• DOI:10.1002/2014JD022879
• Corpus ID: 59369401

Lidar observations of gravity wave activity in the middle atmosphere over Davis (69°S, 78°E), Antarctica

@article{Kaifler2015LidarOO,
  title={Lidar observations of gravity wave activity in the middle atmosphere over Davis (69°S, 78°E), Antarctica},
  author={Bernd Kaifler and Franz‐Josef L{\"u}bken and Josef H{\"o}ffner and Ray J. Morris and Timo P. Viehl},
  journal={Journal of Geophysical Research: Atmospheres},
  year={2015},
  volume={120},
  pages={4506 - 4521},
  url={https://api.semanticscholar.org/CorpusID:59369401}
}

• B. Kaifler, F. Lübken, +2 authors T. Viehl
• Published 27 May 2015
• Environmental Science, Physics
• Journal of Geophysical Research: Atmospheres

A 16 month series of lidar measurements in the stratosphere and mesosphere‐lower thermosphere (MLT) region over Davis Station (69°S, 78°E) in Antarctica is used to study gravity waves. The unprecedentedly large number of observations totaling 2310 h allows us to investigate seasonal variations in gravity wave activity in great detail. In the stratosphere the gravity wave potential energy density (GWPED) is shown to have a large seasonal variation with a double peak in winter and minimum in… 

A 16 month series of lidar measurements in the stratosphere and mesosphere‐lower thermosphere (MLT) region over Davis Station (69°S, 78°E) in Antarctica is used to study gravity waves. The unprecedentedly large number of observations totaling 2310 h allows us to investigate seasonal variations in gravity wave activity in great detail. In the stratosphere the gravity wave potential energy density (GWPED) is shown to have a large seasonal variation with a double peak in winter and minimum in summer. We find conservative wave propagation to occur between 29 and 41 km altitude in winter as well as in summer, whereas smaller energy growth rates were observed in spring and autumn. These results are consistent with selective critical‐level filtering of gravity waves in the lower stratosphere. In the MLT region the GWPED is found to have a semiannual oscillation with maxima in winter and summer. The structure of the winter peak is identical to that in the stratosphere, suggesting that the gravity wave flux reaching the MLT region is controlled by the wind field near the tropopause level.