The paper discusses the conditions corresponding to the largest and smallest North Atlantic Oscillations (NAOs). It is shown that in winter, when NAOs are at a minimum, the number of cyclones over the Black Sea increases. At the same time, cloudiness in the Atlantic-European section becomes heavier, compared with the largest NAO. Heavy cloudiness over the Balkan and Karpaty mountains, with NAO at a minimum, may imply the greater likelihood of Balkan cyclones’ penetration into the Black Sea region. The mechanism responsible for the generation of maximum (minimum) cloudiness in the Atlantic-European section is discussed.
Physical Oceanography – Springer Journals
Published: Oct 22, 2006
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