Seasonal and intra-diurnal variability of small-scale gravity waves in OH airglow at two Alpine stations

Hannawald, Patrick; Schmidt, Carsten; Sedlak, René; Wüst, Sabine; Bittner, Michael

doi:https://doi.org/10.5194/amt-12-457-2019

Articles | Volume 12, issue 1

https://doi.org/10.5194/amt-12-457-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Layered phenomena in the mesopause region (ACP/AMT inter-journal...

https://doi.org/10.5194/amt-12-457-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 1

Research article

|

25 Jan 2019

Research article |

| 25 Jan 2019

Seasonal and intra-diurnal variability of small-scale gravity waves in OH airglow at two Alpine stations

Patrick Hannawald, Carsten Schmidt, René Sedlak, Sabine Wüst, and Michael Bittner

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Final revised paper (published on 25 Jan 2019)
Preprint (discussion started on 04 Oct 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'amt-2018-322 Review', Anonymous Referee #1, 18 Oct 2018
- AC1: 'Reply to Anonymous Referee #1', Patrick Hannawald, 12 Dec 2018
RC2: 'Review of amt-2018-322', Anonymous Referee #2, 17 Nov 2018
- AC2: 'Reply to Anonymous Referee #2', Patrick Hannawald, 12 Dec 2018

Peer-review completion

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

AR by Patrick Hannawald on behalf of the Authors (12 Dec 2018) Author's response Manuscript

ED: Publish as is (18 Dec 2018) by Lars Hoffmann

Short summary

We use a near-infrared camera for the investigation of gravity waves. The camera observes the airglow layer, which is modulated by the gravity waves. The image processing, including the removal of the stars is explained. We describe the analysis with a 2D fast Fourier transform and automatic derivation of the wave parameters. The results show a clear seasonal and intra-diurnal variability, which is characterised in order to improve our understanding of gravity waves in the middle atmosphere.