Gravity waves excited during a minor sudden stratospheric warming

An exceptionally deep upper-air sounding launched from Kiruna airport (67.82◦ N, 20.33◦ E) on 30 January 2016 stimulated the current investigation of internal gravity waves excited during a minor sudden stratospheric warming (SSW) in the Arctic winter 2015/16. The analysis of the radiosonde profile...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Dörnbrack, Andreas, Gisinger, Sonja, Kaifler, Natalie, Portele, Tanja, Bramberger, Martina, Rapp, Markus, Gerding, Michael, Söder, Jens, Zagar, Nedjeljka, Jelic, Damjan
Format: Article in Journal/Newspaper
Language:German
Published: Copernicus Publications 2018
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Online Access:https://elib.dlr.de/121768/
https://elib.dlr.de/121768/1/D%C3%B6rnbrack-gravity-waves-excited-Atmos-Chem-Phys.pdf
https://doi.org/10.5194/acp-18-12915-2018
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Summary:An exceptionally deep upper-air sounding launched from Kiruna airport (67.82◦ N, 20.33◦ E) on 30 January 2016 stimulated the current investigation of internal gravity waves excited during a minor sudden stratospheric warming (SSW) in the Arctic winter 2015/16. The analysis of the radiosonde profile revealed large kinetic and potential energies in the upper stratosphere without any simultaneous enhancement of upper tropospheric and lower stratospheric values. Upward-propagating inertia-gravity waves in the upper stratosphere and downward-propagating modes in the lower stratosphere indicated a region of gravity wave Generation in the stratosphere. Two-dimensional wavelet analysis was applied to vertical time series of temperature fluctuations in order to determine the vertical propagation direction of the stratospheric gravity waves in 1-hourly high-resolution meteorological analyses and short-term forecasts. The separation of upward- and downward-propagating waves provided further evidence for a stratospheric source of gravity waves. The scale-dependent decomposition of the flow into a balanced component and inertia-gravity waves showed that coherent wave packets preferentially occurred at the inner edge of the Arctic polar vortex where a sub-vortex formed during the minor SSW.