Short vertical-wavelength inertia-gravity waves generated by a jet–front system at Arctic latitudes – VHF radar, radiosondes and numerical modelling

Inertia-gravity waves with very short vertical wavelength (λz≤1000 m) are a very common feature of the lowermost stratosphere as observed by the 52 MHz radar ESRAD (Esrange MST radar) in northern Scandinavia (67.88° N, 21.10° E). The waves are seen most clearly in radar-derived profiles of buoyancy...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Réchou, A., Kirkwood, S., Arnault, J., Dalin, P.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/acp-14-6785-2014
https://noa.gwlb.de/receive/cop_mods_00044940
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00044560/acp-14-6785-2014.pdf
https://acp.copernicus.org/articles/14/6785/2014/acp-14-6785-2014.pdf