What is it about?
This paper investigates an extreme Koshava episode (EKE) which occurred at the beginning of 2014. Koshava is a local wind in southeast Europe. Koshava is typically strong wind, but this EKE was extremely vigorous. Wind gusts were above 45 m/s and the whole event was a blizzard with snow drifts as deep as 4 m. We investigated synoptic weather conditions which resulted in this EKE. Furthermore, we analyzed local and mesoscale factors responsible for this wind hazard. Lastly, the whole event was numerically simulated using Weather Research and Forecasting (WRF) models (NMM core) with several different settings. It has been concluded that numerical models are not capable of fully capturing and reproducing such high wind velocities.
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Why is it important?
- The strongest Koshava event ever analyzed in a peer-reviewer paper - Contributing factors to extremely high wind speeds were identified and analyzed - First numerical simulation of such a strong Koshava event - Drawbacks of numerical models to simulate extreme wind events are identified - Vertical structure of the Koshava layer is investigated using thermodynamic diagrams
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This page is a summary of: Investigation of an extreme Koshava wind episode of 30 January-4 February 2014, Atmospheric Science Letters, December 2015, Wiley,
DOI: 10.1002/asl.643.
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