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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 <i>ε</i> 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...

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Detaylı Bibliyografya
Asıl Yazarlar: Q. Li, M. Rapp, A. Schrön, A. Schneider, G. Stober
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Copernicus Publications 2016-12-01
Seri Bilgileri:Annales Geophysicae
Online Erişim:https://www.ann-geophys.net/34/1209/2016/angeo-34-1209-2016.pdf
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