"Vertical structure of the Arctic spring transition in the middle atmosphere"

In the middle atmosphere, spring transition is the time period where the zonal circulation reverses from winter westerly to summer easterly which has a strong impact on the vertical wave propagation influencing the ionospheric variability. The spring transition can be rapid in form of a final sudden...

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Bibliographic Details
Main Authors: Matthias, Vivien, Stober, Gunter, Kozlovsky, Alexander, Lester, Mark, Belova, Evgenia, Kero, Johan
Other Authors: Manney, G.L., Butler, A., Wargan, Krzysztof, Grooss, Jens-Uwe
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: Wiley 2021
Subjects:
Online Access:https://elib.dlr.de/141897/