Articles | Volume 25, issue 21
https://doi.org/10.5194/acp-25-14839-2025
https://doi.org/10.5194/acp-25-14839-2025
Research article
 | 
05 Nov 2025
Research article |  | 05 Nov 2025

Spectral variability of gravity-wave kinetic and potential energy at 69° N: a seven-year lidar study

Mohamed Mossad, Irina Strelnikova, Robin Wing, Gerd Baumgarten, and Michael Gerding

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Assessing atmospheric gravity wave spectra in the presence of observational gaps
Mohamed Mossad, Irina Strelnikova, Robin Wing, and Gerd Baumgarten
Atmos. Meas. Tech., 17, 783–799, https://doi.org/10.5194/amt-17-783-2024,https://doi.org/10.5194/amt-17-783-2024, 2024
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Cited articles

Alexander, M. J., Liu, C. C., Bacmeister, J., Bramberger, M., Hertzog, A., and Richter, J. H.: Observational validation of parameterized gravity waves from tropical convection in the whole atmosphere community climate model, J. Geophys. Res.-Atmos., 126, https://doi.org/10.1029/2020JD033954, 2021. a
Alexander, S., Klekociuk, A., and Murphy, D.: Rayleigh lidar observations of gravity wave activity in the winter upper stratosphere and lower mesosphere above Davis, Antarctica (69°S, 78°E), J. Geophys. Res.-Atmos., 116, https://doi.org/10.1029/2010JD015164, 2011. a
Allen, S. J. and Vincent, R. A.: Gravity wave activity in the lower atmosphere: seasonal and latitudinal variations, J. Geophys. Res.-Atmos., 100, 1327–1350, https://doi.org/10.1029/94JD02688, 1995. a, b, c
Baumgarten, G.: Doppler Rayleigh/Mie/Raman lidar for wind and temperature measurements in the middle atmosphere up to 80 km, Atmos. Meas. Tech., 3, 1509–1518, https://doi.org/10.5194/amt-3-1509-2010, 2010. a, b, c
Baumgarten, G., Fiedler, J., Hildebrand, J., and Lübken, F.: Inertia gravity wave in the stratosphere and mesosphere observed by Doppler wind and temperature lidar, Geophys. Res. Lett., 42, 10929–10936, https://doi.org/10.1002/2015GL066991, 2015. a, b, c
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We studied gravity waves using a unique lidar that measures both temperature and wind. This is the first long-term study of how their energies vary with height and season in the middle atmosphere near the Arctic. Waves were stronger and varied more in winter, while in summer slow waves tied to Earth's rotation dominated. We also observed new patterns in how energy is shared between both energy types and height-dependent changes in wave behaviour. These results refine our view of such waves.
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