Articles | Volume 16, issue 4
https://doi.org/10.5194/acp-16-2299-2016
https://doi.org/10.5194/acp-16-2299-2016
Research article
 | 
26 Feb 2016
Research article |  | 26 Feb 2016

Change in turbopause altitude at 52 and 70° N

Chris M. Hall, Silje E. Holmen, Chris E. Meek, Alan H. Manson, and Satonori Nozawa

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chris Hall on behalf of the Authors (07 Dec 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 Dec 2015) by Gabriele Stiller
RR by Anonymous Referee #2 (19 Jan 2016)
RR by Anonymous Referee #3 (19 Jan 2016)
ED: Reconsider after minor revisions (Editor review) (20 Jan 2016) by Gabriele Stiller
AR by Chris Hall on behalf of the Authors (22 Jan 2016)  Author's response   Manuscript 
ED: Publish as is (10 Feb 2016) by Gabriele Stiller
AR by Chris Hall on behalf of the Authors (16 Feb 2016)  Manuscript 
Download
Short summary
Turbulent energy dissipation rates are calculated using MF-radar signals from 70 and 52° N for the period 2001–2014 inclusive, and they are used to estimate turbopause altitudes. A positive trend in turbopause altitude is identified for 70° N in summer, but not in winter and not at 52° N. The turbopause altitude change between 2001 and 2014 can be used to hypothesize a corresponding change in atomic oxygen concentration.
Altmetrics
Final-revised paper
Preprint