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 " 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 ballo...

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Bibliographic Details
Published in:Annales Geophysicae
Main Authors: Li, Qiang, Rapp, Markus, Schrön, Anne, Schneider, Andreas, Stober, Gunter
Other Authors: KOTRONI, Vassiliki
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Lidar
Institut für Physik der Atmosphäre
Alomar
Andøya
Norway
Online Access:https://elib.dlr.de/119948/
https://elib.dlr.de/119948/1/angeo-34-1209-2016.pdf
https://doi.org/10.5194/angeo-34-1209-2016
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Summary:We present the derivation of turbulent energy dissipation rate " 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-borne radiosondes based on a campaign in the summer 2013. Spectral widths are converted to " after the removal of the broadening effects due to the finite beam width of the radar.

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