Derivation of turbulent energy dissipation rate with the Middle Atmosphere Alomar Radar System (MAARSY) and radiosondes at Andøya, Norway

We present the derivation of turbulent energy dissipation rate ε from a total of 522 days of observations with the Middle Atmosphere Alomar Radar SYstem (MAARSY) mesosphere–stratosphere–troposphere (MST) radar running tropospheric experiments during the period of 2010–2013 as well as with balloon-bo...

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Bibliographic Details
Published in:Annales Geophysicae
Main Authors: Li, Qiang, Rapp, Markus, Schrön, Anne, Schneider, Andreas, Stober, Gunter
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/angeo-34-1209-2016
https://noa.gwlb.de/receive/cop_mods_00011030
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010987/angeo-34-1209-2016.pdf
https://angeo.copernicus.org/articles/34/1209/2016/angeo-34-1209-2016.pdf