Articles | Volume 34, issue 12
https://doi.org/10.5194/angeo-34-1209-2016
https://doi.org/10.5194/angeo-34-1209-2016
Regular paper
 | 
16 Dec 2016
Regular paper |  | 16 Dec 2016

Derivation of turbulent energy dissipation rate with the Middle Atmosphere Alomar Radar System (MAARSY) and radiosondes at Andøya, Norway

Qiang Li, Markus Rapp, Anne Schrön, Andreas Schneider, and Gunter Stober

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Short summary
Turbulence is an essential process in the atmosphere and ocean. Clear-air turbulence is a well-known threat for the safety of aviation. Using a powerful MST radar, we detected turbulence and compared it with the results from radiosondes. The correlation between turbulence and background conditions, e.g., Richardson number and wind shears, is determined. There is a nearly negative correlation between turbulence and Richardson number independent of the length scale over which it was calculated.