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 we...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-12-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/34/1209/2016/angeo-34-1209-2016.pdf |