Representation of the equatorial stratopause semiannual oscillation in global atmospheric reanalyses

Kawatani, Yoshio; Hirooka, Toshihiko; Hamilton, Kevin; Smith, Anne K.; Fujiwara, Masatomo

doi:https://doi.org/10.5194/acp-20-9115-2020

Articles | Volume 20, issue 14

https://doi.org/10.5194/acp-20-9115-2020

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

Special issue:

The SPARC Reanalysis Intercomparison Project (S-RIP) (ACP/ESSD...

https://doi.org/10.5194/acp-20-9115-2020

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

Articles | Volume 20, issue 14

Research article

|

31 Jul 2020

Research article |

| 31 Jul 2020

Representation of the equatorial stratopause semiannual oscillation in global atmospheric reanalyses

Yoshio Kawatani, Toshihiko Hirooka, Kevin Hamilton, Anne K. Smith, and Masatomo Fujiwara

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Final revised paper (published on 31 Jul 2020)
Preprint (discussion started on 09 Mar 2020)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of Kawatani et al', Gloria Manney, 11 Apr 2020
- SC1: 'Tides', Paul Pukite, 21 May 2020
  - AC2: 'Reply to Dr. Pukite', Yoshio Kawatani, 19 Jun 2020
- AC3: 'Reply to Dr. Manney', Yoshio Kawatani, 21 Jun 2020
EC1: 'Review to ACP-2020-73', Martin Dameris, 29 May 2020
- AC1: 'Reply to the editor and reply to referee #2', Yoshio Kawatani, 30 May 2020

Peer-review completion

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

AR by Yoshio Kawatani on behalf of the Authors (21 Jun 2020) Author's response Manuscript

ED: Publish as is (29 Jun 2020) by Martin Dameris

Short summary

This paper reports on a project to compare the representation of the semiannual oscillation (SAO) among six major global atmospheric reanalyses and with recent satellite observations. The differences among the zonal mean zonal wind as represented by the various reanalyses display a prominent equatorial maximum that increases with height. It is shown that assimilation of satellite temperature measurements is crucial for the realistic representation of the tropical upper stratospheric circulation.