
Manuscript
In the response to earlier comments the authors used TIEGCM simulation to justify wind field differences between N and S viewing directions cannot be larger than certain values. I don't think TIEGCM with resolution 100 km? can be a good reference. TIEGCM electric field is based on empirical convection pattern does not have small structure you would expect to see near auroral zone. Some additional clarifications are needed.