Articles | Volume 14, issue 9
Atmos. Meas. Tech., 14, 5873–5886, 2021
https://doi.org/10.5194/amt-14-5873-2021
Atmos. Meas. Tech., 14, 5873–5886, 2021
https://doi.org/10.5194/amt-14-5873-2021

Research article 31 Aug 2021

Research article | 31 Aug 2021

Using vertical phase differences to better resolve 3D gravity wave structure

Corwin J. Wright et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on amt-2021-93', Anonymous Referee #1, 06 May 2021
  • RC2: 'Comment on amt-2021-93', Anonymous Referee #2, 18 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Corwin Wright on behalf of the Authors (28 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (29 Jun 2021) by Jorge Luis Chau
RR by Anonymous Referee #1 (02 Jul 2021)
RR by Anonymous Referee #2 (17 Jul 2021)
ED: Publish subject to technical corrections (21 Jul 2021) by Jorge Luis Chau
AR by Corwin Wright on behalf of the Authors (29 Jul 2021)  Author's response    Manuscript
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Short summary
Measuring atmospheric gravity waves in low vertical-resolution data is technically challenging, especially when the waves are significantly longer in the vertical than in the length of the measurement domain. We introduce and demonstrate a modification to the existing Stockwell transform methods of characterising these waves that address these problems, with no apparent reduction in the other capabilities of the technique.