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
Main Authors: Li, Qiang, Rapp, Markus, Schrön, Anne, Schneider, Andreas, Stober, Gunter
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2016
Subjects:
530
Online Access:https://doi.org/10.34657/1447
https://oa.tib.eu/renate/handle/123456789/4026