Articles | Volume 41, issue 2
https://doi.org/10.5194/angeo-41-409-2023
https://doi.org/10.5194/angeo-41-409-2023
Regular paper
 | 
18 Oct 2023
Regular paper |  | 18 Oct 2023

Inferring neutral winds in the ionospheric transition region from atmospheric-gravity-wave traveling-ionospheric-disturbance (AGW-TID) observations with the EISCAT VHF radar and the Nordic Meteor Radar Cluster

Florian Günzkofer, Dimitry Pokhotelov, Gunter Stober, Ingrid Mann, Sharon L. Vadas, Erich Becker, Anders Tjulin, Alexander Kozlovsky, Masaki Tsutsumi, Njål Gulbrandsen, Satonori Nozawa, Mark Lester, Evgenia Belova, Johan Kero, Nicholas J. Mitchell, and Claudia Borries

Viewed

Total article views: 1,197 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
898 250 49 1,197 34 35
  • HTML: 898
  • PDF: 250
  • XML: 49
  • Total: 1,197
  • BibTeX: 34
  • EndNote: 35
Views and downloads (calculated since 14 Apr 2023)
Cumulative views and downloads (calculated since 14 Apr 2023)

Viewed (geographical distribution)

Total article views: 1,197 (including HTML, PDF, and XML) Thereof 1,194 with geography defined and 3 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 08 May 2024
Download
Short summary
Gravity waves (GWs) are waves in Earth's atmosphere and can be observed as cloud ripples. Under certain conditions, these waves can propagate up into the ionosphere. Here, they can cause ripples in the ionosphere plasma, observable as oscillations of the plasma density. Therefore, GWs contribute to the ionospheric variability, making them relevant for space weather prediction. Additionally, the behavior of these waves allows us to draw conclusions about the atmosphere at these altitudes.