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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union

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Atmos. Meas. Tech., 10, 4895-4903, 2017
https://doi.org/10.5194/amt-10-4895-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article
14 Dec 2017
Variability of the Brunt–Väisälä frequency at the OH* layer height
Sabine Wüst et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review of amt-2017-191', Christian von Savigny, 20 Jul 2017 Printer-friendly Version 
AC1: 'Answerto amt-2017-191-RC1', Sabine Wüst, 26 Sep 2017 Printer-friendly Version Supplement 
 
RC2: 'amt-2017-191-review', Anonymous Referee #2, 24 Jul 2017 Printer-friendly Version Supplement 
AC2: 'Answer to amt-2017-191-RC2', Sabine Wüst, 26 Sep 2017 Printer-friendly Version Supplement 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sabine Wüst on behalf of the Authors (26 Sep 2017)  Author's response  Manuscript
ED: Publish subject to technical corrections (01 Oct 2017) by Sheila Kirkwood  
AR by Sabine Wüst on behalf of the Authors (09 Oct 2017)  Author's response  Manuscript
CC BY 4.0
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Short summary
In the Alpine region, the most dense subnetwork of identical NDMC (Network for the Detection of Mesospheric Change) instruments can be found. With these instruments the mesopause temperature is derived each night. The data can be used for the investigation of the amount of energy which is transported by small-scale atmospheric waves, known as gravity waves, provided that the so-called Brunt–Väisälä frequency is known. Information about the variability of this parameter is provided here.
In the Alpine region, the most dense subnetwork of identical NDMC (Network for the Detection of...
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