Vertical wind profiling from the troposphere to the lower mesosphere based on high-resolution heterodyne near-infrared spectroradiometry

Rodin, Alexander V.; Churbanov, Dmitry V.; Zenevich, Sergei G.; Klimchuk, Artem Y.; Semenov, Vladimir M.; Spiridonov, Maxim V.; Gazizov, Iskander S.

doi:https://doi.org/10.5194/amt-13-2299-2020

Articles | Volume 13, issue 5

https://doi.org/10.5194/amt-13-2299-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/amt-13-2299-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 5

Research article

|

13 May 2020

Research article |

| 13 May 2020

Vertical wind profiling from the troposphere to the lower mesosphere based on high-resolution heterodyne near-infrared spectroradiometry

Alexander V. Rodin, Dmitry V. Churbanov, Sergei G. Zenevich, Artem Y. Klimchuk, Vladimir M. Semenov, Maxim V. Spiridonov, and Iskander S. Gazizov

Download

Final revised paper (published on 13 May 2020)
Preprint (discussion started on 19 Dec 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Review report_amt-2019-444', Anonymous Referee #1, 25 Jan 2020
- AC1: 'Reply to Review 1', Alexander Rodin, 02 Mar 2020
RC2: 'Review', Anonymous Referee #2, 06 Feb 2020
- AC2: 'Reply to Review 2', Alexander Rodin, 10 Mar 2020

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Alexander Rodin on behalf of the Authors (10 Mar 2020) Manuscript

ED: Referee Nomination & Report Request started (23 Mar 2020) by Ad Stoffelen

RR by Anonymous Referee #2 (27 Mar 2020)

RR by Anonymous Referee #1 (07 Apr 2020)

ED: Publish subject to technical corrections (08 Apr 2020) by Ad Stoffelen

AR by Alexander Rodin on behalf of the Authors (09 Apr 2020) Author's response Manuscript

Short summary

The paper presents a new technique in remote wind measurements that may potentially complement conventional aerological observations and eventually greatly improve our knowledge about our climate system, especially concerning processes related to troposphere–stratosphere coupling. The technique may be implemented at relatively low cost in various applications from meteorological observation posts to remote sensing spacecraft.