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...
Published in: | Annales Geophysicae |
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Main Authors: | , , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2016
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Subjects: | |
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 |
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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