Articles | Volume 11, issue 5
https://doi.org/10.5194/amt-11-2937-2018
https://doi.org/10.5194/amt-11-2937-2018
Research article
 | 
18 May 2018
Research article |  | 18 May 2018

Derivation of gravity wave intrinsic parameters and vertical wavelength using a single scanning OH(3-1) airglow spectrometer

Sabine Wüst, Thomas Offenwanger, Carsten Schmidt, Michael Bittner, Christoph Jacobi, Gunter Stober, Jeng-Hwa Yee, Martin G. Mlynczak, and James M. Russell III

Viewed

Total article views: 3,007 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,475 1,210 322 3,007 102 354
  • HTML: 1,475
  • PDF: 1,210
  • XML: 322
  • Total: 3,007
  • BibTeX: 102
  • EndNote: 354
Views and downloads (calculated since 10 Oct 2017)
Cumulative views and downloads (calculated since 10 Oct 2017)

Viewed (geographical distribution)

Total article views: 3,007 (including HTML, PDF, and XML) Thereof 2,884 with geography defined and 123 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Jul 2024
Download
Short summary
OH*-spectrometer measurements allow the analysis of gravity wave ground-based periods, but spatial information cannot necessarily be deduced. We combine the approach of Wachter at al. (2015) in order to derive horizontal wavelengths (but based on only one OH* spectrometer) with additional information about wind and temperature and compute vertical wavelengths. Knowledge of these parameters is a precondition for the calculation of further information such as the wave group velocity.